2012 Assessment Work Report

A Drilling Exploration Project

Richardson Lake & Upper Scotch Lake Area

Thunder Bay Mining Division, Ontario

Prepared and Submitted by

China Metallurgical Exploration Corp. (CME)

(145 Riviera Drive, Unit 7, Markham,

Ontario L3R 5J6, Canada)

July 20, 2012

Table of Content

List of Figures ............................................................................................................... 3

List of Tables ................................................................................................................. 3

List of Appendices ........................................................................................................ 3

1. Introduction ........................................................................................................... 4

2. Claims, Location, and Access ............................................................................... 4

2.1 Property Description and Ownership ...................................................... 4

3. Property Location and Access .............................................................................. 9

4. Previous Work Performed by CME .................................................................. 10

5. Regional Geological Setting ............................................................................... 11

5.1. Rock type .................................................................................................. 11

5.2. Stratum. .................................................................................................... 11

5.3. Mineralization .......................................................................................... 11

6. Drilling Exploration Project 2011 ...................................................................... 17

6.1. General information ................................................................................ 12

6.2. Products and Conclusion ........................................................................ 13

7. References ............................................................................................................ 25

List of Figures

Figure 1: Claim Map ......................................................................................................................... 8

Figure 2: Property Location Map ...................................................................................................... 9

Figure 3: Property Access Map ....................................................................................................... 10

Figure 4: Drilling Site Map ............................................................. Error! Bookmark not defined.

List of Tables

Table 1: Property Claim Identity ....................................................................................................... 4

Table 2: Property Co-ordinates ......................................................................................................... 8

List of Appendices

Appendix 1 Summary Report of Drilling Exploration…………..………….…independent File

1. Introduction

The whole CME’s Richardson Lake & Upper Scotch Lake Property and claims were acquired or staked / recorded by CME through 2009 and 2012due to its potential of hosting Copper, Zinc, and Gold. Since some of the current claims on this property were staked / recorded after the Drilling Exploration which was performed in March 2011, they are NOT part of this assessment work report. All the information, materials, and maps discussed in this report and its appendices only cover and refer to the claims recorded before the Drilling Exploration. Terms such as “the property”, “this property”, or “the Richardson Lake & Upper Scotch Lake Property” used below through the whole report for the purpose of convenient narration as well only refer to these claims recorded before the Drilling Exploration. In March 2011, a CME geology team did a traverse visit to the property; and in the same month, a Drilling Exploration was performed on this property to prove valuable magnetic and electromagnetic information gathered by the helicopter-borne survey carried in 2010 as basis for further exploration work. On the basis of interpretation and recommendations by Geotech, CME conducted a 12 hole diamond drill program totaling 1,658.72 metres to test selected airborne magnetic and electromagnetic anomalies. The drill program was conducted from March to May,2011 and focused on identification of potential base metal mineralization associated with the geophysical conductors.

2. Claims, Location, and Access

2.1 Property Description and Ownership

The Property consists of 51 contiguous unpatented claims within the Richardson Lake Area and Upper Scotch Lake Area. Specific claim information is provided in Table 1. The claims location and layout, along with their coordinates are given in Figure 1,

and Table 2.

Table 1: Property Claim Identity

Township/Area Claim

Number Recording

Date Claim Due Date

RICHARDSON LAKE AREA 4248129 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4248130 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252241 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252242 2009-Aug-04 2012-Aug-04

RICHARDSON LAKE AREA 4252243 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252244 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252245 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252246 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252247 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252248 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252249 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252250 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4254299 2010-Nov-22 2012-Nov-22 RICHARDSON LAKE AREA 4256067 2010-Nov-22 2012-Nov-22 RICHARDSON LAKE AREA 4256068 2010-Nov-22 2012-Nov-22 RICHARDSON LAKE AREA 4256069 2010-Nov-22 2012-Nov-22 RICHARDSON LAKE AREA 4258300 2010-Nov-22 2012-Nov-22 RICHARDSON LAKE AREA 4258830 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4258831 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4258832 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4258833 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260202 2011-Sep-09 2013-Sep-09 RICHARDSON LAKE AREA 4260205 2011-Sep-09 2013-Sep-09 RICHARDSON LAKE AREA 4260206 2011-Sep-09 2013-Sep-09 RICHARDSON LAKE AREA 4260210 2011-Sep-09 2013-Sep-09 RICHARDSON LAKE AREA 4260221 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260222 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260223 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260224 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260228 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260229 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260230 2011-Mar-02 2013-Mar-02 UPPER SCOTCH LAKE AREA 4252233 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252234 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252235 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252236 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252237 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252238 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252239 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252240 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4259018 2011-Jan-31 2013-Jan-31 UPPER SCOTCH LAKE AREA 4259019 2011-Jan-31 2013-Jan-31 UPPER SCOTCH LAKE AREA 4261360 2011-Apr-26 2013-Apr-26

UPPER SCOTCH LAKE AREA 4263611 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263612 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263613 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263614 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263615 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263616 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263617 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263618 2011-Apr-26 2013-Apr-26

Table 2: Property Co-ordinates at Date of Drilling

Infl. Point

Longitude/Latitude Infl. Point

Longitude/Latitude

1 91° 9’ 10.19” W 49° 9’ 19.48” N 13 91° 9’ 37.38” W 49° 4’ 28.58” N 2 91° 6’ 31.13” W 49° 9’ 16.23” N 14 91° 10’ 55.73” W 49° 4’ 29.46” N

3 91° 6’ 33.80” W 49° 7’ 59.66” N 15 91° 10’ 56.02” W 49° 4’ 37.74” N 4 91° 5’ 55.07” W 49° 7’ 59.36” N 16 91° 12’ 14.07” W 49° 4’ 39.52” N

5 91° 5’ 56.55” W 49° 7’ 7.63” N 17 91° 12’ 12.59” W 49° 5’ 30.96” N 6 91° 5’ 17.52” W 49° 7’ 6.45” N 18 91° 11’ 18.79” W 49° 5’ 31.55” N

7 91° 5’ 20.18” W 49° 5’ 48.69” N 19 91° 11’ 15.83” W 49° 5’ 54.02” N 8 91° 7’ 58.64” W 49° 5’ 51.95” N 20 91° 10’ 56.32” W 49° 5’ 54.31” N

9 91° 8’ 0.71” W 49° 4’ 46.61” N 21 91° 10’ 54.84” W 49° 6’ 33.33” N 10 91° 8’ 40.03” W 49° 4’ 46.02” N 22 91° 10’ 15.52” W 49° 6’ 32.74” N

11 91° 8’ 41.51” W 49° 4’ 9.07” N 23 91° 10’ 11.68” W 49° 8’ 2.91” N 12 91° 9’ 38.27” W 49° 4’ 10.25” N 24 91° 9’ 13.44” W 49° 8’ 2.32” N

Figure 1: Claim Map at Date of Drilling

3. Property Location and Access

CME’s Richardson Lake & Upper Scotch Lake Property is located in Richardson Lake & Upper Scotch Lake areas, Thunder Bay Mining Division, ON. The closest town is Upsala, approximately 45 km² to the East of the property. Thunder Bay is approximately 190 km² in the Southeast (Figure 2).

Figure 2: Property Location Map

The TransCanada Highway 17 runs E-W through Upsala and to the East and North of the property. A trail off Hwy 17 at Graham Road leads to the property. . (Figure 3)

Figure 3: Property Access Map

4. Previous Work Performed by CME

A CME geology team did a preliminary a traverse visit to the property in May, 2010. Exploration products such as mapping or systematic sample assays were not intended or produced. The main objective of the visit was to acquire some valuable information regarding the geological setting, mineralization conditions of the property and provide reference in support of future geology work. The team observed and examined the outcrops and mineralization at the geological observation points. A NITON XL3t-500 handheld X-ray fluorescence ore analyzer was used to analyze the mineralized rocks (ore) to preliminarily determine the content of Cu and Zn in the field. A few samples were collected to analyze the grade of Cu and Au. A total of 24 geological points with a total length of approximately 16.6km were surveyed. In order to better understand the property’s geology and collect its magnetic and electromagnetic information, in September, 2010, a helicopter-borne geophysical survey was carried out by Geotech Ltd. on behalf of CME over its Richardson Lake & Upper Scotch Lake property. The total survey coverage for the area was 495.5 line-km.

The survey was flown at 100 metres line spacing with a West to East (N90º E/N 270°E) flight line direction.

5. Regional Geological Setting

The topography of the property shows low-to-moderate hills and the elevation is approximately 460-560 meters. Numerous rivers connect various lakes and the surrounding wetlands. Outcrops can be observed and the most areas are covered by sand, soil, and vegetation. In 1985, M.C. Jackson performed a research of the geological features in the Lumby Lake area. Much of the property is located in the area defined in Jackson’s study. According to Jackson’s research, Lumby Lake is in the Canadian Shield area, represented by Archean greenstone belt.

5.1. Rock type

According to the past research and the CME traverse survey, the rock types in the property include the Archaeozoic mafic metavolcanics, felsic metavolcanics, metamorphic sedimentary rocks, felsic intrusive rocks and mafic intrusive rocks. Mafic metavolcanics: widespread, the outcrops observed by the CME geo team are mostly mafic metavolcanics. Rock types are mainly massive and pillow lavas. Felsic intrusive rock: distributed at the western and northeastern edge of the property. Rock type is granite. According to CME team’s observation, Granite is light reddish, containing feldspar and quartz.

5.2. Stratum.

Stratums distributed in this area include Archaeozoic and Cenozoic strata. Archaean: mafic metavolcanic rocks, felsic - neutral metavolcanic rocks, metamorphic clastic sedimentary rocks and metamorphic sedimentary rocks. Mafic metavolcanics is the main lithology in this area, making up to 80 percent of the greenstone. The main rock types include massive or pillow lava, variolite, tuff, lapilli tuff, tuff breccia, plagioclase-porphyritic flows, etc. Cenozoic: in recent and pleistocene lake, stream and wetland deposits, glacial, glaciofluvial and glaciolacustrine deposits: sand, gravel, clay, till.

5.3. Mineralization

Mineral exploration in this area began in 1913. Minerals include iron, gold, and some base metals. Gold mineralization is mainly observed in the sedimentary rocks containing iron construction. Base metals (copper, lead, zinc) are mainly found in copper-nickel sulfide deposits.

The CME geo team observed limonitization in the mafic metavolcanics and the metamorphic sedimentary rocks in the property. Some outcrops (floats) exhibits minor Cu and Zn mineralization.

6. Drilling Exploration 2011

6.1. General information

On the basis of interpretation and recommendations by Geotech, CME conducted a 12 hole diamond drill program totaling 1,658.72 metres to test selected airborne magnetic and electromagnetic anomalies. The drill program was conducted from March to May, 2011 and focused on identification of potential base metal mineralization associated with the geophysical conductors. We analysed 458 pieces of sample for copper and gold. (The planned drilling hole ZK5 did not drilled)（表 3，图 9）

Table 3 Drilling Hole Information of Richardson Lake Property, 2011

Hole# Measured coordinate Designed

dip /azimuth

(°)

Designed

depth

（m）

Completion

depth （m）

Sample

analysis

（piece） X Y Z

ZK1 633682.998 5438207.218 497.124 45/90 150 163.68 62

ZK2 633404.587 5438233.876 501.690 45/70 120 123.44 9

ZK3 633025.454 5438170.008 510.101 55/60 150 150.88 33

ZK4 635010.358 5440603.521 540.182 60/250 200 177.39 18

ZK5 50/70 150 Undrilling /

ZK6 634089.253 5440803.821 510.628 60/90 160 141.73 95

ZK7 634713.398 5441172.069 507.698 50/55 120 124.05 33

ZK8 634409.031 5441157.381 511.544 55/65 150 150.88 8

ZK9 634321.713 5443331.717 502.892 65/270 120 133.20 40

ZK10 636738.912 5445230.614 514.427 55/110 120 123.44 38

ZK11 636874.032 5445451.449 507.698 50/120 80 117.35 62

ZK12 636708.874 5445441.670 511.544 55/110 80 105.16 9

ZK13 635309.305 5443119.607 564.416 45/150 150 147.52 10

Total 1600 1658.72 417

Figure 9 TAU、CVG anomaly isogram and geology map

(with site of planned drilling hole，ZK5 undrilled)

6.2. Products and Conclusion

Products:

Except drilling hole ZK2、ZK4、ZK8、ZK12 andZK13 show little sulfide, the other drilling hole met plenty of sulfide zone (table 4), no result of copper and gold mineralization, the airborne anomaly was almost caused by pyrrhotine and pyrite.

Table4 Sulfide Zone Information of Richardson Lake Property, 2011

Hole

#

Sulfide Zone depth（m） Rock/ore type

Sulfid

e type

Analysis result

Cu（%） Au（g/t）

Form To Coun tenor Tenor tenor Tenor

t Ave Ave

ZK1

9.75 20.05 10.30 Basalt ,pyrrho

tine

Po、bit

Py、

precio

us

little

Clp

0.026-0.052 0.036 / /

20.05 86.57 66.52 Metavolcanite

, pyrrhotine

Po、

Mag、

bit

Py、

precio

us

little

Clp

0.001-0.196 0.027 0.019-0.253 0.056

ZK2 Bit Po、Py 0.012-0.070 0.024 <0.005 <0.005

ZK3

7.02 10.67 3.65

Andesite,

pyrrhotine

Po 0.013-0.135 0.074 / /

80.02 113.99 33.97 Metavolcanite

, pyrrhotine

Po、

Py、

precio

us

little

Clp

0.004-0.099 0.034 0.012-0.064 0.031

ZK4 Bit Po 0.003-0.258 0.038 <0.005 <0.005

ZK6

18.06 42.86 24.80

Andesite,

pyrrhotine

Po、Py 0.006-0.116 0.039 0.007-0.025 0.015

45.86 68.28 22.42 Massive

sulfide Po、Py 0.015-0.064 0.032 0.009-0.026 0.016

68.28 82.46 14.18 Andesite,

pyrrhotine Po、Py 0.007-0.034 0.015 0.005-0.025 0.012

83.20 106.28 23.08 Massive

sulfide Py、Po 0.002-0.059 0.014 <0.005-0.012 0.005

108.00 116.31 8.31 Massive

sulfide Py、Po 0.004-0.017 0.012 0.009 0.009

ZK7

1.30 9.40 8.10 Andesite,

pyrrhotine Py、Po 0.011-0.044 0.021 <0.005 <0.005

29.87 33.81 3.94 Andesite,

pyrrhotine

Py、

Po、

precio

us

little

Clp

<0.001-0.031 0.018 0.006-0.010 0.008

44.81 57.27 12.46 Andesite,

pyrrhotine

Py、

Po、

precio

us

little

Clp

0.005-0.025 0.013 <0.005-0.006 <0.005

ZK8 Bit Py、precious little Clp 0.010-0.117 0.029 / /

ZK9

13.43 38.16 24.73 Andesite,

pyrrhotine

Po、bit

Py,、

precio

us

little

Clp

0.004-0.036 0.016 <0.005-0.036 0.017

38.16 52.09 13.93 Andesite,

pyrrhotine Bit Po 0.007-0.014 0.012 <0.005 <0.005

52.09 59.17 7.08 Andesite,

pyrrhotine

Po、

precio

us

little

Clp

0.008-0.027 0.019 <0.005-0.008 <0.005

ZK1

0

11.77 42.05 30.28

Andesite,

Massive

sulfide

Py、

Po、

precio

us

little

Clp

<0.001-0.756 0.078 <0.005-0.034 0.013

44.00 54.56 10.56

Andesite,

Massive

sulfide

Py、

Po、

precio

us

little

0.013-0.447 0.130 0.014 0.014

Clp

ZK1

1 16.51 86.87 70.36 Andesite

Py、

Po、

precio

us

little

Clp

0.020-0.142 0.036 <0.005-0.019 0.008

ZK1

2 61.52 61.92 0.40

Andesite,

pyrrhotine Py、Po 0.063 0.063 0.007 0.007

ZK1

3 8.80 10.76 1.96

Andesite,

pyrrhotine

Py、

Po、

Clp

0.133-0.301 0.217 0.095 0.095

6.2.1 Drill Logs & Assays

6.2.2 Conclusion

(1) A helicopter-borne geophysical survey and magnetic measurement interpreted some geophysical anomaly, The airborne anomaly was almost caused by Basalt, pyrrhotine and pyrite, some of the anomaly was caused by basic and ultrabasic rock what proved by drilling, (2)The result of the drilling shows that there are a lot of sulfides in the area, distributed as massive、denseness immerse、stripe. Sulfides almost pyrrhotine and pyrite are distributed as fine grained xenoblast-half idiomorphism condition.. There are some magnetite distributes in somewhere of anomaly area A, almost no chalcopyrite. The analysised sample shows no copper mineralization, representative sample and all samples from ZK9 shows no gold mineralization.

7. References（根据打钻公司、参与人员进行修改）

Geotech Ltd. September, 2010: Report on a Helicopter-borne Versatile Time Electromagnetic

(VTEM) and Aeromagnetic Geophysical Survey

Xianjun Li & Shawn Yang June, 2010: Summary of Geological Traverse Survey, Palmer Township and Ryan

Township, Sault Ste. Marie District, Ontario

Jackson, M.C. 1985: Geology of the Lumby Lake Area, Eastern Part, Districts of Kenora and Rainy

River; Ontario Geological Survey, Open File Report 5535,142p., 7 tables, 12 figures, 7 photographs, and l map in back pocket.

序号 工程编号 送样编号 岩矿心长 采取率 采样规格 样品重量 岩（矿）石 名 称采

样日

期

No. DH No.Sample

No.to Lab自

(From)至

(To)样长

(Length)

Length of

core (m)

Recovery

factor(%)Size(mm) Weight(kg) Rock/Ore type

Samp

ling

date

ME Au AgAl

%

As

ppm

Ba

ppm

Be

ppm

Ca

%

Cd

ppm

Cr

ppm

Co

ppm

Cu

ppm

Fe

%

K

%

La

ppm

Li

ppm

Mg

%

Mn

ppm

Mo

ppm

Ni

ppm

P

%

Pb

ppm

Sb

ppm

Sc

ppm

Sn

ppm

1 ZK1 RL.H-1 9.75 11.28 1.53 0.93 61 42/2 磁黄铁矿化(变）玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.6 90 180 <5 1.1 <10 670 100 390 7.99 2.7 10 40 1.41 1560 <10 280 0.05 70 <50 40 <50

2 ZK1 RL.H-2 12.68 1.40 1.40 100 42/2 磁黄铁矿化(变）玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.7 40 170 <5 0.5 <10 730 90 260 7.56 2.7 10 30 1.12 1700 <10 260 0.02 60 <50 40 <50

3 ZK1 RL.H-3 14.08 1.40 1.40 100 42/2 磁黄铁矿化(变）玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.8 <30 170 <5 0.7 <10 700 80 370 7.91 2.6 10 40 1.25 1980 <10 220 0.03 60 <50 41 <50

4 ZK1 RL.H-4 15.43 1.35 1.35 100 42/2 磁黄铁矿化(变）玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.4 90 190 <5 0.5 <10 690 70 260 7.04 2.6 10 40 1.26 1890 <10 250 0.02 60 <50 40 <50

5 ZK1 RL.H-5 16.80 1.37 1.37 100 42/2 磁黄铁矿化(变）玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.3 <30 170 <5 0.8 <10 680 120 520 9.75 2.5 10 40 1.25 1740 <10 350 0.02 80 <50 40 <50

6 ZK1 RL.H-6 18.17 1.37 1.37 100 42/2 磁黄铁矿化(变）玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.7 <30 160 <5 1 <10 710 90 370 8.73 2.5 10 30 1.15 2010 <10 270 0.02 60 <50 41 <50

7 ZK1 RL.H-7 19.05 0.88 0.88 100 42/2 磁黄铁矿化(变）玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.2 <30 160 <5 1.1 <10 700 80 380 9.75 2.2 <10 30 1.14 2620 <10 240 0.02 50 <50 41 <50

8 ZK1 RL.H-8 20.05 1.00 1.00 100 42/2 磁黄铁矿化(变）玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.1 <30 150 <5 0.7 <10 760 100 330 11.4 2.1 10 30 1 2590 <10 290 0.02 40 <50 41 <50

9 ZK1 RL.H-9 21.35 1.30 1.30 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.73 <30 10 <5 3.8 <10 120 30 100 25.6 0.2 <10 <10 3.02 3860 <10 80 0.08 <20 <50 5 <50

10 ZK1 RL.H-10 22.70 1.35 1.35 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 2.39 <30 70 <5 3.3 <10 160 40 110 27.1 0.4 <10 20 3.3 2850 <10 80 0.06 <20 <50 8 <50

11 RL.H-11 ICP90A 7.15 <30 480 5 0.7 <10 10 <10 <10 1.54 4.3 90 40 0.17 330 <10 <10 0.02 20 <50 <5 <50

12 ZK1 RL.H-12 23.97 1.27 1.27 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 4.68 50 160 <5 2.8 <10 300 70 170 22 1.1 <10 30 2.43 3030 <10 150 0.04 20 <50 16 <50

13 ZK1 RL.H-13 25.33 1.36 1.30 96 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 2.84 <30 130 <5 3 <10 240 50 280 26.3 0.4 <10 20 2.86 3850 <10 100 0.06 <20 <50 11 <50

14 ZK1 RL.H-14 26.52 1.19 1.14 96 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.33 50 20 <5 4 <10 200 30 100 27.3 0.2 <10 <10 3.27 4270 <10 60 0.08 <20 <50 <5 <50

15 ZK1 RL.H-15 27.92 1.40 1.40 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 2.14 <30 50 <5 2.4 <10 140 50 310 27.6 0.1 <10 <10 2.55 3600 <10 120 0.08 <20 <50 6 <50

16 ZK1 RL.H-16 29.57 1.65 1.65 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 0.68 <30 10 <5 3.3 <10 40 <10 40 24.9 <0.1 <10 <10 2.93 4390 <10 30 0.06 <20 <50 <5 <50

17 ZK1 RL.H-17 30.86 1.29 1.20 93 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 7.7 80 130 <5 2.2 <10 320 70 200 14 0.7 30 50 1.58 2010 <10 160 0.04 30 <50 20 <50

18 ZK1 RL.H-18 32.26 1.40 1.30 93 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 9.98 <30 230 <5 3.1 <10 220 50 330 7.43 1.2 60 50 1.53 950 <10 100 0.05 40 <50 20 <50

19 ZK1 RL.H-19 33.66 1.40 1.33 95 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 7.82 <30 190 <5 3.2 <10 230 90 550 11.1 1 20 40 1.65 1170 <10 170 0.05 60 <50 19 <50

20 ZK1 RL.H-20 34.92 1.26 1.20 95 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 4.12 80 80 <5 2.2 <10 180 80 1960 13.2 0.6 <10 30 1.47 1270 <10 140 0.02 30 <50 14 <50

21 ZK1 RL.H-21 36.09 1.17 1.14 97 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 4.44 90 80 <5 2.1 <10 220 110 610 17 0.8 <10 30 1.94 1860 <10 200 0.03 50 <50 13 <50

22 RL.H-22 ICP90A 7.4 100 590 <5 0.8 20 30 20 4450 4.85 4.8 10 10 0.88 520 170 30 0.1 2080 70 12 260

23 ZK1 RL.H-23 37.41 1.32 1.32 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 5.84 <30 130 <5 1 <10 300 80 370 15.3 1 10 50 1.19 1840 <10 140 0.04 40 <50 18 <50

24 ZK1 RL.H-24 38.71 1.30 1.30 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 4.74 80 140 <5 0.7 <10 110 120 560 22.7 0.9 10 30 0.77 1070 <10 230 0.03 50 <50 12 <50

25 ZK1 RL.H-25 39.76 1.05 1.05 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 3.89 70 110 <5 1.1 <10 110 120 690 24.9 0.7 <10 20 1.2 1360 <10 210 0.02 50 <50 12 <50

26 ZK1 RL.H-26 40.91 1.15 1.15 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 0.56 <30 <10 <5 2 <10 30 20 100 10.5 <0.1 <10 <10 1.58 2030 <10 30 0.03 <20 <50 <5 <50

27 ZK1 RL.H-27 42.29 1.38 1.35 98 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 0.89 <30 10 <5 3 <10 40 20 100 18.5 <0.1 <10 <10 2.72 3580 <10 40 0.05 <20 <50 <5 <50

28 ZK1 RL.H-28 43.51 1.22 1.15 94 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 5.81 40 100 <5 2.8 <10 290 50 150 15.5 0.8 10 50 2.04 2590 <10 110 0.03 <20 <50 16 <50

29 ZK1 RL.H-29 44.81 1.30 1.23 94 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 8.09 <30 270 <5 1.2 <10 300 80 440 14.6 1.7 20 60 1.36 1750 <10 170 0.04 30 <50 22 <50

30 ZK1 RL.H-30 45.91 1.10 1.10 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 2 <30 <10 <5 3.1 <10 130 60 240 20.4 0.2 <10 10 2.17 3180 <10 180 0.03 <20 <50 <5 <50

31 ZK1 RL.H-31 46.91 1.00 1.00 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 3.52 <30 60 <5 2.1 <10 250 50 540 22 0.2 <10 20 1.83 2880 <10 160 0.03 <20 <50 11 <50

32 ZK1 RL.H-32 47.85 0.94 0.94 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 4.17 <30 <10 <5 1.8 <10 310 40 290 22.6 <0.1 <10 20 2.08 4340 <10 130 0.04 <20 <50 13 <50

33 RL.H-33 ICP90A FAI323 Au AAS21E Ag 6.96 <30 380 <5 0.7 <10 10 <10 20 1.78 4.2 80 40 0.16 360 <10 <10 0.02 30 <50 <5 <50

34 ZK1 RL.H-34 49.07 1.22 1.22 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 2.09 <30 20 <5 2.8 <10 140 30 130 17.8 0.1 <10 10 2.27 2990 <10 90 0.05 <20 <50 6 <50

35 ZK1 RL.H-35 50.42 1.35 1.35 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 2.69 <30 100 <5 1.9 <10 190 40 360 17.3 0.5 <10 20 1.76 1940 <10 120 0.05 <20 <50 9 <50

36 ZK1 RL.H-36 51.87 1.45 1.44 99 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.98 <30 20 <5 3.6 <10 240 30 370 15.4 0.2 <10 10 2.27 3100 <10 100 0.05 <20 <50 7 <50

37 ZK1 RL.H-37 53.26 1.39 1.38 99 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.32 <30 <10 <5 1.9 <10 60 10 40 20.3 <0.1 <10 <10 1.98 5080 <10 50 0.03 <20 <50 <5 <50

38 ZK1 RL.H-38 54.56 1.30 1.30 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 0.77 <30 120 <5 2.1 <10 170 <10 10 17.7 0.2 <10 <10 2.59 5080 <10 70 0.03 <20 <50 <5 <50

39 ZK1 RL.H-39 56.01 1.45 1.45 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.8 <30 280 <5 3 <10 310 10 30 15.9 0.3 <10 10 3.32 4370 <10 100 0.05 <20 <50 6 <50

40 ZK1 RL.H-40 57.34 1.33 1.33 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 3.1 <30 80 <5 5.1 <10 140 10 70 9.38 0.3 <10 20 2.47 3130 10 50 0.04 <20 <50 7 <50

41 ZK1 RL.H-41 58.74 1.40 1.40 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 5.29 80 110 <5 2.5 <10 90 50 230 17.6 0.6 30 30 1.14 1330 <10 170 0.05 20 <50 11 <50

42 ZK1 RL.H-42 60.05 1.31 1.31 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 5.62 40 100 <5 2.4 <10 350 170 680 17.4 0.7 <10 30 1.31 1290 <10 260 0.04 30 <50 17 <50

43 ZK1 RL.H-43 61.25 1.20 1.20 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 8.38 <30 170 <5 2 <10 470 40 430 9.51 1.2 20 50 1.36 1600 <10 190 0.02 20 <50 25 <50

44 RL.H-44 ICP90A 6.06 460 1520 <5 2.6 60 350 30 25900 6.75 2.4 20 20 1.89 940 1280 260 0.13 7850 90 12 110

45 ZK1 RL.H-45 62.55 1.30 1.30 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 6.79 60 140 <5 2.4 <10 460 110 480 17.2 0.9 <10 40 1.39 1260 <10 260 0.03 20 <50 24 <50

46 ZK1 RL.H-46 63.95 1.40 1.40 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.86 <30 40 <5 4.3 <10 150 90 390 16.1 0.4 <10 10 2.22 2800 <10 160 0.05 <20 <50 8 <50

47 ZK1 RL.H-47 65.50 1.55 1.55 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 6.18 40 180 <5 14.6 <10 380 50 180 6.86 2.2 <10 20 2.3 3370 <10 130 0.04 <20 <50 32 <50

48 ZK1 RL.H-48 66.90 1.40 1.40 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 6.73 30 240 <5 7.6 <10 410 50 100 8.46 1.8 10 20 2.6 2510 <10 170 0.06 <20 <50 28 <50

49 ZK1 RL.H-49 68.11 1.21 1.20 98 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 7.82 <30 180 <5 3.4 <10 550 70 310 12 1.6 10 30 1.49 1350 <10 140 0.02 <20 <50 28 <50

50 ZK1 RL.H-50 69.19 1.08 1.06 98 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 7.69 30 140 <5 3.2 <10 680 50 140 11.1 1.4 10 30 1.48 1500 <10 130 0.02 <20 <50 31 <50

51 ZK1 RL.H-51 70.39 1.20 1.15 96 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 6.92 <30 130 <5 3.3 <10 420 70 130 13.3 1.2 <10 20 1.57 1710 <10 150 0.04 <20 <50 26 <50

52 ZK1 RL.H-52 71.58 1.19 1.14 96 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 5.36 <30 80 <5 2.9 <10 210 40 130 10.2 0.6 10 20 1.15 1480 <10 110 0.01 <20 <50 16 <50

53 ZK1 RL.H-53 72.91 1.33 1.30 98 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 5.91 <30 90 <5 2.4 <10 230 40 100 11.8 0.8 <10 20 1.02 1270 <10 130 0.03 20 <50 18 <50

54 ZK1 RL.H-54 74.13 1.22 1.22 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 9.64 <30 170 <5 2.4 <10 420 30 140 6.57 1.5 10 50 1.26 1880 <10 170 0.04 <20 <50 34 <50

55 RL.H-55 ICP90A 7.18 <30 380 <5 0.7 <10 <10 <10 <10 1.54 4.5 90 40 0.16 320 <10 10 0.01 20 <50 <5 <50

56 ZK1 RL.H-56 75.29 1.16 1.16 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 3.22 <30 80 <5 7.4 <10 140 50 190 19.5 0.6 <10 20 2.83 3780 <10 170 0.02 <20 <50 16 <50

57 ZK1 RL.H-57 76.59 1.30 1.30 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 2 30 10 <5 6.3 <10 130 110 210 22.2 0.2 <10 <10 2.53 4090 50 190 0.01 <20 <50 8 <50

58 ZK1 RL.H-58 77.79 1.20 1.20 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.53 <30 20 <5 4.2 <10 100 20 80 8.18 0.2 <10 <10 1.66 2680 <10 70 0.01 <20 <50 5 <50

59 ZK1 RL.H-59 78.94 1.15 1.15 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 0.24 <30 <10 <5 6.3 <10 20 20 70 8.49 <0.1 <10 <10 2.43 3960 <10 70 0.03 <20 <50 <5 <50

60 ZK1 RL.H-60 80.04 1.10 1.10 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.81 <30 <10 <5 8.6 <10 100 20 120 14.8 <0.1 <10 <10 3.4 5970 <10 130 0.01 <20 <50 6 <50

61 ZK1 RL.H-61 81.08 1.04 1.04 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 1.79 <30 <10 <5 6.1 <10 70 40 130 15.6 <0.1 <10 <10 2.53 4870 <10 140 0.01 <20 <50 5 <50

62 ZK1 RL.H-62 82.28 1.20 1.20 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 4.41 <30 30 <5 6.4 <10 90 20 110 12.9 0.4 <10 10 2.6 4900 <10 120 0.03 <20 <50 10 <50

63 ZK1 RL.H-63 83.48 1.20 1.20 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 7.98 30 130 <5 2 <10 310 40 60 6.41 1.5 20 50 0.9 1110 <10 140 0.03 <20 <50 21 <50

64 ZK1 RL.H-64 84.94 1.46 1.46 100 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 6.77 30 90 <5 2.1 <10 190 40 90 6.71 0.8 10 40 0.9 1200 <10 140 0.03 <20 <50 21 <50

65 ZK1 RL.H-65 86.57 1.63 1.60 98 42/2 磁黄铁矿化含铁（变）火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 4.93 <30 80 <5 3.1 <10 170 30 70 5.77 0.4 <10 20 1.16 1750 <10 110 0.02 <20 <50 19 <50

66 RL.H-66 ICP90A FAI323 Au AAS21E Ag 7.45 100 590 <5 0.7 20 30 20 4500 4.76 4.7 10 10 0.88 520 180 30 0.09 2120 70 12 270

67 ZK1 RL.H-67 87.91 1.34 1.30 98 42/2 (变）安山岩/(Altered) Andesite ICP90A 8 <30 180 <5 7.8 <10 120 30 70 7.29 0.5 10 20 3.81 2740 <10 70 0.1 <20 <50 23 <50

68 ZK1 RL.H-68 89.03 1.12 1.10 98 42/2 (变）安山岩/(Altered) Andesite ICP90A 5.21 <30 210 <5 9.2 <10 190 50 110 7.84 0.5 <10 <10 3.35 3940 <10 200 0.02 <20 <50 23 <50

69 ZK2 RL.H-69 13.58 14.74 1.16 1.16 100 42/2 (变）安山岩/(Altered) Andesite ICP90A 8.11 <30 20 <5 7.8 <10 280 50 120 9.34 0.2 <10 40 4.25 1780 <10 130 0.03 <20 <50 42 <50

70 ZK2 RL.H-70 15.94 1.20 1.20 100 42/2 (变）安山岩/(Altered) Andesite ICP90A FAI323 Au AAS21E Ag 7.93 <30 10 <5 8.9 <10 270 50 130 8.85 <0.1 <10 20 3.93 1700 <10 120 0.03 <20 <50 40 <50

71 ZK2 RL.H-71 19.36 20.38 1.02 1.02 100 42/2 (变）安山岩/(Altered) Andesite ICP90A 7.75 <30 40 <5 12.5 <10 270 50 170 6.41 0.1 <10 10 2.2 1720 <10 140 0.04 <20 <50 38 <50

72 ZK2 RL.H-72 21.48 1.10 1.10 100 42/2 (变）安山岩/(Altered) Andesite ICP90A 8.75 <30 820 <5 3.9 <10 100 70 360 6.79 1.9 20 30 2.35 760 <10 120 0.12 <20 <50 21 <50

73 ZK2 RL.H-73 91.08 92.23 1.15 1.15 100 42/2 (变）安山岩/(Altered) Andesite ICP90A 7.76 <30 50 <5 8.9 <10 360 50 150 7.07 0.2 <10 20 4.37 1690 <10 80 0.01 <20 <50 44 <50

74 ZK2 RL.H-74 121.87 123.44 1.57 1.40 89 42/2 (变）安山岩/(Altered) Andesite ICP90A FAI323 Au AAS21E Ag 4.58 <30 40 6 18.4 <10 90 30 120 4.71 0.3 <10 30 2.8 2940 <10 50 0.04 <20 <50 27 <50

75 ZK3 RL.H-75 7.67 9.17 1.50 1.50 100 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Mineralization (altered),Andesite ICP90A 6.1 <30 180 <5 8 <10 160 130 1350 13.1 0.6 <10 30 3.15 1970 <10 190 0.01 <20 <50 34 <50

76 ZK3 RL.H-76 10.67 1.50 1.50 100 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Mineralization (altered),Andesite ICP90A 7.45 <30 90 <5 9.9 <10 210 50 130 8.45 0.5 <10 20 3.61 2040 <10 160 0.02 <20 <50 41 <50

77 RL.H-77 ICP90A 6.82 <30 400 5 0.8 <10 40 <10 <10 1.42 4.3 80 40 0.19 320 <10 <10 0.02 <20 <50 <5 <50

78 ZK3 RL.H-78 78.72 80.02 1.30 1.30 100 42/2 (变）安山岩/(Altered) Andesite ICP90A 6.36 <30 160 <5 11.7 <10 180 40 190 7.63 0.4 <10 20 3.5 1920 <10 100 0.01 <20 <50 34 <50

79 ZK3 RL.H-79 81.22 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.74 <30 230 <5 6 <10 150 50 460 7.79 1.6 <10 20 2.06 1030 <10 90 0.04 <20 <50 29 <50

80 ZK3 RL.H-80 82.52 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 6.44 <30 140 <5 3 <10 80 120 630 11.1 1.2 20 20 1.37 570 <10 110 0.03 30 <50 10 <50

81 ZK3 RL.H-81 83.82 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 7.97 <30 200 <5 3.8 <10 210 60 620 7.32 2.1 20 20 1.86 600 <10 80 0.04 30 <50 17 <50

82 ZK3 RL.H-82 85.16 1.34 1.33 99 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.09 40 240 <5 3.4 <10 100 70 710 6.28 2.1 10 10 1.69 610 <10 90 0.03 40 <50 19 <50

83 ZK3 RL.H-83 86.47 1.31 1.30 99 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 10.6 80 350 <5 5.5 <10 190 60 320 4.52 2.7 10 20 3.37 630 <10 90 0.03 <20 <50 43 <50

84 ZK3 RL.H-84 87.68 1.21 1.20 99 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 4.74 350 140 <5 2.6 <10 60 40 170 4.69 1.1 10 60 1.65 430 <10 50 0.02 <20 <50 8 <50

85 ZK3 RL.H-85 88.68 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.22 70 220 <5 1.8 <10 60 30 130 7.5 2 10 80 2.18 540 <10 70 0.05 <20 <50 15 <50

86 ZK3 RL.H-86 89.59 0.91 0.91 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 2.82 <30 110 <5 6.2 <10 110 30 290 14.7 0.6 <10 <10 3.86 1800 <10 100 0.07 <20 <50 6 <50

87 ZK3 RL.H-87 90.52 0.93 0.93 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.38 <30 600 <5 5 <10 800 40 70 7.52 1.4 30 10 7.54 1230 <10 430 0.16 <20 <50 19 <50

88 RL.H-88 ICP90A FAI323 Au AAS21E Ag 5.81 460 1480 <5 2.6 60 380 30 24700 6.73 2.4 20 20 1.8 920 1250 350 0.13 7720 80 12 110

89 ZK3 RL.H-89 91.83 1.31 1.30 99 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 5.69 80 170 <5 1 <10 80 90 670 8.62 1.5 10 40 1.86 330 <10 90 0.04 30 <50 12 <50

90 ZK3 RL.H-90 92.96 1.13 1.12 99 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.6 40 300 <5 2 <10 90 100 990 7.92 2.9 20 10 1.35 510 <10 120 0.06 30 <50 18 <50

91 ZK3 RL.H-91 94.01 1.05 1.02 97 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 7.22 <30 270 <5 2.2 <10 70 60 560 12 2.6 20 20 1.84 1520 <10 100 0.04 30 <50 16 <50

92 ZK3 RL.H-92 95.45 1.44 1.40 97 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 0.42 <30 <10 <5 2.6 <10 60 <10 70 18.8 <0.1 <10 <10 2.38 2660 <10 20 0.06 <20 <50 <5 <50

93 ZK3 RL.H-93 96.61 1.16 1.10 95 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 0.94 <30 10 <5 5 <10 20 10 160 17.2 0.2 <10 <10 2.83 2990 <10 20 0.04 <20 <50 <5 <50

94 ZK3 RL.H-94 97.87 1.26 1.20 95 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.49 <30 320 <5 1.3 <10 30 30 220 6.2 3.7 20 <10 0.84 540 <10 130 0.08 <20 <50 11 <50

分析结果/Assay Result

基本析样品取样及分析结果登记表

取样位置Sampling location (m)

Sample Log

分析方法/Assay Method

正元国际矿业有限公司W W W . C N Z I M C . C O M

正元国际矿业有限公司W W W . C N Z I M C . C O M

第 1 页，共 10 页

序号 工程编号 送样编号 岩矿心长 采取率 采样规格 样品重量 岩（矿）石 名 称采

样日

期

No. DH No.Sample

No.to Lab自

(From)至

(To)样长

(Length)

Length of

core (m)

Recovery

factor(%)Size(mm) Weight(kg) Rock/Ore type

Samp

ling

date

ME Au AgAl

%

As

ppm

Ba

ppm

Be

ppm

Ca

%

Cd

ppm

Cr

ppm

Co

ppm

Cu

ppm

Fe

%

K

%

La

ppm

Li

ppm

Mg

%

Mn

ppm

Mo

ppm

Ni

ppm

P

%

Pb

ppm

Sb

ppm

Sc

ppm

Sn

ppm

分析结果/Assay Result

基本析样品取样及分析结果登记表

取样位置Sampling location (m)

Sample Log

分析方法/Assay Method

正元国际矿业有限公司W W W . C N Z I M C . C O M

正元国际矿业有限公司W W W . C N Z I M C . C O M

95 ZK3 RL.H-95 99.06 1.19 1.13 95 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.49 <30 360 <5 1.1 <10 60 40 280 5.86 3.7 20 10 0.99 340 <10 110 0.05 <20 <50 12 <50

96 ZK3 RL.H-96 100.08 1.02 1.00 98 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.36 50 420 <5 1.1 <10 90 40 310 4.87 4.1 20 10 0.98 350 <10 140 0.05 30 <50 15 <50

97 ZK3 RL.H-97 101.10 1.02 1.00 98 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 6.54 40 370 <5 1.3 <10 120 50 470 6.06 3.3 20 10 1.36 530 <10 140 0.03 <20 <50 14 <50

98 ZK3 RL.H-98 102.11 1.01 1.00 99 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.6 <30 340 <5 1 <10 60 30 260 6.24 3.4 30 10 1.32 420 <10 80 0.05 <20 <50 12 <50

99 RL.H-99 ICP90A 6.9 <30 480 <5 0.8 <10 20 <10 <10 1.29 4.3 80 40 0.15 300 <10 <10 0.02 <20 <50 <5 <50

100 ZK3 RL.H-100 103.46 1.35 1.35 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.18 <30 380 <5 1.4 <10 110 30 130 5.13 3.7 30 20 1.41 420 <10 90 0.05 <20 <50 13 <50

101 ZK3 RL.H-101 104.86 1.40 1.40 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.17 <30 390 <5 0.7 <10 100 40 620 5.15 3.9 20 20 1.43 340 <10 100 0.04 <20 <50 13 <50

102 ZK3 RL.H-102 106.29 1.43 1.40 98 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.15 <30 450 <5 1.6 <10 100 60 300 5.88 4.2 20 10 1.47 410 <10 120 0.04 <20 <50 14 <50

103 ZK3 RL.H-103 107.80 1.51 1.48 98 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.98 <30 350 <5 2.9 <10 140 60 150 9.7 3.5 20 30 3.01 730 <10 130 0.03 <20 <50 32 <50

104 ZK3 RL.H-104 109.10 1.30 1.27 98 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.87 <30 430 <5 2.3 <10 70 20 260 4.07 3.2 20 10 1.87 480 <10 80 0.06 <20 <50 10 <50

105 ZK3 RL.H-105 110.40 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.36 <30 400 <5 1.6 <10 60 30 180 5.5 3.2 20 10 1.54 830 <10 70 0.04 <20 <50 11 <50

106 ZK3 RL.H-106 111.65 1.25 1.25 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 5.66 <30 280 <5 3.1 <10 80 50 390 7.52 2.6 20 <10 1.61 1230 <10 120 0.04 <20 <50 11 <50

107 ZK3 RL.H-107 112.75 1.10 1.10 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.78 <30 400 <5 1 <10 120 60 210 6.37 3.9 20 20 2.09 520 <10 130 0.05 <20 <50 17 <50

108 ZK3 RL.H-108 113.99 1.24 1.24 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 8.03 <30 500 <5 1 <10 80 30 40 4.52 3.7 20 30 2.15 440 <10 90 0.05 <20 <50 14 <50

109 ZK3 RL.H-109 115.19 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化含铁（变）火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.45 <30 190 <5 5.3 <10 120 30 40 6.33 1.2 <10 20 4.92 1020 <10 100 0.02 <20 <50 24 <50

110 RL.H-110 ICP90A 7.39 100 580 <5 0.9 20 50 20 4450 4.81 4.9 10 10 0.87 530 160 40 0.1 2060 70 11 270

111 ZK3 RL.H-111 116.39 1.20 1.20 100 42/2 (变）安山岩/(Altered) Andesite ICP90A 8.14 <30 300 <5 9 <10 160 50 80 7.58 1.6 <10 10 4.39 1390 <10 130 0.02 <20 <50 38 <50

112 ZK10 RL.H-112 10.67 11.77 1.10 1.10 100 42/2 (变）安山岩/(Altered) Andesite ICP90A 7.43 <30 30 <5 8.1 <10 160 40 40 9.07 0.4 <10 30 3.73 1520 <10 90 0.09 <20 <50 36 <50

113 ZK10 RL.H-113 13.02 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.08 <30 30 <5 7.4 <10 310 50 70 7.83 0.4 <10 30 3.69 1870 <10 110 0.03 <20 <50 42 <50

114 ZK10 RL.H-114 14.46 1.44 1.40 97 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.79 <30 40 <5 6.9 <10 300 50 90 8.15 0.5 <10 40 3.98 1960 <10 110 0.02 <20 <50 41 <50

115 ZK10 RL.H-115 15.85 1.39 1.30 94 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.9 <30 40 <5 8.5 <10 310 50 160 7.95 0.5 <10 30 3.41 2200 <10 110 0.02 <20 <50 41 <50

116 ZK10 RL.H-116 17.07 1.22 1.15 94 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.9 <30 10 <5 12 <10 300 40 60 7.44 0.2 <10 20 2.97 2600 10 110 0.02 <20 <50 41 <50

117 ZK10 RL.H-117 18.29 1.22 1.20 98 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.57 <30 20 <5 8.2 <10 280 50 80 6.81 0.2 <10 20 3 1840 20 110 0.01 <20 <50 40 <50

118 ZK10 RL.H-118 19.66 1.37 1.35 98 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.06 <30 50 <5 9 <10 310 50 60 7.34 0.4 <10 20 3.16 2010 10 110 0.02 <20 <50 43 <50

119 ZK10 RL.H-119 20.66 1.00 1.00 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.73 <30 20 <5 10.5 <10 280 40 50 7.52 0.3 <10 20 3.09 2270 30 110 0.02 <20 <50 38 <50

120 ZK10 RL.H-120 20.99 0.33 0.33 100 42/2 块状硫化物 VMS ICP90A 1.69 <30 <10 <5 2.6 <10 130 100 840 >30 <0.1 <10 <10 0.49 500 70 100 <0.01 <20 <50 <5 <50

121 RL.H-121 ICP90A 6.95 <30 470 <5 0.9 <10 20 <10 <10 1.35 4.2 70 40 0.17 300 10 <10 0.01 <20 <50 <5 <50

122 ZK10 RL.H-122 22.06 1.07 1.07 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 6.37 <30 60 <5 7.8 <10 170 20 230 7.09 0.6 <10 20 3.08 1360 140 70 0.03 <20 <50 30 <50

123 ZK10 RL.H-123 23.31 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.94 <30 50 <5 8.2 <10 210 40 150 7.44 0.8 <10 40 3.96 1490 <10 90 0.02 <20 <50 40 <50

124 ZK10 RL.H-124 24.66 1.35 1.35 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.76 <30 80 <5 7.9 <10 330 50 80 8.08 1.7 <10 60 4.83 1460 20 120 0.02 <20 <50 40 <50

125 ZK10 RL.H-125 26.00 1.34 1.34 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.56 <30 20 <5 8.4 <10 280 40 90 8.05 0.6 <10 30 4.51 1570 <10 110 0.02 <20 <50 40 <50

126 ZK10 RL.H-126 26.94 0.94 0.94 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 7.96 <30 300 <5 3.1 <10 10 <10 <10 1.42 1.8 10 40 0.92 300 <10 10 0.03 <20 <50 <5 <50

127 ZK10 RL.H-127 27.94 1.00 1.00 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 7.89 <30 340 <5 3.2 <10 100 <10 <10 1.37 1.6 <10 40 0.94 320 <10 <10 0.03 <20 <50 <5 <50

128 ZK10 RL.H-128 28.96 1.02 1.02 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.16 <30 10 <5 11.5 <10 260 40 40 7.37 0.2 <10 20 3.97 2110 <10 90 0.02 <20 <50 40 <50

129 ZK10 RL.H-129 30.20 1.24 1.24 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.75 <30 10 <5 9.4 <10 270 40 100 7.88 0.4 <10 20 3.75 1700 30 100 0.02 <20 <50 41 <50

130 ZK10 RL.H-130 31.50 1.30 1.30 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.64 <30 20 <5 9.6 <10 250 30 90 7.08 0.4 <10 30 3.48 1460 <10 80 0.02 <20 <50 38 <50

131 ZK10 RL.H-131 32.60 1.10 1.10 100 42/2 块状硫化物/VMS ICP90A FAI323 Au AAS21E Ag 2.34 50 30 <5 3.7 <10 60 120 2200 >30 0.4 <10 20 1.92 880 80 140 0.01 <20 <50 16 <50

132 RL.H-132 ICP90A 5.91 460 1460 <5 2.7 60 370 30 25700 6.67 2.4 20 20 1.84 940 1260 260 0.13 7840 90 12 110

133 ZK10 RL.H-133 33.52 0.92 0.92 100 42/2 块状硫化物/VMS ICP90A FAI323 Au AAS21E Ag 1.6 90 10 <5 4 <10 60 100 5540 >30 0.2 <10 <10 1.63 720 110 120 <0.01 40 <50 8 <50

134 ZK10 RL.H-134 35.05 1.53 1.53 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.06 <30 60 <5 8.5 <10 300 40 190 7.71 0.6 <10 20 3.9 1730 <10 110 0.04 <20 <50 44 <50

135 ZK10 RL.H-135 36.15 1.10 1.10 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.65 <30 100 <5 8.3 <10 250 30 260 7.08 0.9 <10 40 4.48 1710 10 90 0.02 <20 <50 48 <50

136 ZK10 RL.H-136 37.35 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.48 <30 70 <5 7.8 <10 310 40 60 5.89 0.6 <10 20 4.37 1340 30 100 0.03 <20 <50 46 <50

137 ZK10 RL.H-137 38.70 1.35 1.35 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.31 <30 80 <5 6.9 <10 260 30 350 7.47 0.6 <10 20 3.85 1300 <10 100 0.02 <20 <50 35 <50

138 ZK10 RL.H-138 39.97 1.27 1.27 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.75 <30 40 <5 8.8 <10 290 40 120 7.27 0.4 <10 20 3.95 1580 <10 90 0.03 <20 <50 42 <50

139 ZK10 RL.H-139 41.15 1.18 1.18 100 42/2 块状硫化物/VMS ICP90A FAI323 Au AAS21E Ag 0.44 120 <10 <5 2 <10 10 230 1860 >30 <0.1 <10 <10 0.35 330 20 140 <0.01 20 <50 <5 <50

140 ZK10 RL.H-140 42.05 0.90 0.90 100 42/2 块状硫化物/VMS ICP90A 1.38 <30 30 <5 4 <10 30 80 7560 >30 0.3 <10 10 2.03 910 60 430 0.01 40 <50 <5 <50

141 ZK10 RL.H-141 43.05 1.00 1.00 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 7.24 <30 30 <5 1 <10 <10 <10 180 1.05 1.5 <10 <10 0.04 190 <10 <10 <0.01 20 <50 7 <50

142 ZK10 RL.H-142 44.00 0.95 0.95 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 6.66 <30 30 <5 1.3 <10 30 <10 180 0.92 2.1 <10 <10 0.04 330 <10 <10 <0.01 30 <50 6 <50

143 RL.H-143 ICP90A FAI323 Au AAS21E Ag 6.87 <30 420 <5 1.3 <10 30 <10 20 1.16 4.1 70 40 0.14 280 <10 <10 0.02 20 <50 <5 <50

144 ZK10 RL.H-144 45.04 1.04 1.04 100 42/2 块状硫化物/VMS ICP90A FAI323 Au AAS21E Ag 0.74 90 10 <5 3.9 <10 10 140 1930 >30 0.4 <10 <10 2.11 860 30 190 <0.01 30 <50 6 <50

145 ZK10 RL.H-145 46.29 1.25 1.25 100 42/2 块状硫化物/VMS ICP90A 0.92 80 <10 <5 2.6 <10 30 150 3410 >30 0.1 <10 <10 1.15 580 180 240 <0.01 50 <50 <5 <50

146 ZK10 RL.H-146 47.74 1.45 1.45 100 42/2 块状硫化物/VMS ICP90A FAI323 Au AAS21E Ag 0.95 <30 <10 <5 2 <10 10 80 4470 >30 0.5 <10 20 1.5 900 50 500 <0.01 40 <50 8 <50

147 ZK10 RL.H-147 48.84 1.10 1.10 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 5.69 <30 10 8 7.8 <10 110 20 640 9.51 0.8 <10 40 5.52 3140 <10 60 0.03 <20 <50 52 <50

148 ZK10 RL.H-148 50.29 1.45 1.45 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 5.19 <30 40 15 11.4 <10 80 20 360 5.91 0.9 <10 30 5.37 2870 <10 30 0.04 <20 <50 16 <50

149 ZK11 RL.H-149 15.31 16.51 1.20 1.20 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 6.76 <30 560 5 5.7 <10 480 40 40 6.53 1.5 20 70 6.1 1170 <10 290 0.15 <20 <50 19 <50

150 ZK11 RL.H-150 17.71 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.56 <30 140 7 6 <10 320 100 200 7.64 0.9 <10 30 3.24 1080 <10 380 0.03 <20 <50 39 <50

151 ZK11 RL.H-151 18.86 1.15 1.15 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.99 <30 80 8 7.9 <10 320 80 200 6.43 0.6 <10 20 2.65 1070 <10 280 0.03 <20 <50 41 <50

152 ZK11 RL.H-152 19.81 0.95 0.95 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.9 <30 130 6 7.5 <10 340 80 290 6.59 1.1 <10 40 2.99 1150 20 330 0.03 70 <50 40 <50

153 ZK11 RL.H-153 21.11 1.30 1.30 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 6.69 <30 40 9 11.6 <10 230 50 250 8.65 0.3 <10 20 4.05 1890 30 290 0.03 20 <50 30 <50

154 RL.H-154 ICP90A 7.48 100 590 <5 0.7 20 40 20 4440 4.89 4.7 10 10 0.9 540 200 30 0.09 2070 60 12 260

155 ZK11 RL.H-155 22.31 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.68 <30 80 6 4.5 <10 220 50 570 8.03 0.7 <10 40 1.76 650 40 230 0.02 30 <50 33 <50

156 ZK11 RL.H-156 23.61 1.30 1.30 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.06 <30 70 8 5 <10 240 80 370 6.95 0.8 <10 40 1.85 810 10 210 0.03 <20 <50 32 <50

157 ZK11 RL.H-157 24.71 1.10 1.10 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.07 <30 60 8 3.8 <10 260 70 410 6.59 0.7 <10 50 1.8 710 <10 270 0.03 <20 <50 33 <50

158 ZK11 RL.H-158 25.91 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.35 <30 30 7 5.6 <10 300 90 220 8.59 0.3 <10 30 2.43 1000 <10 370 0.02 <20 <50 38 <50

159 ZK11 RL.H-159 27.26 1.35 1.35 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.15 <30 40 6 4.4 <10 290 80 290 8.85 0.3 <10 30 2.78 930 <10 420 0.03 <20 <50 38 <50

160 ZK11 RL.H-160 28.41 1.15 1.15 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.2 <30 60 <5 5.6 <10 270 120 250 13.7 0.4 <10 30 2.04 810 <10 420 0.03 <20 <50 33 <50

161 ZK11 RL.H-161 29.66 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.78 <30 70 5 7.6 <10 310 70 240 9.21 0.4 <10 30 1.8 940 40 320 0.03 <20 <50 37 <50

162 ZK11 RL.H-162 30.86 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.47 <30 100 5 6.5 <10 190 40 260 8.19 0.3 <10 20 0.87 760 20 300 0.03 <20 <50 22 <50

163 ZK11 RL.H-163 32.00 1.14 1.14 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.97 <30 130 7 4.7 <10 90 10 130 3.7 0.6 <10 30 1.03 520 <10 100 0.05 <20 <50 11 <50

164 ZK11 RL.H-164 33.10 1.10 1.10 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.34 <30 120 7 6 <10 210 130 710 11.8 0.6 <10 40 2.22 890 <10 440 0.05 <20 <50 28 <50

165 RL.H-165 ICP90A 7.04 <30 370 8 0.9 <10 10 <10 10 1.74 4.3 80 40 0.16 340 <10 <10 0.01 <20 <50 <5 <50

166 ZK11 RL.H-166 34.40 1.30 1.30 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.41 <30 80 5 8.6 <10 280 100 320 12.5 0.3 <10 20 2.11 1200 30 390 0.03 <20 <50 36 <50

167 ZK11 RL.H-167 35.75 1.35 1.35 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.25 <30 50 <5 8.3 <10 290 80 240 9.35 0.4 <10 30 2.64 1260 <10 270 0.04 <20 <50 38 <50

168 ZK11 RL.H-168 36.95 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.2 <30 30 <5 6.8 <10 270 150 330 13.8 0.3 <10 30 2.22 980 20 420 0.02 <20 <50 35 <50

169 ZK11 RL.H-169 38.10 1.15 1.15 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.13 <30 30 5 7.7 <10 310 70 210 8.92 0.3 <10 20 2.71 1140 <10 300 0.02 <20 <50 40 <50

170 ZK11 RL.H-170 39.35 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.25 <30 60 <5 7 <10 300 70 270 8.96 0.6 <10 40 2.29 1090 20 260 0.02 <20 <50 39 <50

171 ZK11 RL.H-171 40.65 1.30 1.30 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.46 <30 40 7 9 <10 280 90 240 10.7 0.2 <10 20 1.66 1250 <10 270 0.02 <20 <50 36 <50

172 ZK11 RL.H-172 41.80 1.15 1.15 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.73 <30 80 6 6.4 <10 320 50 220 7.2 0.6 <10 50 2.34 1010 <10 260 0.03 <20 <50 42 <50

173 ZK11 RL.H-173 43.10 1.30 1.30 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 8.23 <30 80 <5 6.6 <10 310 90 280 9.95 0.5 <10 50 2.61 1170 <10 270 0.02 <20 <50 40 <50

174 ZK11 RL.H-174 44.20 1.10 1.10 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.24 <30 80 6 6.7 <10 310 60 280 8.05 0.4 <10 40 2.16 950 <10 260 0.03 <20 <50 39 <50

175 ZK11 RL.H-175 44.84 0.64 0.64 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.28 <30 60 9 7.5 <10 270 60 260 7.28 0.4 <10 40 2.05 940 10 220 0.02 <20 <50 38 <50

176 RL.H-176 ICP90A 6.05 480 1510 6 2.6 60 370 30 25300 6.83 2.4 20 20 1.91 920 1280 260 0.13 7870 90 12 120

177 ZK11 RL.H-177 46.29 1.45 1.45 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.95 <30 20 7 8.9 <10 200 50 150 9.7 0.4 <10 40 4.44 1810 <10 70 0.03 <20 <50 43 <50

178 ZK11 RL.H-178 47.74 1.45 1.45 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.47 <30 50 <5 8.1 <10 200 40 130 9.35 0.4 <10 30 4.25 1700 <10 70 0.03 <20 <50 42 <50

179 ZK11 RL.H-179 48.99 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.16 <30 160 <5 7.3 <10 200 50 160 7.99 0.9 <10 40 3.79 1430 <10 80 0.02 <20 <50 38 <50

180 ZK11 RL.H-180 50.29 1.30 1.30 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 6.43 <30 130 7 9.5 <10 240 80 730 10.5 0.8 <10 30 1.83 2290 10 180 0.03 <20 <50 37 <50

181 ZK11 RL.H-181 51.44 1.15 1.15 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.22 <30 40 6 7.9 <10 190 40 160 8.9 0.5 <10 20 3.99 1710 <10 70 0.03 <20 <50 40 <50

182 ZK11 RL.H-182 52.59 1.15 1.15 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.06 <30 20 5 8.4 <10 180 30 100 8.25 0.3 <10 20 3.74 1550 <10 60 0.03 <20 <50 39 <50

183 ZK11 RL.H-183 53.74 1.15 1.15 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.41 <30 10 <5 7.9 <10 180 40 90 9.37 0.3 <10 20 4.17 1720 <10 60 0.03 <20 <50 42 <50

184 ZK11 RL.H-184 54.89 1.15 1.15 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.44 <30 30 8 6.6 <10 170 40 140 7.74 0.4 <10 20 3.5 1460 <10 80 0.03 <20 <50 37 <50

185 ZK11 RL.H-185 56.09 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.7 <30 40 8 8.6 <10 280 80 500 9.8 0.3 <10 <10 1.63 1150 20 340 0.03 <20 <50 36 <50

186 ZK11 RL.H-186 57.39 1.30 1.30 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.67 <30 <10 7 5.7 <10 90 190 1100 24.7 0.1 <10 <10 0.61 1040 60 540 0.01 <20 <50 10 <50

187 RL.H-187 ICP90A 7.06 <30 380 14 0.8 <10 20 <10 20 1.56 4.3 80 40 0.16 340 <10 <10 0.03 <20 <50 <5 <50

188 ZK11 RL.H-188 58.39 1.00 1.00 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 6.72 <30 40 9 6.2 <10 150 50 280 10.9 0.4 <10 10 0.7 950 160 250 0.03 <20 <50 23 <50

第 2 页，共 10 页

序号 工程编号 送样编号 岩矿心长 采取率 采样规格 样品重量 岩（矿）石 名 称采

样日

期

No. DH No.Sample

No.to Lab自

(From)至

(To)样长

(Length)

Length of

core (m)

Recovery

factor(%)Size(mm) Weight(kg) Rock/Ore type

Samp

ling

date

ME Au AgAl

%

As

ppm

Ba

ppm

Be

ppm

Ca

%

Cd

ppm

Cr

ppm

Co

ppm

Cu

ppm

Fe

%

K

%

La

ppm

Li

ppm

Mg

%

Mn

ppm

Mo

ppm

Ni

ppm

P

%

Pb

ppm

Sb

ppm

Sc

ppm

Sn

ppm

分析结果/Assay Result

基本析样品取样及分析结果登记表

取样位置Sampling location (m)

Sample Log

分析方法/Assay Method

正元国际矿业有限公司W W W . C N Z I M C . C O M

正元国际矿业有限公司W W W . C N Z I M C . C O M

189 ZK11 RL.H-189 59.44 1.05 1.05 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 5.01 <30 70 7 5.1 <10 150 60 520 13.8 0.5 <10 30 0.68 850 40 340 0.02 <20 <50 22 <50

190 ZK11 RL.H-190 60.44 1.00 1.00 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 1.26 <30 <10 <5 2.2 <10 90 50 280 9.1 0.2 <10 <10 0.28 390 10 180 0.02 <20 <50 5 <50

191 ZK11 RL.H-191 61.44 1.00 1.00 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 1.06 <30 <10 <5 4.8 <10 50 130 970 26.3 <0.1 <10 <10 0.25 800 120 510 <0.01 <20 <50 <5 <50

192 ZK11 RL.H-192 62.48 1.04 1.04 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.09 <30 100 7 8.3 <10 210 40 170 8.22 0.7 <10 20 2.44 1400 <10 110 0.04 <20 <50 34 <50

193 ZK11 RL.H-193 63.73 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.63 <30 60 9 10.2 <10 270 60 280 8.17 0.4 <10 20 1.5 1730 70 190 0.04 <20 <50 32 <50

194 ZK11 RL.H-194 64.98 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.65 <30 70 7 5.5 <10 250 60 370 5.67 0.5 <10 10 0.93 690 <10 180 0.02 <20 <50 30 <50

195 ZK11 RL.H-195 66.23 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.98 <30 60 7 7.4 <10 280 70 360 7.45 0.3 <10 10 1.16 880 <10 240 0.03 <20 <50 34 <50

196 ZK11 RL.H-196 67.38 1.15 1.15 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.16 <30 60 <5 3.8 <10 260 90 920 10.1 0.5 <10 50 2.41 770 <10 370 0.02 <20 <50 33 <50

197 ZK11 RL.H-197 68.58 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.35 <30 80 7 3.9 <10 260 140 1210 11.3 1 <10 30 2.96 910 <10 390 0.03 <20 <50 34 <50

198 RL.H-198 ICP90A 7.39 110 580 <5 0.7 20 40 20 4380 4.91 4.8 10 10 0.87 530 180 30 0.1 2060 70 12 280

199 ZK11 RL.H-199 69.78 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.85 <30 100 7 2.9 <10 290 90 1310 8.78 1.3 <10 50 2.87 560 <10 380 0.03 <20 <50 36 <50

200 ZK11 RL.H-200 70.83 1.05 1.05 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.59 <30 80 5 6 <10 210 60 390 7.65 0.9 <10 30 2.42 1110 <10 160 0.03 <20 <50 35 <50

201 ZK11 RL.H-201 72.75 1.92 1.92 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 7.9 <30 260 <5 1.2 <10 20 <10 20 0.8 2.8 <10 10 0.11 130 <10 <10 <0.01 <20 <50 <5 <50

202 ZK11 RL.H-202 74.00 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.78 <30 50 7 8.1 <10 220 40 70 8.85 0.7 <10 20 4.14 1710 <10 120 0.05 <20 <50 42 <50

203 ZK11 RL.H-203 75.20 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.86 <30 80 <5 4.2 <10 100 110 510 13.7 0.7 <10 10 0.97 680 20 530 0.02 <20 <50 14 <50

204 ZK11 RL.H-204 76.40 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 5.39 <30 270 <5 5 <10 670 140 290 13.6 0.9 10 40 4.21 810 <10 420 0.08 <20 <50 25 <50

205 ZK11 RL.H-205 77.72 1.32 1.32 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.95 <30 90 <5 3 <10 210 60 1420 10.6 0.7 <10 30 2.43 700 <10 340 0.02 <20 <50 41 <50

206 ZK11 RL.H-206 78.92 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.89 <30 80 6 3.2 <10 240 100 280 9.8 0.7 <10 30 2.38 1100 <10 190 0.04 <20 <50 41 <50

207 ZK11 RL.H-207 80.17 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 6.24 <30 130 <5 4 <10 240 100 180 10.9 0.6 <10 20 1.72 690 <10 260 0.02 <20 <50 31 <50

208 ZK11 RL.H-208 81.42 1.25 1.25 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 4.85 <30 360 <5 2.6 <10 200 30 60 5.68 1.4 20 30 2.44 590 <10 180 0.06 <20 <50 16 <50

209 RL.H-209 ICP90A 7.2 <30 380 11 1.2 <10 30 <10 10 1.77 4.4 80 40 0.19 360 <10 <10 0.02 <20 <50 <5 <50

210 ZK11 RL.H-210 82.62 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 6.84 <30 50 <5 8.2 <10 220 40 190 11.3 0.4 <10 <10 1.49 1200 <10 210 0.03 <20 <50 34 <50

211 ZK11 RL.H-211 83.82 1.20 1.20 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 1.76 40 <10 <5 6.9 <10 70 100 180 23.8 <0.1 <10 <10 0.2 1100 10 220 0.01 <20 <50 6 <50

212 ZK11 RL.H-212 84.82 1.00 1.00 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 0.31 <30 <10 <5 2.2 <10 40 70 210 14.8 <0.1 <10 <10 0.04 240 10 160 <0.01 <20 <50 <5 <50

213 ZK11 RL.H-213 85.82 1.00 1.00 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 0.32 <30 <10 <5 1 <10 60 30 150 4.66 <0.1 <10 <10 0.05 260 10 150 <0.01 <20 <50 <5 <50

214 ZK11 RL.H-214 86.87 1.05 1.05 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 2.65 <30 60 <5 1.9 <10 60 20 210 4.33 0.5 <10 <10 0.1 450 <10 190 0.01 <20 <50 <5 <50

215 ZK11 RL.H-215 88.02 1.15 1.15 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 6.67 <30 320 7 1.1 <10 30 <10 30 1.54 1.6 <10 20 0.18 340 <10 10 0.01 <20 <50 <5 <50

216 ZK11 RL.H-216 89.32 1.30 1.30 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.09 <30 300 <5 1.2 <10 20 <10 30 1.02 2.1 <10 10 0.12 250 <10 <10 <0.01 <20 <50 <5 <50

217 ZK12 RL.H-217 4.57 5.85 1.28 1.25 98 42/2 （变）安山岩/(Altered) Andesite ICP90A 6.87 <30 70 <5 6.7 <10 40 50 100 12 0.4 <10 40 2.79 1720 <10 40 0.06 <20 <50 42 <50

218 ZK12 RL.H-218 46.64 48.04 1.40 1.40 100 42/2 弱黄铁矿化（变）安山岩/Weak Pyrite Mienralization (Altered) Andesite ICP90A 7.16 <30 650 <5 8.5 <10 200 40 160 6.79 1.1 70 50 3.66 1330 <10 100 0.14 <20 <50 27 <50

219 ZK12 RL.H-219 60.52 61.52 1.00 1.00 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.67 <30 40 <5 8.1 <10 300 50 100 8.68 0.4 <10 40 5.19 1590 <10 140 0.02 <20 <50 39 <50

220 RL.H-220 ICP90A FAI323 Au AAS21E Ag 6.06 450 1510 <5 2.7 60 380 30 25600 6.92 2.4 20 20 1.89 950 1290 300 0.13 7850 80 12 120

221 ZK12 RL.H-221 61.92 0.40 0.40 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Pyrrhotite&Pyrite Mineralization(altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.33 <30 140 <5 6.6 <10 390 90 630 15.3 0.6 10 20 0.96 940 20 190 0.03 <20 <50 13 <50

222 ZK12 RL.H-222 63.18 1.26 1.26 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.81 <30 410 <5 6.6 <10 180 70 130 5.1 1.2 30 50 2.27 960 <10 250 0.08 <20 <50 28 <50

223 ZK12 RL.H-223 64.48 1.30 1.30 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 8.68 <30 120 <5 6.6 <10 310 60 90 5.89 0.5 10 30 2.93 1310 <10 170 0.05 <20 <50 41 <50

224 ZK12 RL.H-224 66.13 1.65 1.65 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.74 <30 70 <5 6.6 <10 200 40 140 6.99 0.4 <10 30 2.29 1200 <10 110 0.04 <20 <50 35 <50

225 ZK12 RL.H-225 67.33 1.20 1.20 100 42/2 硅化（变）安山岩/Silicified (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 6.11 <30 360 <5 4.9 <10 120 20 40 2.88 1.2 20 10 0.35 570 10 90 0.03 <20 <50 15 <50

226 ZK12 RL.H-226 68.58 1.25 1.25 100 42/2 硅化（变）安山岩/Silicified (Altered) Andesite ICP90A 5.37 <30 340 <5 3.4 <10 50 30 120 3.44 1.6 20 20 0.89 600 <10 80 0.03 <20 <50 13 <50

227 ZK9 RL.H-227 12.38 13.43 1.05 1.05 100 42/2 （变）安山岩/(Altered) Andesite ICP90A FAI323 Au 6.67 <30 140 <5 9.2 <10 220 40 90 7.99 1.6 20 40 4.33 3360 <10 100 0.09 130 <50 32 <50

228 ZK9 RL.H-228 14.63 1.20 1.20 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 6.09 <30 90 <5 7.3 20 90 20 120 7.87 1.8 10 20 2.5 5150 <10 70 0.03 110 <50 18 <50

229 ZK9 RL.H-229 15.83 1.20 1.20 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 4.6 <30 80 <5 8.2 <10 100 30 190 8.59 1.2 10 30 3.04 4840 <10 80 0.03 <20 <50 14 <50

230 ZK9 RL.H-230 17.13 1.30 1.30 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 4.39 <30 80 <5 10.8 30 130 40 120 13.1 0.9 <10 20 3.99 6040 <10 110 0.03 <20 <50 24 <50

231 RL.H-231 ICP90A 7.02 <30 390 <5 0.8 <10 30 <10 <10 2.04 4.3 90 40 0.2 420 10 <10 0.01 <20 <50 <5 <50

232 ZK9 RL.H-232 18.37 1.24 1.24 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 2.51 <30 50 <5 6.8 <10 170 40 150 13.2 0.7 <10 10 2.12 2630 <10 120 0.03 <20 <50 11 <50

233 ZK9 RL.H-233 19.37 1.00 1.00 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 2.72 <30 60 <5 1.6 <10 110 60 210 16.8 1 <10 20 0.79 970 <10 150 0.03 20 <50 7 <50

234 ZK9 RL.H-234 20.42 1.05 1.05 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 0.35 <30 10 <5 2.1 <10 50 10 60 6.35 0.1 <10 <10 0.81 1770 <10 50 <0.01 <20 <50 <5 <50

235 ZK9 RL.H-235 21.62 1.20 1.20 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 0.91 <30 20 <5 3 <10 70 10 40 5.39 0.2 <10 <10 1.18 2870 <10 30 0.01 <20 <50 <5 <50

236 ZK9 RL.H-236 22.82 1.20 1.20 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 1.21 <30 10 <5 4 <10 60 10 80 6.81 0.2 <10 <10 1.92 3950 <10 40 0.02 <20 <50 7 <50

237 ZK9 RL.H-237 23.87 1.05 1.05 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 0.51 <30 <10 <5 4.5 <10 30 30 140 12.4 <0.1 <10 <10 2.01 5070 <10 100 0.03 <20 <50 <5 <50

238 ZK9 RL.H-238 25.12 1.25 1.25 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 1.52 <30 30 <5 1.9 <10 60 30 110 9.43 0.5 <10 <10 0.88 1260 <10 80 0.01 <20 <50 6 <50

239 ZK9 RL.H-239 26.27 1.15 1.15 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 4.28 <30 60 <5 2.4 <10 70 70 220 18.4 1.4 20 10 0.92 910 <10 170 0.03 20 <50 9 <50

240 ZK9 RL.H-240 27.37 1.10 1.10 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 2.67 <30 20 <5 3.1 <10 70 70 260 18.5 0.4 10 20 1.5 1080 <10 170 0.02 <20 <50 6 <50

241 ZK9 RL.H-241 28.57 1.20 1.20 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 5.2 <30 70 <5 1.8 <10 100 80 360 21.3 1.4 10 30 1.15 1010 <10 200 0.05 40 <50 13 <50

242 RL.H-242 ICP90A FAI323 Au AAS21E Ag 7.4 110 590 <5 0.8 20 40 20 4420 4.9 4.8 20 10 0.88 530 160 30 0.1 2110 70 11 280

243 ZK9 RL.H-243 29.57 1.00 1.00 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 2.31 <30 20 <5 1.7 <10 60 90 210 23.2 0.4 <10 10 1.07 650 <10 210 0.01 <20 <50 5 <50

244 ZK9 RL.H-244 30.77 1.20 1.20 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 2.24 <30 10 <5 1.8 <10 50 100 250 25.3 0.3 <10 <10 0.94 650 <10 220 0.02 <20 <50 5 <50

245 ZK9 RL.H-245 31.97 1.20 1.20 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 4.71 <30 30 <5 2.2 <10 70 40 220 12.1 0.6 20 20 2.31 880 <10 110 0.04 <20 <50 9 <50

246 ZK9 RL.H-246 33.17 1.20 1.20 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 5.62 30 50 <5 1.3 <10 80 70 170 18.6 0.6 <10 40 1.95 1130 <10 170 0.03 <20 <50 14 <50

247 ZK9 RL.H-247 34.27 1.10 1.10 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 3.96 <30 70 <5 2.9 <10 70 50 180 14.8 0.7 10 10 1.37 740 <10 130 0.03 <20 <50 9 <50

248 ZK9 RL.H-248 35.51 1.24 1.24 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 6.98 <30 60 <5 5.9 <10 250 40 100 10.7 0.5 10 20 3.63 1600 <10 100 0.08 <20 <50 34 <50

249 ZK9 RL.H-249 36.91 1.40 1.40 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 6.75 <30 70 <5 3.9 <10 120 50 120 12.5 1.4 10 30 2.48 1130 <10 100 0.05 <20 <50 28 <50

250 ZK9 RL.H-250 38.16 1.25 1.25 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 2.72 <30 60 <5 4.2 <10 70 40 110 11 0.7 <10 10 1.34 1460 <10 80 0.02 <20 <50 11 <50

251 ZK9 RL.H-251 39.46 1.30 1.30 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.21 <30 90 <5 7.3 <10 130 40 120 10.3 0.7 <10 20 3.76 1980 <10 50 0.04 <20 <50 44 <50

252 ZK9 RL.H-252 40.66 1.20 1.20 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.43 <30 110 <5 8.5 <10 130 50 140 11 1.6 <10 30 3.05 4890 <10 80 0.06 60 <50 38 <50

253 RL.H-253 ICP90A FAI323 Au 7.12 <30 410 <5 0.8 <10 40 <10 <10 1.72 4.4 90 40 0.18 370 <10 <10 0.02 <20 <50 <5 <50

254 ZK9 RL.H-254 41.76 1.10 1.10 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 6.87 <30 40 <5 9.1 <10 130 40 110 10.4 0.5 <10 20 3.25 2280 <10 60 0.06 <20 <50 35 <50

255 ZK9 RL.H-255 42.96 1.20 1.20 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 6.88 <30 50 <5 9.5 <10 110 40 140 10 0.4 <10 20 2.76 2070 <10 70 0.06 <20 <50 34 <50

256 ZK9 RL.H-256 44.16 1.20 1.20 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.14 <30 <10 <5 6.7 <10 120 50 140 11 0.1 <10 20 3.61 1720 <10 70 0.06 <20 <50 36 <50

257 ZK9 RL.H-257 45.51 1.35 1.35 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.4 <30 10 <5 7.6 <10 120 50 110 10.7 0.1 <10 20 3.42 1870 <10 70 0.06 <20 <50 37 <50

258 ZK9 RL.H-258 46.71 1.20 1.20 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.37 <30 60 <5 8.1 <10 130 40 110 11 0.2 <10 20 3.46 2110 <10 70 0.07 <20 <50 36 <50

259 ZK9 RL.H-259 47.85 1.14 1.14 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.49 <30 260 <5 8.3 <10 140 50 120 10.5 0.6 <10 20 2.85 1920 <10 60 0.07 <20 <50 36 <50

260 ZK9 RL.H-260 49.05 1.20 1.20 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.57 <30 140 <5 7 <10 140 40 120 10.4 0.4 <10 20 3.47 1980 <10 60 0.07 <20 <50 37 <50

261 ZK9 RL.H-261 50.15 1.10 1.10 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.58 <30 180 <5 6.7 <10 270 50 90 9.39 0.5 10 20 4.13 1860 <10 130 0.08 <20 <50 34 <50

262 ZK9 RL.H-262 51.09 0.94 0.94 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.74 <30 200 <5 7.8 <10 240 40 70 7.93 0.7 10 40 3.54 1760 <10 120 0.07 <20 <50 31 <50

263 ZK9 RL.H-263 52.09 1.00 1.00 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.79 <30 80 <5 8.2 <10 130 40 120 10.4 0.7 <10 20 2.97 1840 <10 60 0.07 <20 <50 38 <50

264 RL.H-264 ICP90A FAI323 Au 6.01 460 1510 <5 2.7 60 370 30 25800 6.69 2.4 20 20 1.84 930 1260 250 0.13 7790 80 12 120

265 ZK9 RL.H-265 53.29 1.20 1.20 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization(altered), Andesite ICP90A FAI323 Au 5.96 <30 100 <5 10.1 <10 100 30 170 7.92 1 <10 20 3.35 2110 <10 50 0.05 20 <50 26 <50

266 ZK9 RL.H-266 54.35 1.06 1.06 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization(altered), Andesite ICP90A FAI323 Au 6.72 <30 150 <5 3.9 <10 80 30 140 8.27 2 20 30 1.82 890 <10 70 0.05 <20 <50 20 <50

267 ZK9 RL.H-267 55.70 1.35 1.35 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization(altered), Andesite ICP90A FAI323 Au AAS21E Ag 4.21 <30 130 <5 2 <10 90 50 200 18.3 1.5 20 30 1.07 850 <10 130 0.04 <20 <50 8 <50

268 ZK9 RL.H-268 57.00 1.30 1.30 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization(altered), Andesite ICP90A FAI323 Au AAS21E Ag 0.76 <30 20 <5 2.6 <10 30 50 260 17 0.2 <10 <10 1.53 1210 <10 120 0.02 <20 <50 <5 <50

269 ZK9 RL.H-269 58.00 1.00 1.00 100 42/2 磁黄铁矿化（变）安山岩/Pyrrhotite Mineralization(altered), Andesite ICP90A FAI323 Au 4.53 <30 90 <5 4.9 <10 120 40 270 15 0.6 10 30 2.18 3600 <10 110 0.03 <20 <50 18 <50

270 ZK9 RL.H-270 59.17 1.17 1.17 100 42/2 （变）安山岩/(Altered) Andesite ICP90A FAI323 Au 7.75 <30 150 <5 8.2 <10 320 40 80 9.03 0.5 10 30 4.93 1640 <10 140 0.04 <20 <50 36 <50

271 ZK13 RL.H-271 6.62 7.75 1.13 1.13 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.68 <30 330 <5 6.3 <10 240 40 210 7.31 2.6 <10 50 1.76 1970 <10 130 0.03 <20 <50 43 <50

272 ZK13 RL.H-272 8.80 1.05 1.05 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 8.69 <30 140 <5 7.4 <10 250 50 290 8.55 2.7 <10 30 2 2200 <10 140 0.03 <20 <50 49 <50

273 ZK13 RL.H-273 9.90 1.10 1.10 100 42/2 磁黄铁矿化黄铁矿化黄铜矿化（变）安山岩/Pyrrhotite&Pyrite&Chalcopyrite Mineralization(Altered), Andesite ICP90A 7.89 <30 160 <5 5.6 <10 260 50 3010 8.83 2.4 <10 40 1.79 1730 <10 130 0.03 <20 <50 42 <50

274 ZK13 RL.H-274 10.76 0.86 0.86 100 42/2 磁黄铁矿化黄铁矿化黄铜矿化（变）安山岩/Pyrrhotite&Pyrite&Chalcopyrite Mineralization(Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.06 <30 130 <5 4.2 <10 210 180 1330 14.2 2.2 <10 30 1.75 1300 <10 220 0.03 <20 <50 30 <50

275 RL.H-275 ICP90A FAI323 Au AAS21E Ag 7 <30 530 <5 1.5 <10 20 <10 <10 1.57 4.3 90 40 0.17 320 <10 <10 0.01 <20 <50 <5 <50

276 ZK13 RL.H-276 11.86 1.10 1.10 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 8.36 <30 140 <5 9.6 <10 230 50 300 7.23 2.4 <10 40 2.44 2090 <10 140 0.03 <20 <50 35 <50

277 ZK13 RL.H-277 12.96 1.10 1.10 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 9.71 <30 180 <5 5.1 <10 300 70 290 7.89 3.1 <10 50 1.76 1480 <10 190 0.03 <20 <50 47 <50

278 ZK13 RL.H-278 123.14 124.14 1.00 1.00 100 42/2 辉长岩/Gabbro ICP90A 7.99 <30 660 <5 6.4 <10 90 40 70 7.46 1.8 30 60 4.68 1070 <10 70 0.29 <20 <50 30 <50

279 ZK13 RL.H-279 125.14 1.00 1.00 100 42/2 辉长岩/Gabbro ICP90A 8.07 <30 640 <5 6.6 <10 100 40 80 7.74 1.7 30 50 4.93 1100 <10 70 0.3 <20 <50 31 <50

280 ZK7 RL.H-280 1.30 2.40 1.10 1.10 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.19 <30 70 <5 4.5 <10 310 50 120 9.29 0.3 <10 20 3.42 2780 <10 120 0.04 <20 <50 38 <50

281 ZK7 RL.H-281 3.60 1.20 1.20 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.14 <30 280 <5 7.1 <10 420 60 240 8.96 0.5 30 20 4.9 2280 <10 210 0.12 <20 <50 26 <50

282 ZK7 RL.H-282 4.90 1.30 1.30 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.1 <30 300 <5 3.9 <10 360 50 130 8.77 0.6 20 40 3.84 2400 <10 200 0.09 <20 <50 34 <50

第 3 页，共 10 页

序号 工程编号 送样编号 岩矿心长 采取率 采样规格 样品重量 岩（矿）石 名 称采

样日

期

No. DH No.Sample

No.to Lab自

(From)至

(To)样长

(Length)

Length of

core (m)

Recovery

factor(%)Size(mm) Weight(kg) Rock/Ore type

Samp

ling

date

ME Au AgAl

%

As

ppm

Ba

ppm

Be

ppm

Ca

%

Cd

ppm

Cr

ppm

Co

ppm

Cu

ppm

Fe

%

K

%

La

ppm

Li

ppm

Mg

%

Mn

ppm

Mo

ppm

Ni

ppm

P

%

Pb

ppm

Sb

ppm

Sc

ppm

Sn

ppm

分析结果/Assay Result

基本析样品取样及分析结果登记表

取样位置Sampling location (m)

Sample Log

分析方法/Assay Method

正元国际矿业有限公司W W W . C N Z I M C . C O M

正元国际矿业有限公司W W W . C N Z I M C . C O M

283 ZK7 RL.H-283 6.12 1.22 1.20 98 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.73 <30 70 <5 2 <10 320 50 110 9.83 0.2 <10 40 2.43 2890 <10 120 0.04 <20 <50 42 <50

284 ZK7 RL.H-284 7.22 1.10 1.08 98 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 8.73 <30 240 <5 2.4 <10 330 80 250 10.5 0.3 <10 30 1.75 2750 <10 160 0.04 <20 <50 38 <50

285 ZK7 RL.H-285 8.23 1.01 1.00 98 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.63 <30 240 <5 2.4 <10 350 80 210 11 0.3 <10 20 1.69 2800 <10 170 0.04 <20 <50 31 <50

286 RL.H-286 ICP90A 6.94 90 540 <5 0.7 20 30 20 4150 4.49 4.4 20 10 0.84 500 160 30 0.08 1940 60 11 250

287 ZK7 RL.H-287 9.40 1.17 1.17 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.07 <30 80 <5 2.8 <10 280 90 440 12.7 0.2 <10 20 1.9 2810 <10 170 0.04 <20 <50 29 <50

288 ZK7 RL.H-288 10.50 1.10 1.10 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.6 <30 70 <5 5.5 <10 210 40 120 7.68 0.1 <10 <10 2.55 3010 <10 80 0.04 <20 <50 45 <50

289 ZK7 RL.H-289 28.77 29.87 1.10 1.10 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.93 <30 40 <5 3.8 <10 150 50 110 13.8 <0.1 <10 30 2.39 3360 <10 80 0.06 <20 <50 40 <50

290 ZK7 RL.H-290 30.81 0.94 0.94 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.38 <30 250 <5 2.5 <10 100 50 160 12.1 1 <10 40 1.79 2170 <10 80 0.05 <20 <50 27 <50

291 ZK7 RL.H-291 31.81 1.00 1.00 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.07 <30 820 <5 2.4 <10 30 <10 <10 1.85 2.1 10 20 0.58 420 <10 <10 0.06 <20 <50 <5 <50

292 ZK7 RL.H-292 32.81 1.00 1.00 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 6.85 <30 560 <5 1.8 <10 130 30 310 6.06 2.4 20 20 1.21 500 <10 80 0.07 <20 <50 10 <50

293 ZK7 RL.H-293 33.81 1.00 1.00 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.47 <30 180 <5 1.1 <10 60 60 250 12.6 1.4 10 30 1.12 1170 <10 130 0.04 <20 <50 14 <50

294 ZK7 RL.H-294 34.91 1.10 1.10 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 8.04 <30 40 <5 5.7 <10 130 40 70 11.4 0.2 <10 20 3.43 2570 <10 70 0.06 <20 <50 36 <50

295 ZK7 RL.H-295 36.11 1.20 1.20 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.64 <30 50 <5 5.3 <10 140 50 110 10.4 0.2 <10 20 3.66 2300 <10 60 0.07 <20 <50 37 <50

296 ZK7 RL.H-296 43.51 44.81 1.30 1.30 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 8.37 <30 700 <5 5.4 <10 140 50 130 10.6 1.4 <10 50 2.89 1730 <10 80 0.07 <20 <50 43 <50

297 RL.H-297 ICP90A 7.14 <30 470 6 0.7 <10 <10 <10 <10 1.61 4.3 90 40 0.18 350 <10 <10 0.02 <20 <50 <5 <50

298 ZK7 RL.H-298 46.01 1.20 1.20 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.05 <30 170 <5 3.4 <10 100 40 100 12.2 1.3 10 30 2.46 1420 <10 60 0.11 <20 <50 42 <50

299 ZK7 RL.H-299 46.91 0.90 0.90 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 6.37 <30 130 <5 6.7 <10 40 30 60 10.7 1.2 10 20 2.73 2390 <10 30 0.1 <20 <50 35 <50

300 ZK7 RL.H-300 47.91 1.00 1.00 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 6.48 <30 80 <5 5.7 <10 40 30 50 12.2 0.6 <10 10 2.7 2200 <10 20 0.11 <20 <50 35 <50

301 ZK7 RL.H-301 49.01 1.10 1.10 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.8 <30 90 <5 3.9 <10 80 30 110 11.2 0.7 10 60 2.1 1230 <10 60 0.07 <20 <50 19 <50

302 ZK7 RL.H-302 49.91 0.90 0.90 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.03 <30 160 <5 0.7 <10 80 40 110 13.1 1.4 20 50 1.33 610 <10 130 0.04 <20 <50 13 <50

303 ZK7 RL.H-303 50.90 0.99 0.99 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 3.96 <30 70 <5 3.8 <10 110 30 220 13.1 0.6 <10 10 1.5 1820 <10 100 0.02 <20 <50 13 <50

304 ZK7 RL.H-304 52.00 1.10 1.10 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 7.67 <30 100 <5 4.5 <10 240 40 130 11.4 0.9 <10 30 4.66 1710 <10 120 0.03 <20 <50 35 <50

305 ZK7 RL.H-305 53.10 1.10 1.10 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 6.85 <30 90 <5 4.4 <10 50 30 70 10.9 1 10 40 2.88 1570 <10 50 0.11 <20 <50 37 <50

306 ZK7 RL.H-306 54.20 1.10 1.10 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.33 <30 120 <5 0.3 <10 110 60 210 13.4 1.6 10 30 0.92 530 <10 120 0.03 <20 <50 16 <50

307 ZK7 RL.H-307 55.40 1.20 1.20 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 6.38 <30 140 <5 0.4 <10 70 40 130 8.85 1.4 20 60 1.44 430 <10 110 0.03 30 <50 10 <50

308 RL.H-308 ICP90A 6.14 470 1550 <5 2.6 60 370 30 26200 6.7 2.5 20 20 1.87 900 1260 260 0.12 8060 90 12 120

309 ZK7 RL.H-309 56.40 1.00 1.00 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 7.09 <30 80 <5 2.4 <10 50 50 250 12.7 0.6 10 70 2.14 1290 <10 60 0.08 20 <50 30 <50

310 ZK7 RL.H-310 57.27 0.87 0.87 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 7.09 <30 90 <5 4.4 <10 40 40 80 12.3 0.6 10 20 2.47 1740 <10 30 0.11 <20 <50 36 <50

311 ZK7 RL.H-311 58.27 1.00 1.00 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 6.93 <30 20 <5 5 <10 40 40 40 12.6 <0.1 10 <10 2.17 1720 <10 20 0.11 <20 <50 36 <50

312 ZK7 RL.H-312 74.59 75.59 1.00 1.00 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 9.11 <30 270 <5 1.3 <10 160 30 110 5.23 3.3 20 20 1.6 1030 <10 80 0.03 <20 <50 21 <50

313 ZK7 RL.H-313 76.79 1.20 1.20 100 42/2 （变）安山岩夹黄铁矿细脉/(Altered) Andesite, associated with Pyrite veinlets ICP90A 8.47 <30 270 <5 0.5 <10 150 40 160 7.03 3 20 20 1.5 980 <10 100 0.03 <20 <50 22 <50

314 ZK7 RL.H-314 77.79 1.00 1.00 100 42/2 （变）安山岩夹黄铁矿细脉/(Altered) Andesite, associated with Pyrite veinlets ICP90A FAI323 Au AAS21E Ag 7.74 <30 390 <5 2 <10 200 30 110 6.6 2.4 20 20 2.21 1370 <10 110 0.05 <20 <50 19 <50

315 ZK7 RL.H-315 78.74 0.95 0.95 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.23 <30 420 <5 3.6 <10 310 40 100 8.54 1.3 20 20 3.57 1930 <10 140 0.08 <20 <50 25 <50

316 ZK2 RL.H-316 36.15 37.35 1.20 1.20 100 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A FAI323 Au AAS21E Ag 8.85 <30 690 <5 4.1 <10 250 40 700 7.09 2.2 20 30 2.42 930 <10 80 0.07 <20 <50 24 <50

317 ZK2 RL.H-317 38.10 0.75 0.75 100 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 7.91 <30 900 <5 4.7 <10 90 40 230 6.36 1.4 20 20 2.46 980 <10 50 0.14 <20 <50 17 <50

318 ZK2 RL.H-318 39.10 1.00 1.00 100 42/2 (变）安山岩/(Altered) Andesite ICP90A 7.92 <30 690 <5 5.9 <10 230 30 190 6.87 0.9 20 20 3.96 1280 <10 70 0.14 <20 <50 24 <50

319 RL.H-319 ICP90A 6.89 <30 430 6 0.7 <10 20 <10 <10 1.58 4.2 90 40 0.17 340 <10 <10 0.02 <20 <50 <5 <50

320 ZK10 RL.H-320 50.29 51.39 1.10 1.10 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (altered), Andesite ICP90A 7.44 <30 80 <5 10.2 <10 270 30 130 5.86 1.2 <10 40 4.82 1970 <10 70 0.02 <20 <50 38 <50

321 ZK10 RL.H-321 52.69 1.30 1.30 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (altered), Andesite ICP90A 6.96 <30 80 6 10.2 <10 210 30 300 5.97 1.5 <10 50 4.48 2080 <10 60 0.04 <20 <50 34 <50

322 ZK10 RL.H-322 53.64 0.95 0.95 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (altered), Andesite ICP90A 7.42 <30 120 <5 4.9 <10 130 40 310 5.84 1.5 <10 30 2.81 1020 <10 60 0.05 <20 <50 34 <50

323 ZK10 RL.H-323 54.56 0.92 0.92 100 42/2 黄铁矿化（变）安山岩/Pyrite Mineralization (altered), Andesite ICP90A 8.22 <30 170 6 5.6 <10 170 40 180 9.02 2.7 <10 60 3.96 1250 <10 70 0.09 <20 <50 48 <50

324 ZK13 RL.H-324 104.85 105.95 1.10 1.10 100 42/2 辉长岩/Gabbro ICP90A 8.17 <30 720 <5 5.9 <10 110 30 100 7.12 1.8 30 40 4.27 1020 <10 60 0.26 <20 <50 28 <50

325 ZK13 RL.H-325 107.25 1.30 1.30 100 42/2 辉长岩/Gabbro ICP90A 8.29 <30 760 <5 6 <10 130 30 80 7.01 2 30 30 4.25 1020 <10 70 0.27 <20 <50 27 <50

326 ZK8 RL.H-326 41.15 42.30 1.15 1.15 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralizaiton, (altered) Andesite ICP90A 7.61 <30 70 <5 7.8 <10 190 50 110 13.4 0.6 <10 40 2.55 5140 <10 120 0.04 <20 <50 38 <50

327 ZK8 RL.H-327 43.55 1.25 1.25 100 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralizaiton, (altered) Andesite ICP90A 7.96 <30 80 <5 8 <10 200 60 100 11.2 0.6 <10 40 2.43 4470 <10 120 0.04 <20 <50 39 <50

328 ZK8 RL.H-328 58.69 60.00 1.31 1.30 99 42/2 （变）安山岩/(Altered) Andesite ICP90A 8.81 <30 170 <5 6.9 <10 230 60 190 8.11 0.3 <10 30 2.13 3300 <10 150 0.04 <20 <50 41 <50

329 ZK8 RL.H-329 60.65 0.65 0.64 99 42/2 弱磁黄铁矿化黄铜矿化（变）安山岩/Weak Pyrrhotite&Chalcopyrite Mineralzation (Altered) Andesite ICP90A 6.4 <30 100 <5 11.2 <10 160 70 1170 14.2 0.5 <10 50 2 5330 <10 110 0.03 <20 <50 34 <50

330 RL.H-330 ICP90A 7.35 80 540 <5 0.8 20 40 20 4300 4.74 4.6 20 10 0.89 550 160 30 0.09 2030 70 12 250

331 ZK8 RL.H-331 61.91 1.26 1.25 99 42/2 （变）安山岩/(Altered) Andesite ICP90A 8.94 <30 190 <5 5.7 <10 220 60 160 6.87 0.4 <10 30 2.06 2670 <10 130 0.06 <20 <50 42 <50

332 ZK8 RL.H-332 114.30 115.58 1.28 1.25 98 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralizaiton, (altered) Andesite ICP90A 7 <30 90 <5 7.8 <10 80 50 170 13.4 0.3 <10 40 3.14 5090 <10 60 0.05 400 <50 46 <50

333 ZK8 RL.H-333 116.65 1.07 1.05 98 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralizaiton, (altered) Andesite ICP90A 7.03 <30 100 <5 7 <10 60 50 160 11.2 0.5 <10 40 2.75 4270 <10 60 0.05 <20 <50 45 <50

334 ZK8 RL.H-334 117.85 1.20 1.18 98 42/2 弱磁黄铁矿化（变）安山岩/Weak Pyrrhotite Mineralizaiton, (altered) Andesite ICP90A 7 <30 20 <5 8.3 <10 70 50 240 12.2 0.2 <10 30 2.42 4360 <10 60 0.05 <20 <50 45 <50

335 ZK6 RL.H-335 11.39 12.44 1.05 1.05 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 7.78 <30 320 <5 8.5 <10 280 60 300 9.06 1.5 <10 40 3.86 1720 <10 140 0.03 <20 <50 39 <50

336 ZK6 RL.H-336 13.54 1.10 1.10 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.64 <30 140 <5 9 <10 300 40 130 7.57 1 <10 30 3.87 1470 <10 130 0.02 <20 <50 37 <50

337 ZK6 RL.H-337 14.62 1.08 1.08 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 7.34 <30 230 <5 7.8 <10 310 90 210 9.92 1.4 <10 50 4.55 1340 <10 140 0.03 <20 <50 34 <50

338 ZK6 RL.H-338 15.85 1.23 1.23 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.9 <30 160 <5 0.7 <10 60 <10 60 0.73 3.9 30 10 0.08 200 <10 <10 0.01 30 <50 <5 <50

339 ZK6 RL.H-339 16.60 0.75 0.75 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.17 <30 170 <5 8.6 <10 240 30 210 6.9 1.4 <10 50 3.19 1700 <10 100 0.03 <20 <50 29 <50

340 ZK6 RL.H-340 18.06 1.46 1.46 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.92 <30 360 <5 0.6 <10 30 <10 30 1.09 4 20 10 0.08 210 <10 <10 <0.01 30 <50 <5 <50

341 RL.H-341 ICP90A 7.12 <30 460 6 0.7 <10 20 <10 40 1.38 4.6 90 40 0.15 330 <10 <10 0.01 <20 <50 <5 <50

342 ZK6 RL.H-342 19.36 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 8.28 <30 120 <5 12.7 <10 360 40 100 8.23 1.3 <10 40 2.82 2470 20 110 0.03 <20 <50 40 <50

343 ZK6 RL.H-343 20.51 1.15 1.15 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 8.55 <30 230 <5 9 <10 340 50 140 7.67 2.4 <10 50 2.48 1500 <10 150 0.03 <20 <50 43 <50

344 ZK6 RL.H-344 21.66 1.15 1.15 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 6 <30 120 <5 9.8 <10 1060 20 280 8.1 1.3 <10 40 3.85 1760 <10 160 0.03 720 <50 33 <50

345 ZK6 RL.H-345 22.16 0.50 0.50 100 42/2 块状硫化物（Po）/VMS (Po) ICP90A 0.74 <30 <10 <5 3.3 <10 30 <10 1100 >30 0.2 <10 <10 0.57 540 20 220 <0.01 <20 <50 <5 <50

346 ZK6 RL.H-346 23.61 1.45 1.44 99 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 6.97 <30 620 <5 3.5 <10 440 20 110 6.16 1.7 20 30 2.56 1040 <10 70 0.07 <20 <50 17 <50

347 ZK6 RL.H-347 24.54 0.93 0.92 99 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 4.62 <30 700 <5 1.4 <10 80 70 730 23.7 1.7 30 20 0.92 710 <10 140 0.06 <20 <50 <5 <50

348 ZK6 RL.H-348 25.22 0.68 0.67 99 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A 0.93 <30 80 <5 1.4 <10 70 40 870 >30 0.3 <10 <10 0.59 430 <10 270 0.02 <20 <50 <5 <50

349 ZK6 RL.H-349 26.26 0.94 0.93 99 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 4.1 <30 150 <5 4.5 <10 720 20 790 20.3 0.7 <10 20 2.96 1300 <10 170 0.01 <20 <50 17 <50

350 ZK6 RL.H-350 27.23 1.07 1.07 100 42/2 中性侵入岩/Intermediate Intrusive ICP90A 7.69 <30 1220 <5 1.9 <10 90 <10 60 2.98 3 40 60 1.04 490 <10 50 0.07 <20 <50 <5 <50

351 ZK6 RL.H-351 28.60 1.37 1.37 100 42/2 块状-稠密浸染状硫化物（Po,Py）/Massive-deseminated VMS (Po,Py) ICP90A FAI323 Au AAS21E Ag 0.46 <30 <10 <5 1.3 <10 40 50 1160 >30 <0.1 <10 <10 0.55 580 <10 250 <0.01 <20 <50 <5 <50

352 RL.H-352 ICP90A FAI323 Au AAS21E Ag 5.89 410 1510 <5 2.6 60 370 30 24700 6.74 2.4 20 20 1.85 950 1240 250 0.11 7750 90 12 110

353 ZK6 RL.H-353 29.80 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 3.61 <30 10 <5 0.8 <10 50 <10 300 7.16 1.7 <10 <10 0.38 500 30 30 <0.01 20 <50 <5 <50

354 ZK6 RL.H-354 31.00 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.78 <30 10 <5 1.6 <10 40 10 210 9.13 0.1 <10 <10 0.72 830 20 40 0.02 <20 <50 <5 <50

355 ZK6 RL.H-355 32.00 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 1.4 <30 20 <5 2.6 <10 40 30 390 15.2 0.1 <10 <10 1.21 1250 <10 50 0.02 <20 <50 <5 <50

356 ZK6 RL.H-356 33.22 1.22 1.20 98 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.2 <30 20 <5 1.8 <10 60 10 460 18.9 0.3 <10 10 1.39 2130 <10 80 0.02 <20 <50 5 <50

357 ZK6 RL.H-357 34.49 1.27 1.25 98 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 3.7 <30 70 <5 5.8 <10 720 50 160 9.29 0.4 <10 20 3.7 1190 <10 120 0.03 <20 <50 22 <50

358 ZK6 RL.H-358 35.75 1.26 1.25 99 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 5.41 <30 40 <5 3.6 <10 1120 40 270 14.9 0.7 <10 50 6.01 1740 <10 260 0.03 <20 <50 30 <50

359 ZK6 RL.H-359 37.10 1.35 1.35 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.77 <30 <10 <5 1.9 <10 80 80 410 24.1 0.2 <10 90 1.9 1830 <10 80 0.03 <20 <50 6 <50

360 ZK6 RL.H-360 38.10 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 7.28 <30 80 <5 6.1 <10 860 40 140 7.78 0.6 <10 50 6.41 1980 <10 120 0.02 <20 <50 45 <50

361 ZK6 RL.H-361 39.10 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 7.78 <30 100 <5 5.7 <10 790 40 150 7.02 0.9 <10 60 5.83 2110 <10 130 0.02 <20 <50 47 <50

362 ZK6 RL.H-362 40.00 0.90 0.90 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 1.6 <30 <10 <5 1.5 <10 90 110 260 26.1 0.2 <10 10 1.23 1060 <10 170 <0.01 <20 <50 <5 <50

363 RL.H-363 ICP90A 7.02 <30 380 8 0.7 <10 30 <10 30 1.96 4.5 80 40 0.17 400 <10 <10 0.01 <20 <50 <5 <50

364 ZK6 RL.H-364 40.90 0.90 0.90 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 1.98 <30 50 <5 2.4 <10 30 60 350 >30 0.4 <10 10 1.02 1330 <10 170 0.02 <20 <50 <5 <50

365 ZK6 RL.H-365 41.79 0.89 0.89 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.66 <30 40 <5 2.1 <10 60 20 390 19.8 0.5 <10 30 1.43 1080 <10 110 <0.01 <20 <50 6 <50

366 ZK6 RL.H-366 42.86 1.07 1.07 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 1.05 <30 10 <5 1.9 <10 60 <10 100 8.49 0.3 <10 10 0.73 1140 20 40 <0.01 <20 <50 <5 <50

367 ZK6 RL.H-367 44.36 1.50 1.50 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.63 <30 200 <5 0.7 <10 40 <10 50 1.5 3.9 20 <10 0.16 360 <10 <10 0.01 20 <50 <5 <50

368 ZK6 RL.H-368 45.86 1.50 1.50 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.72 <30 320 <5 0.7 <10 30 <10 60 1.18 4 30 <10 0.06 300 <10 <10 0.01 30 <50 <5 <50

369 ZK6 RL.H-369 46.92 1.06 1.06 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 1.74 <30 30 <5 3.3 <10 60 <10 170 15.1 0.6 <10 <10 1.31 1880 <10 70 0.02 <20 <50 <5 <50

370 ZK6 RL.H-370 47.80 0.88 0.88 100 42/2 块状硫化物（Py,Po）/VMS (Py,Po) ICP90A 0.7 <30 <10 <5 2.2 <10 30 360 320 >30 0.1 <10 <10 0.6 2060 <10 110 0.02 <20 <50 <5 <50

371 ZK6 RL.H-371 48.90 1.10 1.10 100 42/2 块状硫化物（Py,Po）/VMS (Py,Po) ICP90A 0.42 <30 <10 <5 2.3 <10 40 40 290 >30 0.1 <10 <10 0.51 1840 <10 120 <0.01 <20 <50 <5 <50

372 ZK6 RL.H-372 50.10 1.20 1.20 100 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.25 <30 <10 5 4.4 <10 20 40 390 >30 <0.1 <10 <10 0.36 1770 <10 220 0.02 <20 <50 <5 <50

373 ZK6 RL.H-373 51.33 1.23 1.20 98 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.49 <30 <10 <5 2.1 <10 140 70 310 >30 0.2 <10 <10 0.42 2450 <10 200 0.01 <20 <50 <5 <50

374 RL.H-374 ICP90A 7.24 100 600 <5 0.8 20 50 20 4330 4.85 4.9 20 10 0.86 550 170 30 0.09 2130 80 12 270

375 ZK6 RL.H-375 52.59 1.26 1.22 97 42/2 块状-稠密浸染状硫化物（Po,Py）/Massive-deseminated VMS (Po,Py) ICP90A 0.21 <30 <10 <5 3 <10 90 <10 150 27 <0.1 <10 <10 0.98 2340 <10 140 <0.01 <20 <50 <5 <50

376 ZK6 RL.H-376 53.82 1.23 1.20 98 42/2 块状-稠密浸染状硫化物（Po,Py）/Massive-deseminated VMS (Po,Py) ICP90A 0.37 <30 <10 <5 4.7 <10 50 20 330 >30 <0.1 <10 <10 1.4 1390 <10 140 <0.01 20 <50 <5 <50

第 4 页，共 10 页

序号 工程编号 送样编号 岩矿心长 采取率 采样规格 样品重量 岩（矿）石 名 称采

样日

期

No. DH No.Sample

No.to Lab自

(From)至

(To)样长

(Length)

Length of

core (m)

Recovery

factor(%)Size(mm) Weight(kg) Rock/Ore type

Samp

ling

date

ME Au AgAl

%

As

ppm

Ba

ppm

Be

ppm

Ca

%

Cd

ppm

Cr

ppm

Co

ppm

Cu

ppm

Fe

%

K

%

La

ppm

Li

ppm

Mg

%

Mn

ppm

Mo

ppm

Ni

ppm

P

%

Pb

ppm

Sb

ppm

Sc

ppm

Sn

ppm

分析结果/Assay Result

基本析样品取样及分析结果登记表

取样位置Sampling location (m)

Sample Log

分析方法/Assay Method

正元国际矿业有限公司W W W . C N Z I M C . C O M

正元国际矿业有限公司W W W . C N Z I M C . C O M

377 ZK6 RL.H-377 55.08 1.26 1.25 99 42/2 块状-稠密浸染状硫化物（Po,Py）/Massive-deseminated VMS (Po,Py) ICP90A 0.42 <30 <10 <5 3.1 <10 30 10 370 >30 <0.1 <10 <10 0.76 1000 <10 210 <0.01 <20 <50 <5 <50

378 ZK6 RL.H-378 56.39 1.31 1.29 99 42/2 块状-稠密浸染状硫化物（Po,Py）/Massive-deseminated VMS (Po,Py) ICP90A FAI323 Au AAS21E Ag 0.75 <30 30 <5 2.9 <10 30 30 350 >30 0.1 <10 <10 0.94 5450 <10 180 <0.01 <20 <50 <5 <50

379 ZK6 RL.H-379 57.64 1.25 1.25 100 42/2 稠密浸染状硫化物（Po,Py）/intensively Diseminated VMS (Po,Py) ICP90A 1.01 <30 50 <5 1.9 <10 20 60 320 >30 0.3 <10 <10 0.63 5210 <10 140 0.01 <20 <50 <5 <50

380 ZK6 RL.H-380 58.94 1.30 1.30 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 0.86 <30 40 <5 2.2 <10 20 40 470 >30 0.3 <10 <10 0.91 3670 <10 170 <0.01 <20 <50 <5 <50

381 ZK6 RL.H-381 60.18 1.24 1.24 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 0.56 <30 <10 <5 2.1 <10 20 110 480 >30 0.1 <10 <10 0.89 2180 <10 130 0.01 <20 <50 <5 <50

382 ZK6 RL.H-382 61.38 1.20 1.20 100 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.4 <30 <10 <5 2.2 <10 20 160 640 >30 <0.1 <10 <10 0.97 2780 <10 110 0.02 30 <50 <5 <50

383 ZK6 RL.H-383 62.48 1.10 1.10 100 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A 0.75 <30 <10 <5 3.2 <10 10 110 260 >30 <0.1 <10 <10 1.4 3120 <10 100 <0.01 <20 <50 <5 <50

384 ZK6 RL.H-384 63.63 1.15 1.15 100 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.58 <30 20 <5 1.9 <10 20 160 250 >30 0.2 <10 <10 0.28 3340 <10 120 0.01 <20 <50 <5 <50

385 RL.H-385 ICP90A FAI323 Au AAS21E Ag 6.9 <30 510 8 0.9 <10 20 <10 40 2.63 4.5 80 40 0.17 450 <10 10 0.02 <20 <50 <5 <50

386 ZK6 RL.H-386 64.83 1.20 1.20 100 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A 0.94 <30 50 <5 2 <10 20 110 220 >30 0.4 <10 <10 0.33 4610 <10 140 0.01 <20 <50 <5 <50

387 ZK6 RL.H-387 66.13 1.30 1.30 100 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A 1.38 <30 50 <5 3.2 <10 20 80 260 >30 0.4 <10 <10 0.6 4810 <10 140 <0.01 <20 <50 <5 <50

388 ZK6 RL.H-388 67.13 1.00 1.00 100 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 1.11 <30 30 <5 2.2 <10 20 120 270 >30 0.3 <10 <10 0.33 6540 <10 150 0.01 <20 <50 <5 <50

389 ZK6 RL.H-389 68.28 1.15 1.15 100 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A 1.42 <30 50 <5 2.5 <10 20 90 270 >30 0.5 <10 <10 0.47 6560 <10 130 <0.01 <20 <50 <5 <50

390 ZK6 RL.H-390 69.48 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 4.55 <30 130 <5 4.2 <10 50 10 170 16.9 1.3 10 10 1.45 1410 <10 80 0.03 <20 <50 8 <50

391 ZK6 RL.H-391 70.68 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 6.26 <30 230 7 4.2 <10 60 <10 130 12.2 2 20 20 1.13 1290 <10 60 0.05 <20 <50 14 <50

392 ZK6 RL.H-392 71.98 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 4.98 <30 150 7 2.9 <10 50 30 180 18 1.7 <10 10 0.9 1840 <10 100 0.03 <20 <50 13 <50

393 ZK6 RL.H-393 72.98 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.28 <30 30 5 2.3 <10 30 160 160 >30 0.3 <10 <10 0.77 1870 <10 80 0.02 30 <50 5 <50

394 ZK6 RL.H-394 73.98 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 2.1 30 10 7 2.5 <10 40 130 340 >30 0.2 <10 <10 0.86 3090 <10 160 0.02 <20 <50 <5 <50

395 ZK6 RL.H-395 75.28 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 6.02 <30 130 8 4.9 <10 140 10 130 14.2 1.4 10 <10 1.66 2650 <10 90 0.03 <20 <50 18 <50

396 RL.H-396 ICP90A 6.13 450 1490 8 2.7 60 380 30 24900 6.94 2.4 20 20 1.88 1030 1250 260 0.14 7770 80 12 120

397 ZK6 RL.H-397 76.48 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 5.91 <30 150 7 4.7 <10 590 10 120 10.5 1.6 10 10 1.63 2810 <10 80 0.03 <20 <50 18 <50

398 ZK6 RL.H-398 77.72 1.24 1.24 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.95 <30 170 8 3.7 <10 70 10 110 9.63 1.4 10 10 0.97 1950 <10 60 0.02 <20 <50 17 <50

399 ZK6 RL.H-399 79.02 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 7.14 <30 310 7 4.1 <10 80 10 70 7.39 1.9 20 10 1.02 2330 <10 50 0.04 <20 <50 17 <50

400 ZK6 RL.H-400 79.82 0.80 0.80 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 3.78 <30 80 6 3.3 <10 80 <10 150 24.6 0.6 <10 10 1 2530 <10 130 0.02 <20 <50 10 <50

401 ZK6 RL.H-401 80.72 0.95 0.95 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 1.6 <30 <10 <5 2 <10 50 10 210 >30 <0.1 <10 <10 0.67 2030 <10 190 0.02 <20 <50 <5 <50

402 ZK6 RL.H-402 81.69 0.92 0.90 98 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 1.34 <30 <10 7 1.3 <10 40 130 150 >30 0.1 <10 <10 0.43 1390 <10 110 0.03 <20 <50 <5 <50

403 ZK6 RL.H-403 82.46 0.77 0.75 98 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 1.9 <30 40 7 2 <10 30 110 80 >30 0.6 <10 <10 0.56 2330 <10 70 0.02 <20 <50 <5 <50

404 ZK6 RL.H-404 83.20 0.74 0.73 98 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.74 <30 90 8 0.6 <10 30 <10 50 1.83 3.7 20 <10 0.08 280 <10 20 <0.01 <20 <50 <5 <50

405 ZK6 RL.H-405 84.45 1.25 1.25 100 42/2 块状硫化物（Py）/VMS(Py) ICP90A FAI323 Au AAS21E Ag 1.55 <30 30 6 2.8 <10 30 70 120 >30 0.4 <10 <10 0.4 2610 <10 50 0.02 30 <50 <5 <50

406 ZK6 RL.H-406 85.69 1.24 1.24 100 42/2 块状硫化物（Py）/VMS(Py) ICP90A 0.49 30 <10 6 1.8 <10 30 100 80 >30 <0.1 <10 <10 0.56 3870 <10 60 0.01 <20 <50 <5 <50

407 RL.H-407 ICP90A 7.25 <30 400 12 0.8 <10 20 <10 30 1.55 4.4 80 40 0.18 390 <10 10 0.04 20 <50 <5 <50

408 ZK6 RL.H-408 86.74 1.05 1.05 100 42/2 强硅化磁黄铁矿化黄铁矿化（变）安山岩/strong silicification, Pyrrhotite&Pyrite mineralization, (altered) Andesite ICP90A FAI323 Au AAS21E Ag 0.12 <30 <10 <5 0.4 <10 70 <10 40 1.66 <0.1 <10 <10 0.04 410 <10 30 0.02 <20 <50 <5 <50

409 ZK6 RL.H-409 87.89 1.15 1.15 100 42/2 强硅化磁黄铁矿化黄铁矿化（变）安山岩/strong silicification, Pyrrhotite&Pyrite mineralization, (altered) Andesite ICP90A 0.09 30 <10 <5 0.3 <10 100 <10 20 0.82 <0.1 <10 <10 0.05 270 <10 40 <0.01 <20 <50 <5 <50

410 ZK6 RL.H-410 88.89 1.00 1.00 100 42/2 块状硫化物（Py）/VMS(Py) ICP90A 0.26 40 <10 <5 1.2 <10 20 120 70 >30 <0.1 <10 <10 0.33 2480 <10 40 <0.01 <20 <50 <5 <50

411 ZK6 RL.H-411 89.92 1.03 1.03 100 42/2 块状硫化物（Py）/VMS(Py) ICP90A 0.43 <30 <10 5 2.1 <10 10 100 160 >30 <0.1 <10 <10 0.63 4770 <10 60 0.02 <20 <50 <5 <50

412 ZK6 RL.H-412 91.06 1.14 1.14 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.75 <30 <10 <5 2 <10 40 70 80 27.1 <0.1 <10 <10 0.5 3250 <10 30 <0.01 <20 <50 <5 <50

413 ZK6 RL.H-413 91.77 0.71 0.71 100 42/2 块状硫化物（Py,Po）/VMS (Py,Po) ICP90A 0.82 <30 <10 5 3 <10 20 70 160 >30 <0.1 <10 <10 1.45 8530 <10 140 0.01 <20 <50 5 <50

414 ZK6 RL.H-414 92.48 0.71 0.71 100 42/2 黄铁矿化磁黄铁矿化（变）安山岩/Pyrite&Pyrrhotite mineralization (altered), Andesite ICP90A 0.4 <30 <10 7 3.6 <10 80 <10 140 11.4 <0.1 <10 <10 0.91 6840 <10 40 <0.01 <20 <50 <5 <50

415 ZK6 RL.H-415 93.80 1.32 1.32 100 42/2 块状硫化物（Py,Po）/VMS (Py,Po) ICP90A 0.47 40 <10 6 2.3 <10 <10 100 120 >30 <0.1 <10 <10 0.89 7730 <10 70 0.01 <20 <50 <5 <50

416 ZK6 RL.H-416 95.00 1.20 1.20 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.5 40 30 6 2 <10 20 100 150 >30 0.1 <10 <10 0.57 4260 <10 60 0.02 <20 <50 <5 <50

417 ZK6 RL.H-417 96.01 1.01 1.01 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 0.19 <30 <10 <5 2.6 <10 20 70 150 >30 <0.1 <10 <10 0.76 3230 <10 80 <0.01 <20 <50 <5 <50

418 RL.H-418 ICP90A FAI323 Au AAS21E Ag 7.45 100 550 7 0.8 20 60 10 4250 4.91 4.6 10 10 0.89 560 170 30 0.11 2100 70 11 260

419 ZK6 RL.H-419 97.26 1.25 1.25 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 0.24 <30 <10 <5 2.9 <10 50 30 90 21.7 <0.1 <10 <10 0.81 4090 <10 60 <0.01 <20 <50 <5 <50

420 ZK6 RL.H-420 98.10 1.15 1.15 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 0.11 <30 10 <5 1.1 <10 40 10 140 25.8 <0.1 <10 <10 0.23 1810 <10 90 <0.01 <20 <50 <5 <50

421 ZK6 RL.H-421 99.64 1.23 1.23 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.42 30 <10 <5 1.7 <10 30 60 230 >30 <0.1 <10 <10 0.42 5290 <10 90 0.01 <20 <50 <5 <50

422 ZK6 RL.H-422 100.89 1.25 1.25 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.31 <30 <10 <5 2.4 <10 40 10 90 15.4 <0.1 <10 <10 0.73 5500 <10 60 <0.01 <20 <50 6 <50

423 ZK6 RL.H-423 102.11 1.22 1.22 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.67 30 30 <5 5 <10 40 50 590 29.1 0.1 <10 <10 0.62 5470 <10 70 0.01 <20 <50 <5 <50

424 ZK6 RL.H-424 103.21 1.10 1.10 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 1.21 <30 20 5 10.3 <10 20 60 340 >30 <0.1 <10 <10 0.44 4890 <10 80 0.02 <20 <50 <5 <50

425 ZK6 RL.H-425 104.41 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.34 <30 10 <5 0.8 <10 50 20 50 9.49 <0.1 <10 <10 0.25 2880 <10 30 <0.01 <20 <50 <5 <50

426 ZK6 RL.H-426 105.16 0.75 0.75 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 0.43 50 <10 <5 3.6 <10 10 100 70 >30 <0.1 <10 <10 0.79 3680 <10 50 <0.01 <20 <50 <5 <50

427 ZK6 RL.H-427 106.28 1.12 1.12 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.76 <30 10 <5 2.1 <10 20 50 180 >30 0.1 <10 <10 0.56 4760 <10 110 0.02 <20 <50 <5 <50

428 ZK6 RL.H-428 108.00 1.72 1.72 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.51 <30 180 6 0.6 <10 10 <10 50 1.13 3.5 20 <10 0.08 260 20 <10 <0.01 <20 <50 <5 <50

429 RL.H-429 ICP90A 7.11 <30 370 10 0.7 <10 20 <10 50 1.66 4.2 70 40 0.16 390 <10 10 0.02 20 <50 <5 <50

430 ZK6 RL.H-430 109.22 1.22 1.22 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 1.14 30 30 <5 1.9 <10 50 80 140 >30 0.2 <10 <10 0.79 11000 <10 60 0.01 <20 <50 <5 <50

431 ZK6 RL.H-431 110.42 1.20 1.20 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 0.59 <30 20 <5 2 <10 40 70 170 >30 <0.1 <10 <10 0.67 4110 <10 40 0.01 <20 <50 <5 <50

432 ZK6 RL.H-432 111.83 1.41 1.41 100 42/2 稠密浸染状-块状硫化物（Po,Py）/intensively diseminated-massive VMS(Po,Py) ICP90A 0.43 40 10 <5 1.9 <10 40 70 110 >30 <0.1 <10 <10 0.59 2690 <10 50 0.01 <20 <50 <5 <50

433 ZK6 RL.H-433 112.96 1.13 1.13 100 42/2 磁黄铁矿化黄铁矿化（变）安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.24 <30 <10 <5 1.1 <10 70 20 40 17.9 <0.1 <10 <10 0.25 2310 <10 20 0.02 <20 <50 <5 <50

434 ZK6 RL.H-434 114.03 1.07 1.07 100 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A 0.65 40 <10 6 2.4 <10 20 80 90 >30 <0.1 <10 <10 0.82 7100 <10 50 0.02 <20 <50 <5 <50

435 ZK6 RL.H-435 115.15 1.12 1.11 99 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.57 <30 <10 <5 1.7 <10 20 70 120 >30 <0.1 <10 <10 0.67 6490 <10 50 0.01 <20 <50 <5 <50

436 ZK6 RL.H-436 116.31 1.16 1.14 98 42/2 块状硫化物（Po,Py）/VMS(Po,Py) ICP90A 1.05 30 30 <5 1.8 <10 10 80 160 >30 0.2 <10 <10 0.75 6830 <10 70 0.01 <20 <50 <5 <50

437 ZK6 RL.H-437 117.35 1.04 1.02 98 42/2 钾长花岗岩（少量硫化物）/Feldspar Granite(minor VMS) ICP90A 7.08 <30 270 6 1.1 <10 40 <10 30 1.97 3.1 10 30 0.29 680 10 10 0.02 100 <50 <5 <50

438 ZK6 RL.H-438 118.35 1.00 1.00 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.89 30 340 7 0.6 <10 20 <10 40 1.16 4 20 10 0.12 450 <10 <10 0.02 40 <50 <5 <50

439 ZK4 RL.H-439 54.04 55.41 1.07 1.05 98 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 6.59 <30 130 7 7.7 <10 210 50 240 16.1 0.3 <10 30 3.4 4490 <10 120 0.04 <20 <50 30 <50

440 RL.H-440 ICP90A 6.08 420 1460 7 2.7 60 360 30 24900 6.75 2.3 20 20 1.89 940 1270 270 0.13 7880 80 12 120

441 ZK4 RL.H-441 89.92 90.82 0.90 0.90 100 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 7.47 <30 130 10 9.1 <10 230 40 290 11.3 0.3 <10 30 3.24 4860 <10 110 0.05 <20 <50 42 <50

442 ZK4 RL.H-442 91.66 0.84 0.84 100 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 6.5 <30 80 9 7.4 <10 530 60 280 13.4 0.4 <10 30 3.9 4300 <10 180 0.04 <20 <50 39 <50

443 ZK4 RL.H-443 114.13 115.58 1.45 1.41 97 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 7.13 <30 90 8 8.6 <10 120 50 170 15.6 0.2 <10 40 3.73 6280 <10 100 0.04 <20 <50 42 <50

444 ZK4 RL.H-444 117.00 1.42 1.38 97 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 6.89 <30 20 10 7.2 <10 170 50 370 15.1 0.2 <10 40 3.34 5650 <10 100 0.05 <20 <50 41 <50

445 ZK4 RL.H-445 139.88 141.08 1.20 1.20 100 42/2 磁黄铁矿化（变）安山岩夹石英脉/Pyrrhotite Mineralizaton (altered) Andesite, associated with quartz Vein ICP90A FAI323 Au AAS21E Ag 5.89 <30 70 8 6.3 <10 100 40 200 12.6 0.7 <10 50 2.86 4370 <10 60 0.03 <20 <50 35 <50

446 ZK4 RL.H-446 142.33 1.05 1.05 100 42/2 磁黄铁矿化（变）安山岩夹石英脉/Pyrrhotite Mineralizaton (altered) Andesite, associated with quartz Vein ICP90A 7.5 <30 130 8 6.3 <10 70 50 250 12.3 1.6 <10 100 2.71 4180 <10 100 0.07 <20 <50 45 <50

447 ZK4 RL.H-447 161.54 162.54 1.00 1.00 100 42/2 （变）安山岩/(Altered) Andesite ICP90A 7.68 <30 100 8 8.9 <10 30 40 230 12.4 1.4 <10 30 3.15 5370 <10 60 0.06 <20 <50 47 <50

448 ZK4 RL.H-448 163.42 0.88 0.88 100 42/2 磁黄铁矿化（变）安山岩夹石英脉/Pyrrhotite Mineralizaton (altered) Andesite, associated with quartz Vein ICP90A 4.23 <30 60 7 5.4 <10 60 30 190 7.7 0.6 <10 30 1.93 3160 <10 40 0.07 <20 <50 27 <50

449 ZK4 RL.H-449 164.47 1.05 1.05 100 42/2 硅化磁黄铁矿化（变）安山岩/Silicified Pyrrhotite Mineralization, (altered) Andesite ICP90A 8.47 <30 130 9 8.4 <10 30 50 240 13.6 1.3 <10 60 3.15 6040 <10 60 0.04 <20 <50 52 <50

450 ZK4 RL.H-450 165.62 1.15 1.15 100 42/2 石英脉夹磁黄铁矿化（变）安山岩/Quartz Vein, associated with Pyrrhotite Mineralization (Altered), Andesite ICP90A 1.06 <30 20 <5 1.5 <10 70 10 140 2.39 0.3 <10 10 0.48 1170 <10 30 0.02 20 <50 5 <50

451 RL.H-451 ICP90A 7.08 <30 440 12 0.8 <10 20 <10 170 1.47 4.3 70 40 0.18 400 10 10 0.02 30 <50 <5 <50

452 ZK4 RL.H-452 166.62 1.00 1.00 100 42/2 石英脉夹磁黄铁矿化（变）安山岩/Quartz Vein, associated with Pyrrhotite Mineralization (Altered), Andesite ICP90A 2.18 <30 40 11 3.5 <10 70 20 150 5.4 0.2 <10 10 1.23 2320 <10 30 0.03 <20 <50 12 <50

453 ZK4 RL.H-453 167.82 1.20 1.20 100 42/2 石英脉夹磁黄铁矿化（变）安山岩/Quartz Vein, associated with Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.4 <30 70 7 5.8 <10 170 40 210 6.88 0.1 <10 20 2.73 3240 <10 100 0.02 <20 <50 13 <50

454 ZK4 RL.H-454 168.72 0.90 0.90 100 42/2 石英脉夹磁黄铁矿化（变）安山岩/Quartz Vein, associated with Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 1.89 <30 100 6 2 <10 270 30 160 3.15 0.2 <10 20 2.16 930 <10 120 0.04 <20 <50 7 <50

455 ZK4 RL.H-455 169.77 1.05 1.04 99 42/2 石英脉夹磁黄铁矿化（变）安山岩/Quartz Vein, associated with Pyrrhotite Mineralization (Altered), Andesite ICP90A 0.12 <30 <10 5 0.4 <10 70 <10 30 0.57 <0.1 <10 <10 0.07 170 <10 10 <0.01 <20 <50 <5 <50

456 ZK4 RL.H-456 171.00 1.23 1.23 100 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A FAI323 Au AAS21E Ag 5.84 <30 170 8 6.6 <10 340 70 710 13.4 0.5 <10 40 5.06 3680 <10 250 0.08 <20 <50 32 <50

457 ZK4 RL.H-457 172.36 1.36 1.36 100 42/2 磁黄铁矿化(变）安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 5.2 <30 100 6 6.4 <10 860 70 2580 11.8 0.6 10 70 5.74 3290 <10 300 0.07 110 <50 22 <50

458 ZK4 RL.H-458 176.21 177.39 1.18 42/2 沙状粉末/sand power ICP91A FAI323 Au AAS21E Ag

第 5 页，共 10 页

备 注

Sr

ppm

Ti

%

V

ppm

W

ppm

Y

ppm

Zn

ppm

Au

ppb

Ag

g/t

Pt

ppb

Pd

ppbNote

140 0.61 300 <50 29 2100

90 0.61 290 <50 19 1680

100 0.62 290 <50 19 2050

70 0.6 290 <50 21 930

80 0.58 290 <50 18 1460

80 0.61 300 <50 22 1290

60 0.58 290 <50 19 1000

50 0.58 310 <50 18 830

30 0.1 80 <50 14 150

30 0.14 90 <50 11 290

90 0.12 10 <50 82 50 blank

40 0.25 150 <50 15 440 253 <0.3

40 0.16 110 <50 12 510

40 0.07 70 <50 12 260

30 0.11 80 <50 12 970 63 0.3

20 0.03 40 <50 9 80

100 0.34 160 <50 17 880

220 0.48 110 <50 42 590

180 0.41 140 <50 19 1130 43 0.6

60 0.21 100 4370 9 870

40 0.23 130 420 14 1610

270 0.35 160 <50 18 2610 ME-12

50 0.35 150 <50 14 1010

50 0.25 110 <50 13 1580 31 1

30 0.2 120 <50 11 1160

20 0.03 30 <50 8 90

30 0.05 50 <50 10 120

40 0.29 140 <50 14 630

80 0.41 180 <50 19 1100 31 <0.3

30 0.12 60 <50 11 180

20 0.2 110 <50 13 530

<10 0.25 130 <50 14 240

90 0.12 10 <50 81 50 Blank

10 0.13 70 <50 11 210

10 0.16 90 <50 11 950 76 <0.3

<10 0.16 80 <50 13 350

10 0.07 40 <50 10 80

80 0.05 40 <50 8 50

300 0.12 70 <50 10 80

60 0.16 80 <50 13 140

80 0.24 90 <50 21 290 29 0.3

90 0.32 150 <50 11 440

110 0.41 170 <50 27 310

380 0.32 150 <50 17 8990 ME-11

90 0.34 180 <50 17 2000 61 0.6

20 0.13 80 <50 12 1320

90 0.8 300 <50 21 170

120 0.68 250 <50 29 250

90 0.44 220 <50 17 640

80 0.43 230 <50 17 670

80 0.4 200 <50 14 240 30 <0.3

70 0.3 140 <50 10 190

70 0.3 140 <50 10 250 41 <0.3

120 0.53 250 <50 15 180

90 0.12 10 <50 77 40 Blank

40 0.18 130 <50 15 130

20 0.11 90 <50 11 260 19 0.3

20 0.1 60 <50 8 140

<10 0.02 20 <50 8 50

20 0.1 70 <50 12 100

30 0.1 60 <50 10 130 28 <0.3

50 0.21 100 <50 11 190

100 0.38 160 <50 11 160

80 0.41 170 <50 11 190 23 <0.3

70 0.31 140 <50 8 140

280 0.35 170 <50 17 2580 ME-12

820 0.37 180 <50 11 130

110 0.28 160 <50 18 110

120 0.53 290 <50 19 90

150 0.5 280 <50 18 90 <5 <0.3

90 0.49 260 <50 20 80

650 0.48 200 <50 20 180

130 0.45 280 <50 16 80

50 0.31 180 <50 18 80 <5 <0.3

80 0.4 260 <50 15 80

110 0.48 280 <50 18 120

90 0.12 10 <50 77 40 Blank

80 0.41 240 <50 16 100

90 0.43 210 <50 19 290

70 0.27 80 <50 14 1360 29 2.1

80 0.35 110 <50 17 630 22 1.6

60 0.32 120 <50 15 1380

120 0.49 270 <50 15 210

40 0.16 50 <50 10 70

50 0.31 90 <50 16 110

180 0.14 60 <50 12 110 21 0.8

940 0.41 160 <50 16 110

350 0.31 150 <50 17 9110 1410 78.4 ME-11

50 0.24 70 <50 14 1230

50 0.32 100 <50 18 1610

40 0.29 100 <50 18 1660 64 0.8

20 0.02 30 <50 7 170

30 0.04 30 <50 9 200

50 0.35 60 <50 19 680

分析结果/Assay Result

基本析样品取样及分析结果登记表Sample Log

第 6 页，共 10 页

备 注

Sr

ppm

Ti

%

V

ppm

W

ppm

Y

ppm

Zn

ppm

Au

ppb

Ag

g/t

Pt

ppb

Pd

ppbNote

分析结果/Assay Result

基本析样品取样及分析结果登记表Sample Log

40 0.3 70 <50 20 1600

40 0.32 90 <50 20 1550

40 0.25 80 <50 19 880 12 <0.3

30 0.31 80 <50 21 190

100 0.12 10 <50 78 50 Blank

40 0.27 80 <50 22 140

30 0.25 90 1280 23 350

40 0.27 90 <50 15 770

50 0.39 210 <50 19 90

40 0.21 60 <50 16 60

30 0.27 70 <50 16 190

40 0.22 80 <50 15 910 36 0.4

20 0.34 110 <50 18 140

20 0.36 90 <50 18 60

40 0.31 160 <50 11 80

270 0.35 160 <50 18 2600 ME-12

50 0.42 250 <50 14 100

100 1.3 370 <50 35 100

90 0.56 300 <50 20 150

100 0.47 270 <50 18 140

90 0.47 280 <50 18 170

120 0.46 290 <50 18 170

100 0.45 260 <50 17 100 <5 <0.3

70 0.48 280 <50 18 110

130 0.42 280 <50 17 180

40 0.07 80 <50 5 50

100 0.12 10 <50 75 50 Blank

110 0.43 210 <50 20 150 <5 <0.3

130 0.63 280 <50 23 120 <5 <0.3

150 0.43 250 <50 16 180

190 0.42 260 <50 17 150

100 0.16 20 <50 <5 30

80 0.16 20 <50 <5 30

130 0.44 260 <50 20 160

180 0.46 260 <50 19 120

90 0.42 250 <50 20 180

30 0.18 100 <50 13 290 34 1.4

350 0.31 140 <50 17 9240 ME-11

20 0.09 90 <50 5 300 20 4.6

90 0.49 280 <50 19 170

80 0.42 240 <50 20 170

100 0.52 270 <50 21 120

80 0.41 230 <50 18 130

90 0.49 270 <50 20 130

<10 0.03 40 <50 <5 80 22 1.6

30 0.07 60 <50 6 260

30 <0.01 <10 <50 39 <10

40 0.01 <10 <50 29 50

100 0.11 10 <50 74 50 <0.5 <0.3 Blank

20 0.02 40 <50 6 470 14 1.6

10 0.01 40 <50 <5 280

<10 0.02 50 <50 <5 220 14 3.4

40 0.33 220 <50 26 260

40 0.19 120 <50 15 170

940 0.54 160 <50 13 100

120 0.56 300 <50 18 80

120 0.58 300 <50 19 120

120 0.57 310 <50 17 220

100 0.4 210 <50 14 310

280 0.36 170 <50 18 2560 ME-12

90 0.34 170 <50 21 160 6 0.6

110 0.38 210 <50 19 160

110 0.4 200 <50 17 150

140 0.47 270 <50 15 160

110 0.47 260 <50 13 180

100 0.42 250 <50 13 140 <5 0.3

120 0.48 260 <50 13 130

120 0.33 160 <50 9 70

130 0.23 80 <50 7 60

110 0.37 220 <50 13 160

90 0.12 10 <50 79 40 Blank

100 0.44 260 <50 17 170 6 0.5

120 0.47 270 <50 16 260

120 0.43 250 <50 14 190

120 0.49 280 <50 15 160

110 0.47 270 <50 16 160

90 0.44 260 <50 15 140

90 0.51 290 <50 17 180

90 0.49 290 <50 17 140 6 <0.3

120 0.48 270 <50 16 120

130 0.47 270 <50 15 120

380 0.32 150 <50 18 8860 ME-11

130 0.55 310 <50 19 110

120 0.53 300 <50 17 100

80 0.44 270 <50 14 120

60 0.41 250 <50 20 130 12 0.5

70 0.5 280 <50 17 120

120 0.46 270 <50 17 100

130 0.52 300 <50 17 110

80 0.44 250 <50 16 140

110 0.46 240 <50 16 160 <5 0.6

40 0.14 100 <50 9 320 19 1.7

100 0.12 10 <50 78 50 Blank

90 0.33 190 <50 17 120

第 7 页，共 10 页

备 注

Sr

ppm

Ti

%

V

ppm

W

ppm

Y

ppm

Zn

ppm

Au

ppb

Ag

g/t

Pt

ppb

Pd

ppbNote

分析结果/Assay Result

基本析样品取样及分析结果登记表Sample Log

60 0.3 180 <50 12 470

10 0.08 40 <50 6 300

20 0.05 50 <50 9 160 7 1.7

100 0.55 290 <50 16 140

110 0.53 270 <50 11 270

110 0.36 210 <50 14 150

130 0.41 230 <50 17 200

100 0.4 240 <50 13 210

100 0.42 250 <50 13 320 8 0.9

280 0.35 160 <50 18 2590 ME-12

90 0.43 250 <50 14 210

90 0.41 220 <50 16 120

80 0.04 10 <50 7 10

100 0.56 300 <50 21 130

100 0.18 100 <50 8 190 10 0.3

250 0.31 190 <50 12 530

100 0.54 270 <50 19 290 9 0.7

80 0.56 310 <50 18 210

130 0.4 240 <50 12 460

250 0.26 130 <50 8 170

110 0.13 10 <50 79 50 Blank

90 0.45 260 <50 16 220

10 0.11 100 <50 <5 1210 15 0.3

10 0.02 20 <50 <5 380

<10 0.02 20 <50 <5 390

60 0.06 40 <50 <5 100

120 0.08 20 <50 7 40

250 0.05 10 <50 <5 10

90 0.94 420 <50 34 110

1010 0.4 200 <50 18 110

100 0.43 260 <50 16 100

390 0.33 150 <50 17 9020 1230 78.6 ME-11

60 0.21 100 <50 10 110 7 1.1

440 0.47 220 <50 16 140

280 0.5 280 <50 17 160

190 0.5 270 <50 17 90

80 0.23 120 <50 7 40 <5 <0.3

50 0.24 110 <50 9 170

150 0.64 280 <50 25 760 8

80 0.39 150 <50 18 1150 12

60 0.29 130 <50 21 550 18 0.6

60 0.37 200 <50 37 2640 36

90 0.12 10 <50 80 60 Blank

40 0.17 90 <50 14 600 11 1.4

30 0.17 80 <50 8 70 16 2.1

<10 0.05 20 <50 <5 100 7

10 0.09 50 <50 8 140 6

20 0.13 60 <50 11 390 13

<10 0.04 30 <50 9 360 15 1.8

10 0.13 60 <50 <5 110 10

40 0.24 90 <50 16 570 21

20 0.13 60 <50 11 1330 26 2.2

40 0.29 110 <50 15 730 26

280 0.35 170 <50 17 2600 311 53.7 ME-12

20 0.11 70 <50 10 390 27

20 0.11 70 <50 10 750 30 3.3

40 0.28 90 <50 14 320 18

50 0.32 120 <50 14 270 23

60 0.2 80 <50 13 450 19 1.6

210 0.73 290 <50 22 180 <5

70 0.58 230 <50 22 310 12

30 0.21 110 <50 8 260 9 0.8

70 0.72 350 <50 25 140 <5

80 1.03 380 <50 35 500 <5

100 0.13 10 <50 80 50 <5 Blank

90 0.96 360 <50 35 130 <5

100 0.92 330 <50 34 100 <5

170 0.99 360 <50 34 110 <5

110 1.01 360 <50 35 120 <5

90 0.99 360 <50 34 120 <5

110 0.98 360 <50 33 150 <5 <0.3

100 0.99 380 <50 33 110 <5

270 0.92 340 <50 29 120 <5

330 0.83 290 <50 28 110 <5

100 1.02 370 <50 34 90 <5

390 0.32 150 <50 17 8920 1260 ME-11

90 0.7 260 <50 27 170 7

70 0.56 200 <50 23 250 <5

40 0.26 90 <50 14 180 5 0.8

20 0.04 30 <50 6 180 5 1

70 0.31 140 <50 17 300 8

170 0.65 300 <50 21 110 <5

110 0.51 290 <50 19 60

90 0.58 300 <50 22 70

80 0.55 300 <50 17 70

50 0.49 260 <50 15 60 95 2.1

100 0.12 10 <50 79 110 <5 <0.3 Blank

70 0.56 290 <50 20 50

80 0.65 350 <50 21 60

1070 0.86 310 <50 24 80 <10 6

1060 0.91 320 <50 25 80 <10 <5

140 0.7 310 <50 22 210

470 0.57 220 <50 19 130 5 <0.3

270 0.68 280 <50 22 270

第 8 页，共 10 页

备 注

Sr

ppm

Ti

%

V

ppm

W

ppm

Y

ppm

Zn

ppm

Au

ppb

Ag

g/t

Pt

ppb

Pd

ppbNote

分析结果/Assay Result

基本析样品取样及分析结果登记表Sample Log

70 0.77 330 <50 24 490

40 0.77 360 <50 23 320 <5 0.3

30 0.78 370 <50 21 170

250 0.33 150 <50 16 2380 ME-12

40 0.74 350 <50 23 140

60 0.77 340 <50 25 90

90 1.03 400 <50 36 150

90 0.67 260 <50 24 150 6 <0.3

680 0.17 30 <50 <5 40

340 0.26 80 <50 13 1460

60 0.43 140 <50 19 370 10 0.5

120 0.97 360 <50 34 130

110 1.01 380 <50 33 140

100 1.11 410 <50 37 120

110 0.12 10 <50 79 50 Blank

110 1.22 280 <50 42 140

100 1.03 170 <50 48 110

100 1.06 160 <50 48 130

80 0.55 110 <50 29 220 5 <0.3

80 0.36 110 <50 21 410 6 <0.3

80 0.33 130 <50 18 320 <5 <0.3

80 0.6 280 <50 22 120

60 1.11 160 <50 49 110

50 0.33 130 <50 15 1130 6 1.4

50 0.23 90 <50 14 350

390 0.32 150 <50 18 9180 ME-11

80 0.88 150 <50 40 220

70 1.09 160 <50 50 180

90 1.11 150 <50 53 150

60 0.46 170 <50 15 170

30 0.44 170 <50 16 250

240 0.42 150 <50 14 310 5 <0.3

380 0.53 220 <50 17 230

370 0.44 200 <50 20 530 8 <0.3 Additonal Sampling840 0.45 180 <50 18 140 Additonal Sampling950 0.5 210 <50 20 110 Additonal Sampling110 0.12 10 <50 89 50 Blank

80 0.39 250 <50 16 150 Additonal Sampling70 0.54 250 <50 21 160 Additonal Sampling70 0.94 320 <50 35 70 Additonal Sampling70 1.45 440 <50 38 110 Additonal Sampling

1140 0.8 290 <50 24 80 <5 <10 <5 Additonal Sampling1150 0.79 290 <50 23 80 <5 <10 <5 Additonal Sampling50 0.71 330 <50 25 190

90 0.74 330 <50 24 140

140 0.81 360 <50 25 100

100 0.58 300 <50 23 190

260 0.35 160 <50 17 2570 ME-12

150 0.8 360 <50 23 100

70 0.84 410 <50 36 160

80 0.86 400 <50 33 150

70 0.81 390 <50 34 180

100 0.43 260 <50 18 160

80 0.45 270 <50 17 100

80 0.45 260 <50 16 210

80 0.06 <10 <50 7 20

110 0.36 210 <50 15 140

110 0.05 <10 <50 6 20

90 0.12 10 <50 83 60 Blank

110 0.48 290 <50 17 130

110 0.53 300 <50 16 120

130 0.3 210 <50 13 200

<10 0.03 50 <50 <5 60

600 0.25 110 <50 11 140

530 0.15 60 <50 6 90

60 0.05 50 <50 <5 50

180 0.17 130 <50 9 160

810 0.19 50 <50 7 50

10 0.02 50 <50 <5 110 25 2.8

350 0.32 140 <50 17 9120 1240 76.5 ME-11

20 0.04 20 <50 7 70

20 0.04 30 <50 6 90

50 0.08 40 <50 6 190 12 0.9

50 0.13 50 <50 8 260 23 0.9

130 0.17 140 <50 10 150

80 0.24 190 <50 13 290

60 0.18 80 <50 13 480 10 0.5

90 0.29 250 <50 16 170

110 0.3 250 <50 17 180

10 0.1 60 <50 6 210

80 0.12 10 <50 75 50 Blank

40 0.12 70 <50 9 260

40 0.17 80 <50 9 320 7 0.6

10 0.05 30 <50 <5 150

80 0.06 <10 <50 5 30

110 0.05 <10 <50 5 20

30 0.07 40 <50 9 110

10 0.04 60 <50 9 210

10 0.02 40 <50 7 90

20 0.02 50 <50 8 230 9 0.8

10 0.03 60 <50 7 100 11 0.8

260 0.35 170 <50 17 2690 ME-12

10 0.01 40 <50 6 180

<10 0.03 60 <50 15 60

第 9 页，共 10 页

备 注

Sr

ppm

Ti

%

V

ppm

W

ppm

Y

ppm

Zn

ppm

Au

ppb

Ag

g/t

Pt

ppb

Pd

ppbNote

分析结果/Assay Result

基本析样品取样及分析结果登记表Sample Log

<10 0.03 60 <50 9 150

<10 0.04 60 <50 11 590 26 1.2

20 0.06 50 <50 7 160

20 0.03 50 <50 6 200

<10 0.03 50 <50 6 110

<10 0.02 50 <50 8 130 14 1

<10 0.04 50 <50 11 250

20 0.03 50 <50 <5 130 15 0.6

90 0.12 10 <50 78 50 <5 <0.3 Blank

20 0.05 50 <50 <5 250

20 0.07 60 <50 7 1060

20 0.05 50 <50 5 240 21 0.8

20 0.07 50 <50 5 170

60 0.22 80 <50 16 220

70 0.31 100 <50 16 110 8 <0.3

70 0.23 90 <50 16 110 11 0.4

10 0.17 70 <50 10 70 25 0.5

10 0.13 100 <50 10 120

40 0.38 140 <50 18 330

340 0.34 150 <50 17 9140 ME-11

50 0.3 130 <50 19 230

60 0.33 120 <50 18 380 5 0.3

80 0.43 140 <50 21 430

30 0.24 100 <50 12 250

<10 0.1 80 <50 8 360

20 0.1 70 <50 6 80 9 0.4

20 0.09 60 <50 9 140

60 0.05 10 <50 <5 20

20 0.06 50 <50 8 150 12 <0.3

<10 0.03 60 <50 10 50

90 0.13 10 <50 86 60 Blank

<10 0.01 <10 <50 <5 40 <5 1.4

<10 <0.01 <10 <50 <5 20

<10 0.02 50 <50 5 60

10 0.02 60 <50 10 60

20 0.04 50 <50 8 60

<10 0.04 80 <50 19 100

10 0.02 30 <50 10 60

10 0.03 60 <50 13 90

10 0.03 60 <50 10 80 <5 0.5

<10 0.01 60 <50 11 50

240 0.36 160 <50 18 2640 332 48.3 ME-12

<10 0.02 50 <50 12 80

<10 <0.01 40 <50 <5 40

10 0.03 60 <50 7 90 12 1

<10 0.02 40 <50 9 50

50 0.03 60 <50 11 50

90 0.04 50 <50 10 120

<10 0.02 20 <50 <5 50

20 0.02 60 <50 10 60

10 0.05 70 <50 9 90 <5 0.9

70 0.06 <10 <50 5 20

80 0.13 10 <50 78 80 Blank

20 0.07 60 <50 13 90

20 0.03 50 <50 9 60

10 0.02 50 <50 7 50

<10 0.02 30 <50 <5 20

10 0.03 60 <50 14 70

<10 0.03 50 <50 8 80 9 0.7

10 0.06 60 <50 8 80

130 0.12 30 <50 7 100

150 0.06 10 <50 <5 40

70 0.57 250 <50 23 330

340 0.33 150 <50 18 9170 ME-11

80 0.69 320 <50 26 110

50 0.57 290 <50 23 160

60 0.58 320 <50 25 270

70 0.71 350 <50 30 380

40 0.69 350 <50 29 110 <5 <0.3

40 0.94 420 <50 33 130

50 0.95 430 <50 36 150

30 0.51 260 <50 22 170

60 1.03 460 <50 40 160

20 0.11 70 <50 6 30

90 0.13 20 <50 81 90 Blank

30 0.24 140 <50 12 60

100 0.2 130 <50 11 60 <5 <0.3

150 0.16 80 <50 7 40 <5 <0.3

<10 <0.01 10 <50 <5 10

240 0.59 280 <50 24 120 <5 <0.3

50 0.36 170 <50 17 470

<5 4.8

第 10 页，共 10 页

Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd

Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323

Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5

Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb

RL.H-1 10.6 90 180 <5 1.1 <10 670 100 390 7.99 2.7 10 40 1.41 1560 <10 280 0.05 70 <50 40 <50 140 0.61 300 <50 29 2100

RL.H-2 10.7 40 170 <5 0.5 <10 730 90 260 7.56 2.7 10 30 1.12 1700 <10 260 0.02 60 <50 40 <50 90 0.61 290 <50 19 1680

RL.H-3 10.8 <30 170 <5 0.7 <10 700 80 370 7.91 2.6 10 40 1.25 1980 <10 220 0.03 60 <50 41 <50 100 0.62 290 <50 19 2050

RL.H-4 10.4 90 190 <5 0.5 <10 690 70 260 7.04 2.6 10 40 1.26 1890 <10 250 0.02 60 <50 40 <50 70 0.6 290 <50 21 930

RL.H-5 10.3 <30 170 <5 0.8 <10 680 120 520 9.75 2.5 10 40 1.25 1740 <10 350 0.02 80 <50 40 <50 80 0.58 290 <50 18 1460

RL.H-6 10.7 <30 160 <5 1 <10 710 90 370 8.73 2.5 10 30 1.15 2010 <10 270 0.02 60 <50 41 <50 80 0.61 300 <50 22 1290

RL.H-7 10.2 <30 160 <5 1.1 <10 700 80 380 9.75 2.2 <10 30 1.14 2620 <10 240 0.02 50 <50 41 <50 60 0.58 290 <50 19 1000

RL.H-8 10.1 <30 150 <5 0.7 <10 760 100 330 11.4 2.1 10 30 1 2590 <10 290 0.02 40 <50 41 <50 50 0.58 310 <50 18 830

RL.H-9 1.73 <30 10 <5 3.8 <10 120 30 100 25.6 0.2 <10 <10 3.02 3860 <10 80 0.08 <20 <50 5 <50 30 0.1 80 <50 14 150

RL.H-10 2.39 <30 70 <5 3.3 <10 160 40 110 27.1 0.4 <10 20 3.3 2850 <10 80 0.06 <20 <50 8 <50 30 0.14 90 <50 11 290

RL.H-11 7.15 <30 480 5 0.7 <10 10 <10 <10 1.54 4.3 90 40 0.17 330 <10 <10 0.02 20 <50 <5 <50 90 0.12 10 <50 82 50

RL.H-12 4.68 50 160 <5 2.8 <10 300 70 170 22 1.1 <10 30 2.43 3030 <10 150 0.04 20 <50 16 <50 40 0.25 150 <50 15 440 253 <0.3

RL.H-13 2.84 <30 130 <5 3 <10 240 50 280 26.3 0.4 <10 20 2.86 3850 <10 100 0.06 <20 <50 11 <50 40 0.16 110 <50 12 510

RL.H-14 1.33 50 20 <5 4 <10 200 30 100 27.3 0.2 <10 <10 3.27 4270 <10 60 0.08 <20 <50 <5 <50 40 0.07 70 <50 12 260

RL.H-15 2.14 <30 50 <5 2.4 <10 140 50 310 27.6 0.1 <10 <10 2.55 3600 <10 120 0.08 <20 <50 6 <50 30 0.11 80 <50 12 970 63 0.3

RL.H-16 0.68 <30 10 <5 3.3 <10 40 <10 40 24.9 <0.1 <10 <10 2.93 4390 <10 30 0.06 <20 <50 <5 <50 20 0.03 40 <50 9 80

RL.H-17 7.7 80 130 <5 2.2 <10 320 70 200 14 0.7 30 50 1.58 2010 <10 160 0.04 30 <50 20 <50 100 0.34 160 <50 17 880

RL.H-18 9.98 <30 230 <5 3.1 <10 220 50 330 7.43 1.2 60 50 1.53 950 <10 100 0.05 40 <50 20 <50 220 0.48 110 <50 42 590

RL.H-19 7.82 <30 190 <5 3.2 <10 230 90 550 11.1 1 20 40 1.65 1170 <10 170 0.05 60 <50 19 <50 180 0.41 140 <50 19 1130 43 0.6

RL.H-20 4.12 80 80 <5 2.2 <10 180 80 1960 13.2 0.6 <10 30 1.47 1270 <10 140 0.02 30 <50 14 <50 60 0.21 100 4370 9 870

RL.H-21 4.44 90 80 <5 2.1 <10 220 110 610 17 0.8 <10 30 1.94 1860 <10 200 0.03 50 <50 13 <50 40 0.23 130 420 14 1610

RL.H-22 7.4 100 590 <5 0.8 20 30 20 4450 4.85 4.8 10 10 0.88 520 170 30 0.1 2080 70 12 260 270 0.35 160 <50 18 2610

RL.H-23 5.84 <30 130 <5 1 <10 300 80 370 15.3 1 10 50 1.19 1840 <10 140 0.04 40 <50 18 <50 50 0.35 150 <50 14 1010

RL.H-24 4.74 80 140 <5 0.7 <10 110 120 560 22.7 0.9 10 30 0.77 1070 <10 230 0.03 50 <50 12 <50 50 0.25 110 <50 13 1580 31 1

RL.H-25 3.89 70 110 <5 1.1 <10 110 120 690 24.9 0.7 <10 20 1.2 1360 <10 210 0.02 50 <50 12 <50 30 0.2 120 <50 11 1160

RL.H-26 0.56 <30 <10 <5 2 <10 30 20 100 10.5 <0.1 <10 <10 1.58 2030 <10 30 0.03 <20 <50 <5 <50 20 0.03 30 <50 8 90

RL.H-27 0.89 <30 10 <5 3 <10 40 20 100 18.5 <0.1 <10 <10 2.72 3580 <10 40 0.05 <20 <50 <5 <50 30 0.05 50 <50 10 120

RL.H-28 5.81 40 100 <5 2.8 <10 290 50 150 15.5 0.8 10 50 2.04 2590 <10 110 0.03 <20 <50 16 <50 40 0.29 140 <50 14 630

RL.H-29 8.09 <30 270 <5 1.2 <10 300 80 440 14.6 1.7 20 60 1.36 1750 <10 170 0.04 30 <50 22 <50 80 0.41 180 <50 19 1100 31 <0.3

RL.H-30 2 <30 <10 <5 3.1 <10 130 60 240 20.4 0.2 <10 10 2.17 3180 <10 180 0.03 <20 <50 <5 <50 30 0.12 60 <50 11 180

RL.H-31 3.52 <30 60 <5 2.1 <10 250 50 540 22 0.2 <10 20 1.83 2880 <10 160 0.03 <20 <50 11 <50 20 0.2 110 <50 13 530

RL.H-32 4.17 <30 <10 <5 1.8 <10 310 40 290 22.6 <0.1 <10 20 2.08 4340 <10 130 0.04 <20 <50 13 <50 <10 0.25 130 <50 14 240

RL H 33 6 96 <30 380 <5 0 7 <10 10 <10 20 1 78 4 2 80 40 0 16 360 <10 <10 0 02 30 <50 <5 <50 90 0 12 10 <50 81 50

Richardson Lake 2011 Assay Results

RL.H-33 6.96 <30 380 <5 0.7 <10 10 <10 20 1.78 4.2 80 40 0.16 360 <10 <10 0.02 30 <50 <5 <50 90 0.12 10 <50 81 50

RL.H-34 2.09 <30 20 <5 2.8 <10 140 30 130 17.8 0.1 <10 10 2.27 2990 <10 90 0.05 <20 <50 6 <50 10 0.13 70 <50 11 210

RL.H-35 2.69 <30 100 <5 1.9 <10 190 40 360 17.3 0.5 <10 20 1.76 1940 <10 120 0.05 <20 <50 9 <50 10 0.16 90 <50 11 950 76 <0.3

RL.H-36 1.98 <30 20 <5 3.6 <10 240 30 370 15.4 0.2 <10 10 2.27 3100 <10 100 0.05 <20 <50 7 <50 <10 0.16 80 <50 13 350

RL.H-37 1.32 <30 <10 <5 1.9 <10 60 10 40 20.3 <0.1 <10 <10 1.98 5080 <10 50 0.03 <20 <50 <5 <50 10 0.07 40 <50 10 80

RL.H-38 0.77 <30 120 <5 2.1 <10 170 <10 10 17.7 0.2 <10 <10 2.59 5080 <10 70 0.03 <20 <50 <5 <50 80 0.05 40 <50 8 50

RL.H-39 1.8 <30 280 <5 3 <10 310 10 30 15.9 0.3 <10 10 3.32 4370 <10 100 0.05 <20 <50 6 <50 300 0.12 70 <50 10 80

RL.H-40 3.1 <30 80 <5 5.1 <10 140 10 70 9.38 0.3 <10 20 2.47 3130 10 50 0.04 <20 <50 7 <50 60 0.16 80 <50 13 140

RL.H-41 5.29 80 110 <5 2.5 <10 90 50 230 17.6 0.6 30 30 1.14 1330 <10 170 0.05 20 <50 11 <50 80 0.24 90 <50 21 290 29 0.3

RL.H-42 5.62 40 100 <5 2.4 <10 350 170 680 17.4 0.7 <10 30 1.31 1290 <10 260 0.04 30 <50 17 <50 90 0.32 150 <50 11 440

RL.H-43 8.38 <30 170 <5 2 <10 470 40 430 9.51 1.2 20 50 1.36 1600 <10 190 0.02 20 <50 25 <50 110 0.41 170 <50 27 310

RL.H-44 6.06 460 1520 <5 2.6 60 350 30 25900 6.75 2.4 20 20 1.89 940 1280 260 0.13 7850 90 12 110 380 0.32 150 <50 17 8990

RL.H-45 6.79 60 140 <5 2.4 <10 460 110 480 17.2 0.9 <10 40 1.39 1260 <10 260 0.03 20 <50 24 <50 90 0.34 180 <50 17 2000 61 0.6

RL.H-46 1.86 <30 40 <5 4.3 <10 150 90 390 16.1 0.4 <10 10 2.22 2800 <10 160 0.05 <20 <50 8 <50 20 0.13 80 <50 12 1320

RL.H-47 6.18 40 180 <5 14.6 <10 380 50 180 6.86 2.2 <10 20 2.3 3370 <10 130 0.04 <20 <50 32 <50 90 0.8 300 <50 21 170

RL.H-48 6.73 30 240 <5 7.6 <10 410 50 100 8.46 1.8 10 20 2.6 2510 <10 170 0.06 <20 <50 28 <50 120 0.68 250 <50 29 250

RL.H-49 7.82 <30 180 <5 3.4 <10 550 70 310 12 1.6 10 30 1.49 1350 <10 140 0.02 <20 <50 28 <50 90 0.44 220 <50 17 640

RL.H-50 7.69 30 140 <5 3.2 <10 680 50 140 11.1 1.4 10 30 1.48 1500 <10 130 0.02 <20 <50 31 <50 80 0.43 230 <50 17 670

RL.H-51 6.92 <30 130 <5 3.3 <10 420 70 130 13.3 1.2 <10 20 1.57 1710 <10 150 0.04 <20 <50 26 <50 80 0.4 200 <50 14 240 30 <0.3

RL.H-52 5.36 <30 80 <5 2.9 <10 210 40 130 10.2 0.6 10 20 1.15 1480 <10 110 0.01 <20 <50 16 <50 70 0.3 140 <50 10 190

RL.H-53 5.91 <30 90 <5 2.4 <10 230 40 100 11.8 0.8 <10 20 1.02 1270 <10 130 0.03 20 <50 18 <50 70 0.3 140 <50 10 250 41 <0.3

RL.H-54 9.64 <30 170 <5 2.4 <10 420 30 140 6.57 1.5 10 50 1.26 1880 <10 170 0.04 <20 <50 34 <50 120 0.53 250 <50 15 180

RL.H-55 7.18 <30 380 <5 0.7 <10 <10 <10 <10 1.54 4.5 90 40 0.16 320 <10 10 0.01 20 <50 <5 <50 90 0.12 10 <50 77 40

RL.H-56 3.22 <30 80 <5 7.4 <10 140 50 190 19.5 0.6 <10 20 2.83 3780 <10 170 0.02 <20 <50 16 <50 40 0.18 130 <50 15 130

第 1 页，共 9 页

Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd

Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323

Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5

Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb

Richardson Lake 2011 Assay Results

RL.H-57 2 30 10 <5 6.3 <10 130 110 210 22.2 0.2 <10 <10 2.53 4090 50 190 0.01 <20 <50 8 <50 20 0.11 90 <50 11 260 19 0.3

RL.H-58 1.53 <30 20 <5 4.2 <10 100 20 80 8.18 0.2 <10 <10 1.66 2680 <10 70 0.01 <20 <50 5 <50 20 0.1 60 <50 8 140

RL.H-59 0.24 <30 <10 <5 6.3 <10 20 20 70 8.49 <0.1 <10 <10 2.43 3960 <10 70 0.03 <20 <50 <5 <50 <10 0.02 20 <50 8 50

RL.H-60 1.81 <30 <10 <5 8.6 <10 100 20 120 14.8 <0.1 <10 <10 3.4 5970 <10 130 0.01 <20 <50 6 <50 20 0.1 70 <50 12 100

RL.H-61 1.79 <30 <10 <5 6.1 <10 70 40 130 15.6 <0.1 <10 <10 2.53 4870 <10 140 0.01 <20 <50 5 <50 30 0.1 60 <50 10 130 28 <0.3

RL.H-62 4.41 <30 30 <5 6.4 <10 90 20 110 12.9 0.4 <10 10 2.6 4900 <10 120 0.03 <20 <50 10 <50 50 0.21 100 <50 11 190

RL.H-63 7.98 30 130 <5 2 <10 310 40 60 6.41 1.5 20 50 0.9 1110 <10 140 0.03 <20 <50 21 <50 100 0.38 160 <50 11 160

RL.H-64 6.77 30 90 <5 2.1 <10 190 40 90 6.71 0.8 10 40 0.9 1200 <10 140 0.03 <20 <50 21 <50 80 0.41 170 <50 11 190 23 <0.3

RL.H-65 4.93 <30 80 <5 3.1 <10 170 30 70 5.77 0.4 <10 20 1.16 1750 <10 110 0.02 <20 <50 19 <50 70 0.31 140 <50 8 140

RL.H-66 7.45 100 590 <5 0.7 20 30 20 4500 4.76 4.7 10 10 0.88 520 180 30 0.09 2120 70 12 270 280 0.35 170 <50 17 2580

RL.H-67 8 <30 180 <5 7.8 <10 120 30 70 7.29 0.5 10 20 3.81 2740 <10 70 0.1 <20 <50 23 <50 820 0.37 180 <50 11 130

RL.H-68 5.21 <30 210 <5 9.2 <10 190 50 110 7.84 0.5 <10 <10 3.35 3940 <10 200 0.02 <20 <50 23 <50 110 0.28 160 <50 18 110

RL.H-69 8.11 <30 20 <5 7.8 <10 280 50 120 9.34 0.2 <10 40 4.25 1780 <10 130 0.03 <20 <50 42 <50 120 0.53 290 <50 19 90

RL.H-70 7.93 <30 10 <5 8.9 <10 270 50 130 8.85 <0.1 <10 20 3.93 1700 <10 120 0.03 <20 <50 40 <50 150 0.5 280 <50 18 90 <5 <0.3

RL.H-71 7.75 <30 40 <5 12.5 <10 270 50 170 6.41 0.1 <10 10 2.2 1720 <10 140 0.04 <20 <50 38 <50 90 0.49 260 <50 20 80

RL.H-72 8.75 <30 820 <5 3.9 <10 100 70 360 6.79 1.9 20 30 2.35 760 <10 120 0.12 <20 <50 21 <50 650 0.48 200 <50 20 180

RL.H-73 7.76 <30 50 <5 8.9 <10 360 50 150 7.07 0.2 <10 20 4.37 1690 <10 80 0.01 <20 <50 44 <50 130 0.45 280 <50 16 80

RL.H-74 4.58 <30 40 6 18.4 <10 90 30 120 4.71 0.3 <10 30 2.8 2940 <10 50 0.04 <20 <50 27 <50 50 0.31 180 <50 18 80 <5 <0.3

RL.H-75 6.1 <30 180 <5 8 <10 160 130 1350 13.1 0.6 <10 30 3.15 1970 <10 190 0.01 <20 <50 34 <50 80 0.4 260 <50 15 80

RL.H-76 7.45 <30 90 <5 9.9 <10 210 50 130 8.45 0.5 <10 20 3.61 2040 <10 160 0.02 <20 <50 41 <50 110 0.48 280 <50 18 120

RL.H-77 6.82 <30 400 5 0.8 <10 40 <10 <10 1.42 4.3 80 40 0.19 320 <10 <10 0.02 <20 <50 <5 <50 90 0.12 10 <50 77 40

RL.H-78 6.36 <30 160 <5 11.7 <10 180 40 190 7.63 0.4 <10 20 3.5 1920 <10 100 0.01 <20 <50 34 <50 80 0.41 240 <50 16 100

RL.H-79 7.74 <30 230 <5 6 <10 150 50 460 7.79 1.6 <10 20 2.06 1030 <10 90 0.04 <20 <50 29 <50 90 0.43 210 <50 19 290

RL.H-80 6.44 <30 140 <5 3 <10 80 120 630 11.1 1.2 20 20 1.37 570 <10 110 0.03 30 <50 10 <50 70 0.27 80 <50 14 1360 29 2.1

RL.H-81 7.97 <30 200 <5 3.8 <10 210 60 620 7.32 2.1 20 20 1.86 600 <10 80 0.04 30 <50 17 <50 80 0.35 110 <50 17 630 22 1.6

RL.H-82 7.09 40 240 <5 3.4 <10 100 70 710 6.28 2.1 10 10 1.69 610 <10 90 0.03 40 <50 19 <50 60 0.32 120 <50 15 1380

RL.H-83 10.6 80 350 <5 5.5 <10 190 60 320 4.52 2.7 10 20 3.37 630 <10 90 0.03 <20 <50 43 <50 120 0.49 270 <50 15 210

RL.H-84 4.74 350 140 <5 2.6 <10 60 40 170 4.69 1.1 10 60 1.65 430 <10 50 0.02 <20 <50 8 <50 40 0.16 50 <50 10 70

RL.H-85 7.22 70 220 <5 1.8 <10 60 30 130 7.5 2 10 80 2.18 540 <10 70 0.05 <20 <50 15 <50 50 0.31 90 <50 16 110

RL.H-86 2.82 <30 110 <5 6.2 <10 110 30 290 14.7 0.6 <10 <10 3.86 1800 <10 100 0.07 <20 <50 6 <50 180 0.14 60 <50 12 110 21 0.8

RL.H-87 6.38 <30 600 <5 5 <10 800 40 70 7.52 1.4 30 10 7.54 1230 <10 430 0.16 <20 <50 19 <50 940 0.41 160 <50 16 110

RL.H-88 5.81 460 1480 <5 2.6 60 380 30 24700 6.73 2.4 20 20 1.8 920 1250 350 0.13 7720 80 12 110 350 0.31 150 <50 17 9110 1410 78.4

RL H 89 5 69 80 170 <5 1 <10 80 90 670 8 62 1 5 10 40 1 86 330 <10 90 0 04 30 <50 12 <50 50 0 24 70 <50 14 1230RL.H-89 5.69 80 170 <5 1 <10 80 90 670 8.62 1.5 10 40 1.86 330 <10 90 0.04 30 <50 12 <50 50 0.24 70 <50 14 1230

RL.H-90 7.6 40 300 <5 2 <10 90 100 990 7.92 2.9 20 10 1.35 510 <10 120 0.06 30 <50 18 <50 50 0.32 100 <50 18 1610

RL.H-91 7.22 <30 270 <5 2.2 <10 70 60 560 12 2.6 20 20 1.84 1520 <10 100 0.04 30 <50 16 <50 40 0.29 100 <50 18 1660 64 0.8

RL.H-92 0.42 <30 <10 <5 2.6 <10 60 <10 70 18.8 <0.1 <10 <10 2.38 2660 <10 20 0.06 <20 <50 <5 <50 20 0.02 30 <50 7 170

RL.H-93 0.94 <30 10 <5 5 <10 20 10 160 17.2 0.2 <10 <10 2.83 2990 <10 20 0.04 <20 <50 <5 <50 30 0.04 30 <50 9 200

RL.H-94 6.49 <30 320 <5 1.3 <10 30 30 220 6.2 3.7 20 <10 0.84 540 <10 130 0.08 <20 <50 11 <50 50 0.35 60 <50 19 680

RL.H-95 6.49 <30 360 <5 1.1 <10 60 40 280 5.86 3.7 20 10 0.99 340 <10 110 0.05 <20 <50 12 <50 40 0.3 70 <50 20 1600

RL.H-96 7.36 50 420 <5 1.1 <10 90 40 310 4.87 4.1 20 10 0.98 350 <10 140 0.05 30 <50 15 <50 40 0.32 90 <50 20 1550

RL.H-97 6.54 40 370 <5 1.3 <10 120 50 470 6.06 3.3 20 10 1.36 530 <10 140 0.03 <20 <50 14 <50 40 0.25 80 <50 19 880 12 <0.3

RL.H-98 6.6 <30 340 <5 1 <10 60 30 260 6.24 3.4 30 10 1.32 420 <10 80 0.05 <20 <50 12 <50 30 0.31 80 <50 21 190

RL.H-99 6.9 <30 480 <5 0.8 <10 20 <10 <10 1.29 4.3 80 40 0.15 300 <10 <10 0.02 <20 <50 <5 <50 100 0.12 10 <50 78 50

RL.H-100 7.18 <30 380 <5 1.4 <10 110 30 130 5.13 3.7 30 20 1.41 420 <10 90 0.05 <20 <50 13 <50 40 0.27 80 <50 22 140

RL.H-101 7.17 <30 390 <5 0.7 <10 100 40 620 5.15 3.9 20 20 1.43 340 <10 100 0.04 <20 <50 13 <50 30 0.25 90 1280 23 350

RL.H-102 7.15 <30 450 <5 1.6 <10 100 60 300 5.88 4.2 20 10 1.47 410 <10 120 0.04 <20 <50 14 <50 40 0.27 90 <50 15 770

RL.H-103 7.98 <30 350 <5 2.9 <10 140 60 150 9.7 3.5 20 30 3.01 730 <10 130 0.03 <20 <50 32 <50 50 0.39 210 <50 19 90

RL.H-104 6.87 <30 430 <5 2.3 <10 70 20 260 4.07 3.2 20 10 1.87 480 <10 80 0.06 <20 <50 10 <50 40 0.21 60 <50 16 60

RL.H-105 6.36 <30 400 <5 1.6 <10 60 30 180 5.5 3.2 20 10 1.54 830 <10 70 0.04 <20 <50 11 <50 30 0.27 70 <50 16 190

RL.H-106 5.66 <30 280 <5 3.1 <10 80 50 390 7.52 2.6 20 <10 1.61 1230 <10 120 0.04 <20 <50 11 <50 40 0.22 80 <50 15 910 36 0.4

RL.H-107 7.78 <30 400 <5 1 <10 120 60 210 6.37 3.9 20 20 2.09 520 <10 130 0.05 <20 <50 17 <50 20 0.34 110 <50 18 140

RL.H-108 8.03 <30 500 <5 1 <10 80 30 40 4.52 3.7 20 30 2.15 440 <10 90 0.05 <20 <50 14 <50 20 0.36 90 <50 18 60

RL.H-109 6.45 <30 190 <5 5.3 <10 120 30 40 6.33 1.2 <10 20 4.92 1020 <10 100 0.02 <20 <50 24 <50 40 0.31 160 <50 11 80

RL.H-110 7.39 100 580 <5 0.9 20 50 20 4450 4.81 4.9 10 10 0.87 530 160 40 0.1 2060 70 11 270 270 0.35 160 <50 18 2600

RL.H-111 8.14 <30 300 <5 9 <10 160 50 80 7.58 1.6 <10 10 4.39 1390 <10 130 0.02 <20 <50 38 <50 50 0.42 250 <50 14 100

RL.H-112 7.43 <30 30 <5 8.1 <10 160 40 40 9.07 0.4 <10 30 3.73 1520 <10 90 0.09 <20 <50 36 <50 100 1.3 370 <50 35 100

第 2 页，共 9 页

Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd

Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323

Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5

Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb

Richardson Lake 2011 Assay Results

RL.H-113 8.08 <30 30 <5 7.4 <10 310 50 70 7.83 0.4 <10 30 3.69 1870 <10 110 0.03 <20 <50 42 <50 90 0.56 300 <50 20 150

RL.H-114 7.79 <30 40 <5 6.9 <10 300 50 90 8.15 0.5 <10 40 3.98 1960 <10 110 0.02 <20 <50 41 <50 100 0.47 270 <50 18 140

RL.H-115 7.9 <30 40 <5 8.5 <10 310 50 160 7.95 0.5 <10 30 3.41 2200 <10 110 0.02 <20 <50 41 <50 90 0.47 280 <50 18 170

RL.H-116 7.9 <30 10 <5 12 <10 300 40 60 7.44 0.2 <10 20 2.97 2600 10 110 0.02 <20 <50 41 <50 120 0.46 290 <50 18 170

RL.H-117 7.57 <30 20 <5 8.2 <10 280 50 80 6.81 0.2 <10 20 3 1840 20 110 0.01 <20 <50 40 <50 100 0.45 260 <50 17 100 <5 <0.3

RL.H-118 8.06 <30 50 <5 9 <10 310 50 60 7.34 0.4 <10 20 3.16 2010 10 110 0.02 <20 <50 43 <50 70 0.48 280 <50 18 110

RL.H-119 7.73 <30 20 <5 10.5 <10 280 40 50 7.52 0.3 <10 20 3.09 2270 30 110 0.02 <20 <50 38 <50 130 0.42 280 <50 17 180

RL.H-120 1.69 <30 <10 <5 2.6 <10 130 100 840 >30 <0.1 <10 <10 0.49 500 70 100 <0.01 <20 <50 <5 <50 40 0.07 80 <50 5 50

RL.H-121 6.95 <30 470 <5 0.9 <10 20 <10 <10 1.35 4.2 70 40 0.17 300 10 <10 0.01 <20 <50 <5 <50 100 0.12 10 <50 75 50

RL.H-122 6.37 <30 60 <5 7.8 <10 170 20 230 7.09 0.6 <10 20 3.08 1360 140 70 0.03 <20 <50 30 <50 110 0.43 210 <50 20 150 <5 <0.3

RL.H-123 7.94 <30 50 <5 8.2 <10 210 40 150 7.44 0.8 <10 40 3.96 1490 <10 90 0.02 <20 <50 40 <50 130 0.63 280 <50 23 120 <5 <0.3

RL.H-124 7.76 <30 80 <5 7.9 <10 330 50 80 8.08 1.7 <10 60 4.83 1460 20 120 0.02 <20 <50 40 <50 150 0.43 250 <50 16 180

RL.H-125 7.56 <30 20 <5 8.4 <10 280 40 90 8.05 0.6 <10 30 4.51 1570 <10 110 0.02 <20 <50 40 <50 190 0.42 260 <50 17 150

RL.H-126 7.96 <30 300 <5 3.1 <10 10 <10 <10 1.42 1.8 10 40 0.92 300 <10 10 0.03 <20 <50 <5 <50 100 0.16 20 <50 <5 30

RL.H-127 7.89 <30 340 <5 3.2 <10 100 <10 <10 1.37 1.6 <10 40 0.94 320 <10 <10 0.03 <20 <50 <5 <50 80 0.16 20 <50 <5 30

RL.H-128 7.16 <30 10 <5 11.5 <10 260 40 40 7.37 0.2 <10 20 3.97 2110 <10 90 0.02 <20 <50 40 <50 130 0.44 260 <50 20 160

RL.H-129 7.75 <30 10 <5 9.4 <10 270 40 100 7.88 0.4 <10 20 3.75 1700 30 100 0.02 <20 <50 41 <50 180 0.46 260 <50 19 120

RL.H-130 7.64 <30 20 <5 9.6 <10 250 30 90 7.08 0.4 <10 30 3.48 1460 <10 80 0.02 <20 <50 38 <50 90 0.42 250 <50 20 180

RL.H-131 2.34 50 30 <5 3.7 <10 60 120 2200 >30 0.4 <10 20 1.92 880 80 140 0.01 <20 <50 16 <50 30 0.18 100 <50 13 290 34 1.4

RL.H-132 5.91 460 1460 <5 2.7 60 370 30 25700 6.67 2.4 20 20 1.84 940 1260 260 0.13 7840 90 12 110 350 0.31 140 <50 17 9240

RL.H-133 1.6 90 10 <5 4 <10 60 100 5540 >30 0.2 <10 <10 1.63 720 110 120 <0.01 40 <50 8 <50 20 0.09 90 <50 5 300 20 4.6

RL.H-134 8.06 <30 60 <5 8.5 <10 300 40 190 7.71 0.6 <10 20 3.9 1730 <10 110 0.04 <20 <50 44 <50 90 0.49 280 <50 19 170

RL.H-135 7.65 <30 100 <5 8.3 <10 250 30 260 7.08 0.9 <10 40 4.48 1710 10 90 0.02 <20 <50 48 <50 80 0.42 240 <50 20 170

RL.H-136 8.48 <30 70 <5 7.8 <10 310 40 60 5.89 0.6 <10 20 4.37 1340 30 100 0.03 <20 <50 46 <50 100 0.52 270 <50 21 120

RL.H-137 7.31 <30 80 <5 6.9 <10 260 30 350 7.47 0.6 <10 20 3.85 1300 <10 100 0.02 <20 <50 35 <50 80 0.41 230 <50 18 130

RL.H-138 7.75 <30 40 <5 8.8 <10 290 40 120 7.27 0.4 <10 20 3.95 1580 <10 90 0.03 <20 <50 42 <50 90 0.49 270 <50 20 130

RL.H-139 0.44 120 <10 <5 2 <10 10 230 1860 >30 <0.1 <10 <10 0.35 330 20 140 <0.01 20 <50 <5 <50 <10 0.03 40 <50 <5 80 22 1.6

RL.H-140 1.38 <30 30 <5 4 <10 30 80 7560 >30 0.3 <10 10 2.03 910 60 430 0.01 40 <50 <5 <50 30 0.07 60 <50 6 260

RL.H-141 7.24 <30 30 <5 1 <10 <10 <10 180 1.05 1.5 <10 <10 0.04 190 <10 <10 <0.01 20 <50 7 <50 30 <0.01 <10 <50 39 <10

RL.H-142 6.66 <30 30 <5 1.3 <10 30 <10 180 0.92 2.1 <10 <10 0.04 330 <10 <10 <0.01 30 <50 6 <50 40 0.01 <10 <50 29 50

RL.H-143 6.87 <30 420 <5 1.3 <10 30 <10 20 1.16 4.1 70 40 0.14 280 <10 <10 0.02 20 <50 <5 <50 100 0.11 10 <50 74 50 <0.5 <0.3

RL.H-144 0.74 90 10 <5 3.9 <10 10 140 1930 >30 0.4 <10 <10 2.11 860 30 190 <0.01 30 <50 6 <50 20 0.02 40 <50 6 470 14 1.6

RL H 145 0 92 80 <10 <5 2 6 <10 30 150 3410 >30 0 1 <10 <10 1 15 580 180 240 <0 01 50 <50 <5 <50 10 0 01 40 <50 <5 280RL.H-145 0.92 80 <10 <5 2.6 <10 30 150 3410 >30 0.1 <10 <10 1.15 580 180 240 <0.01 50 <50 <5 <50 10 0.01 40 <50 <5 280

RL.H-146 0.95 <30 <10 <5 2 <10 10 80 4470 >30 0.5 <10 20 1.5 900 50 500 <0.01 40 <50 8 <50 <10 0.02 50 <50 <5 220 14 3.4

RL.H-147 5.69 <30 10 8 7.8 <10 110 20 640 9.51 0.8 <10 40 5.52 3140 <10 60 0.03 <20 <50 52 <50 40 0.33 220 <50 26 260

RL.H-148 5.19 <30 40 15 11.4 <10 80 20 360 5.91 0.9 <10 30 5.37 2870 <10 30 0.04 <20 <50 16 <50 40 0.19 120 <50 15 170

RL.H-149 6.76 <30 560 5 5.7 <10 480 40 40 6.53 1.5 20 70 6.1 1170 <10 290 0.15 <20 <50 19 <50 940 0.54 160 <50 13 100

RL.H-150 8.56 <30 140 7 6 <10 320 100 200 7.64 0.9 <10 30 3.24 1080 <10 380 0.03 <20 <50 39 <50 120 0.56 300 <50 18 80

RL.H-151 8.99 <30 80 8 7.9 <10 320 80 200 6.43 0.6 <10 20 2.65 1070 <10 280 0.03 <20 <50 41 <50 120 0.58 300 <50 19 120

RL.H-152 8.9 <30 130 6 7.5 <10 340 80 290 6.59 1.1 <10 40 2.99 1150 20 330 0.03 70 <50 40 <50 120 0.57 310 <50 17 220

RL.H-153 6.69 <30 40 9 11.6 <10 230 50 250 8.65 0.3 <10 20 4.05 1890 30 290 0.03 20 <50 30 <50 100 0.4 210 <50 14 310

RL.H-154 7.48 100 590 <5 0.7 20 40 20 4440 4.89 4.7 10 10 0.9 540 200 30 0.09 2070 60 12 260 280 0.36 170 <50 18 2560

RL.H-155 7.68 <30 80 6 4.5 <10 220 50 570 8.03 0.7 <10 40 1.76 650 40 230 0.02 30 <50 33 <50 90 0.34 170 <50 21 160 6 0.6

RL.H-156 8.06 <30 70 8 5 <10 240 80 370 6.95 0.8 <10 40 1.85 810 10 210 0.03 <20 <50 32 <50 110 0.38 210 <50 19 160

RL.H-157 8.07 <30 60 8 3.8 <10 260 70 410 6.59 0.7 <10 50 1.8 710 <10 270 0.03 <20 <50 33 <50 110 0.4 200 <50 17 150

RL.H-158 8.35 <30 30 7 5.6 <10 300 90 220 8.59 0.3 <10 30 2.43 1000 <10 370 0.02 <20 <50 38 <50 140 0.47 270 <50 15 160

RL.H-159 8.15 <30 40 6 4.4 <10 290 80 290 8.85 0.3 <10 30 2.78 930 <10 420 0.03 <20 <50 38 <50 110 0.47 260 <50 13 180

RL.H-160 7.2 <30 60 <5 5.6 <10 270 120 250 13.7 0.4 <10 30 2.04 810 <10 420 0.03 <20 <50 33 <50 100 0.42 250 <50 13 140 <5 0.3

RL.H-161 7.78 <30 70 5 7.6 <10 310 70 240 9.21 0.4 <10 30 1.8 940 40 320 0.03 <20 <50 37 <50 120 0.48 260 <50 13 130

RL.H-162 7.47 <30 100 5 6.5 <10 190 40 260 8.19 0.3 <10 20 0.87 760 20 300 0.03 <20 <50 22 <50 120 0.33 160 <50 9 70

RL.H-163 7.97 <30 130 7 4.7 <10 90 10 130 3.7 0.6 <10 30 1.03 520 <10 100 0.05 <20 <50 11 <50 130 0.23 80 <50 7 60

RL.H-164 7.34 <30 120 7 6 <10 210 130 710 11.8 0.6 <10 40 2.22 890 <10 440 0.05 <20 <50 28 <50 110 0.37 220 <50 13 160

RL.H-165 7.04 <30 370 8 0.9 <10 10 <10 10 1.74 4.3 80 40 0.16 340 <10 <10 0.01 <20 <50 <5 <50 90 0.12 10 <50 79 40

RL.H-166 7.41 <30 80 5 8.6 <10 280 100 320 12.5 0.3 <10 20 2.11 1200 30 390 0.03 <20 <50 36 <50 100 0.44 260 <50 17 170 6 0.5

RL.H-167 8.25 <30 50 <5 8.3 <10 290 80 240 9.35 0.4 <10 30 2.64 1260 <10 270 0.04 <20 <50 38 <50 120 0.47 270 <50 16 260

RL.H-168 7.2 <30 30 <5 6.8 <10 270 150 330 13.8 0.3 <10 30 2.22 980 20 420 0.02 <20 <50 35 <50 120 0.43 250 <50 14 190

第 3 页，共 9 页

Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd

Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323

Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5

Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb

Richardson Lake 2011 Assay Results

RL.H-169 8.13 <30 30 5 7.7 <10 310 70 210 8.92 0.3 <10 20 2.71 1140 <10 300 0.02 <20 <50 40 <50 120 0.49 280 <50 15 160

RL.H-170 8.25 <30 60 <5 7 <10 300 70 270 8.96 0.6 <10 40 2.29 1090 20 260 0.02 <20 <50 39 <50 110 0.47 270 <50 16 160

RL.H-171 7.46 <30 40 7 9 <10 280 90 240 10.7 0.2 <10 20 1.66 1250 <10 270 0.02 <20 <50 36 <50 90 0.44 260 <50 15 140

RL.H-172 8.73 <30 80 6 6.4 <10 320 50 220 7.2 0.6 <10 50 2.34 1010 <10 260 0.03 <20 <50 42 <50 90 0.51 290 <50 17 180

RL.H-173 8.23 <30 80 <5 6.6 <10 310 90 280 9.95 0.5 <10 50 2.61 1170 <10 270 0.02 <20 <50 40 <50 90 0.49 290 <50 17 140 6 <0.3

RL.H-174 8.24 <30 80 6 6.7 <10 310 60 280 8.05 0.4 <10 40 2.16 950 <10 260 0.03 <20 <50 39 <50 120 0.48 270 <50 16 120

RL.H-175 8.28 <30 60 9 7.5 <10 270 60 260 7.28 0.4 <10 40 2.05 940 10 220 0.02 <20 <50 38 <50 130 0.47 270 <50 15 120

RL.H-176 6.05 480 1510 6 2.6 60 370 30 25300 6.83 2.4 20 20 1.91 920 1280 260 0.13 7870 90 12 120 380 0.32 150 <50 18 8860

RL.H-177 7.95 <30 20 7 8.9 <10 200 50 150 9.7 0.4 <10 40 4.44 1810 <10 70 0.03 <20 <50 43 <50 130 0.55 310 <50 19 110

RL.H-178 7.47 <30 50 <5 8.1 <10 200 40 130 9.35 0.4 <10 30 4.25 1700 <10 70 0.03 <20 <50 42 <50 120 0.53 300 <50 17 100

RL.H-179 7.16 <30 160 <5 7.3 <10 200 50 160 7.99 0.9 <10 40 3.79 1430 <10 80 0.02 <20 <50 38 <50 80 0.44 270 <50 14 120

RL.H-180 6.43 <30 130 7 9.5 <10 240 80 730 10.5 0.8 <10 30 1.83 2290 10 180 0.03 <20 <50 37 <50 60 0.41 250 <50 20 130 12 0.5

RL.H-181 7.22 <30 40 6 7.9 <10 190 40 160 8.9 0.5 <10 20 3.99 1710 <10 70 0.03 <20 <50 40 <50 70 0.5 280 <50 17 120

RL.H-182 7.06 <30 20 5 8.4 <10 180 30 100 8.25 0.3 <10 20 3.74 1550 <10 60 0.03 <20 <50 39 <50 120 0.46 270 <50 17 100

RL.H-183 7.41 <30 10 <5 7.9 <10 180 40 90 9.37 0.3 <10 20 4.17 1720 <10 60 0.03 <20 <50 42 <50 130 0.52 300 <50 17 110

RL.H-184 7.44 <30 30 8 6.6 <10 170 40 140 7.74 0.4 <10 20 3.5 1460 <10 80 0.03 <20 <50 37 <50 80 0.44 250 <50 16 140

RL.H-185 7.7 <30 40 8 8.6 <10 280 80 500 9.8 0.3 <10 <10 1.63 1150 20 340 0.03 <20 <50 36 <50 110 0.46 240 <50 16 160 <5 0.6

RL.H-186 2.67 <30 <10 7 5.7 <10 90 190 1100 24.7 0.1 <10 <10 0.61 1040 60 540 0.01 <20 <50 10 <50 40 0.14 100 <50 9 320 19 1.7

RL.H-187 7.06 <30 380 14 0.8 <10 20 <10 20 1.56 4.3 80 40 0.16 340 <10 <10 0.03 <20 <50 <5 <50 100 0.12 10 <50 78 50

RL.H-188 6.72 <30 40 9 6.2 <10 150 50 280 10.9 0.4 <10 10 0.7 950 160 250 0.03 <20 <50 23 <50 90 0.33 190 <50 17 120

RL.H-189 5.01 <30 70 7 5.1 <10 150 60 520 13.8 0.5 <10 30 0.68 850 40 340 0.02 <20 <50 22 <50 60 0.3 180 <50 12 470

RL.H-190 1.26 <30 <10 <5 2.2 <10 90 50 280 9.1 0.2 <10 <10 0.28 390 10 180 0.02 <20 <50 5 <50 10 0.08 40 <50 6 300

RL.H-191 1.06 <30 <10 <5 4.8 <10 50 130 970 26.3 <0.1 <10 <10 0.25 800 120 510 <0.01 <20 <50 <5 <50 20 0.05 50 <50 9 160 7 1.7

RL.H-192 8.09 <30 100 7 8.3 <10 210 40 170 8.22 0.7 <10 20 2.44 1400 <10 110 0.04 <20 <50 34 <50 100 0.55 290 <50 16 140

RL.H-193 7.63 <30 60 9 10.2 <10 270 60 280 8.17 0.4 <10 20 1.5 1730 70 190 0.04 <20 <50 32 <50 110 0.53 270 <50 11 270

RL.H-194 7.65 <30 70 7 5.5 <10 250 60 370 5.67 0.5 <10 10 0.93 690 <10 180 0.02 <20 <50 30 <50 110 0.36 210 <50 14 150

RL.H-195 7.98 <30 60 7 7.4 <10 280 70 360 7.45 0.3 <10 10 1.16 880 <10 240 0.03 <20 <50 34 <50 130 0.41 230 <50 17 200

RL.H-196 7.16 <30 60 <5 3.8 <10 260 90 920 10.1 0.5 <10 50 2.41 770 <10 370 0.02 <20 <50 33 <50 100 0.4 240 <50 13 210

RL.H-197 7.35 <30 80 7 3.9 <10 260 140 1210 11.3 1 <10 30 2.96 910 <10 390 0.03 <20 <50 34 <50 100 0.42 250 <50 13 320 8 0.9

RL.H-198 7.39 110 580 <5 0.7 20 40 20 4380 4.91 4.8 10 10 0.87 530 180 30 0.1 2060 70 12 280 280 0.35 160 <50 18 2590

RL.H-199 7.85 <30 100 7 2.9 <10 290 90 1310 8.78 1.3 <10 50 2.87 560 <10 380 0.03 <20 <50 36 <50 90 0.43 250 <50 14 210

RL.H-200 7.59 <30 80 5 6 <10 210 60 390 7.65 0.9 <10 30 2.42 1110 <10 160 0.03 <20 <50 35 <50 90 0.41 220 <50 16 120

RL H 201 7 9 <30 260 <5 1 2 <10 20 <10 20 0 8 2 8 <10 10 0 11 130 <10 <10 <0 01 <20 <50 <5 <50 80 0 04 10 <50 7 10RL.H-201 7.9 <30 260 <5 1.2 <10 20 <10 20 0.8 2.8 <10 10 0.11 130 <10 <10 <0.01 <20 <50 <5 <50 80 0.04 10 <50 7 10

RL.H-202 7.78 <30 50 7 8.1 <10 220 40 70 8.85 0.7 <10 20 4.14 1710 <10 120 0.05 <20 <50 42 <50 100 0.56 300 <50 21 130

RL.H-203 5.86 <30 80 <5 4.2 <10 100 110 510 13.7 0.7 <10 10 0.97 680 20 530 0.02 <20 <50 14 <50 100 0.18 100 <50 8 190 10 0.3

RL.H-204 5.39 <30 270 <5 5 <10 670 140 290 13.6 0.9 10 40 4.21 810 <10 420 0.08 <20 <50 25 <50 250 0.31 190 <50 12 530

RL.H-205 7.95 <30 90 <5 3 <10 210 60 1420 10.6 0.7 <10 30 2.43 700 <10 340 0.02 <20 <50 41 <50 100 0.54 270 <50 19 290 9 0.7

RL.H-206 7.89 <30 80 6 3.2 <10 240 100 280 9.8 0.7 <10 30 2.38 1100 <10 190 0.04 <20 <50 41 <50 80 0.56 310 <50 18 210

RL.H-207 6.24 <30 130 <5 4 <10 240 100 180 10.9 0.6 <10 20 1.72 690 <10 260 0.02 <20 <50 31 <50 130 0.4 240 <50 12 460

RL.H-208 4.85 <30 360 <5 2.6 <10 200 30 60 5.68 1.4 20 30 2.44 590 <10 180 0.06 <20 <50 16 <50 250 0.26 130 <50 8 170

RL.H-209 7.2 <30 380 11 1.2 <10 30 <10 10 1.77 4.4 80 40 0.19 360 <10 <10 0.02 <20 <50 <5 <50 110 0.13 10 <50 79 50

RL.H-210 6.84 <30 50 <5 8.2 <10 220 40 190 11.3 0.4 <10 <10 1.49 1200 <10 210 0.03 <20 <50 34 <50 90 0.45 260 <50 16 220

RL.H-211 1.76 40 <10 <5 6.9 <10 70 100 180 23.8 <0.1 <10 <10 0.2 1100 10 220 0.01 <20 <50 6 <50 10 0.11 100 <50 <5 1210 15 0.3

RL.H-212 0.31 <30 <10 <5 2.2 <10 40 70 210 14.8 <0.1 <10 <10 0.04 240 10 160 <0.01 <20 <50 <5 <50 10 0.02 20 <50 <5 380

RL.H-213 0.32 <30 <10 <5 1 <10 60 30 150 4.66 <0.1 <10 <10 0.05 260 10 150 <0.01 <20 <50 <5 <50 <10 0.02 20 <50 <5 390

RL.H-214 2.65 <30 60 <5 1.9 <10 60 20 210 4.33 0.5 <10 <10 0.1 450 <10 190 0.01 <20 <50 <5 <50 60 0.06 40 <50 <5 100

RL.H-215 6.67 <30 320 7 1.1 <10 30 <10 30 1.54 1.6 <10 20 0.18 340 <10 10 0.01 <20 <50 <5 <50 120 0.08 20 <50 7 40

RL.H-216 7.09 <30 300 <5 1.2 <10 20 <10 30 1.02 2.1 <10 10 0.12 250 <10 <10 <0.01 <20 <50 <5 <50 250 0.05 10 <50 <5 10

RL.H-217 6.87 <30 70 <5 6.7 <10 40 50 100 12 0.4 <10 40 2.79 1720 <10 40 0.06 <20 <50 42 <50 90 0.94 420 <50 34 110

RL.H-218 7.16 <30 650 <5 8.5 <10 200 40 160 6.79 1.1 70 50 3.66 1330 <10 100 0.14 <20 <50 27 <50 1010 0.4 200 <50 18 110

RL.H-219 7.67 <30 40 <5 8.1 <10 300 50 100 8.68 0.4 <10 40 5.19 1590 <10 140 0.02 <20 <50 39 <50 100 0.43 260 <50 16 100

RL.H-220 6.06 450 1510 <5 2.7 60 380 30 25600 6.92 2.4 20 20 1.89 950 1290 300 0.13 7850 80 12 120 390 0.33 150 <50 17 9020 1230 78.6

RL.H-221 5.33 <30 140 <5 6.6 <10 390 90 630 15.3 0.6 10 20 0.96 940 20 190 0.03 <20 <50 13 <50 60 0.21 100 <50 10 110 7 1.1

RL.H-222 7.81 <30 410 <5 6.6 <10 180 70 130 5.1 1.2 30 50 2.27 960 <10 250 0.08 <20 <50 28 <50 440 0.47 220 <50 16 140

RL.H-223 8.68 <30 120 <5 6.6 <10 310 60 90 5.89 0.5 10 30 2.93 1310 <10 170 0.05 <20 <50 41 <50 280 0.5 280 <50 17 160

RL.H-224 7.74 <30 70 <5 6.6 <10 200 40 140 6.99 0.4 <10 30 2.29 1200 <10 110 0.04 <20 <50 35 <50 190 0.5 270 <50 17 90

第 4 页，共 9 页

Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd

Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323

Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5

Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb

Richardson Lake 2011 Assay Results

RL.H-225 6.11 <30 360 <5 4.9 <10 120 20 40 2.88 1.2 20 10 0.35 570 10 90 0.03 <20 <50 15 <50 80 0.23 120 <50 7 40 <5 <0.3

RL.H-226 5.37 <30 340 <5 3.4 <10 50 30 120 3.44 1.6 20 20 0.89 600 <10 80 0.03 <20 <50 13 <50 50 0.24 110 <50 9 170

RL.H-227 6.67 <30 140 <5 9.2 <10 220 40 90 7.99 1.6 20 40 4.33 3360 <10 100 0.09 130 <50 32 <50 150 0.64 280 <50 25 760 8

RL.H-228 6.09 <30 90 <5 7.3 20 90 20 120 7.87 1.8 10 20 2.5 5150 <10 70 0.03 110 <50 18 <50 80 0.39 150 <50 18 1150 12

RL.H-229 4.6 <30 80 <5 8.2 <10 100 30 190 8.59 1.2 10 30 3.04 4840 <10 80 0.03 <20 <50 14 <50 60 0.29 130 <50 21 550 18 0.6

RL.H-230 4.39 <30 80 <5 10.8 30 130 40 120 13.1 0.9 <10 20 3.99 6040 <10 110 0.03 <20 <50 24 <50 60 0.37 200 <50 37 2640 36

RL.H-231 7.02 <30 390 <5 0.8 <10 30 <10 <10 2.04 4.3 90 40 0.2 420 10 <10 0.01 <20 <50 <5 <50 90 0.12 10 <50 80 60

RL.H-232 2.51 <30 50 <5 6.8 <10 170 40 150 13.2 0.7 <10 10 2.12 2630 <10 120 0.03 <20 <50 11 <50 40 0.17 90 <50 14 600 11 1.4

RL.H-233 2.72 <30 60 <5 1.6 <10 110 60 210 16.8 1 <10 20 0.79 970 <10 150 0.03 20 <50 7 <50 30 0.17 80 <50 8 70 16 2.1

RL.H-234 0.35 <30 10 <5 2.1 <10 50 10 60 6.35 0.1 <10 <10 0.81 1770 <10 50 <0.01 <20 <50 <5 <50 <10 0.05 20 <50 <5 100 7

RL.H-235 0.91 <30 20 <5 3 <10 70 10 40 5.39 0.2 <10 <10 1.18 2870 <10 30 0.01 <20 <50 <5 <50 10 0.09 50 <50 8 140 6

RL.H-236 1.21 <30 10 <5 4 <10 60 10 80 6.81 0.2 <10 <10 1.92 3950 <10 40 0.02 <20 <50 7 <50 20 0.13 60 <50 11 390 13

RL.H-237 0.51 <30 <10 <5 4.5 <10 30 30 140 12.4 <0.1 <10 <10 2.01 5070 <10 100 0.03 <20 <50 <5 <50 <10 0.04 30 <50 9 360 15 1.8

RL.H-238 1.52 <30 30 <5 1.9 <10 60 30 110 9.43 0.5 <10 <10 0.88 1260 <10 80 0.01 <20 <50 6 <50 10 0.13 60 <50 <5 110 10

RL.H-239 4.28 <30 60 <5 2.4 <10 70 70 220 18.4 1.4 20 10 0.92 910 <10 170 0.03 20 <50 9 <50 40 0.24 90 <50 16 570 21

RL.H-240 2.67 <30 20 <5 3.1 <10 70 70 260 18.5 0.4 10 20 1.5 1080 <10 170 0.02 <20 <50 6 <50 20 0.13 60 <50 11 1330 26 2.2

RL.H-241 5.2 <30 70 <5 1.8 <10 100 80 360 21.3 1.4 10 30 1.15 1010 <10 200 0.05 40 <50 13 <50 40 0.29 110 <50 15 730 26

RL.H-242 7.4 110 590 <5 0.8 20 40 20 4420 4.9 4.8 20 10 0.88 530 160 30 0.1 2110 70 11 280 280 0.35 170 <50 17 2600 311 53.7

RL.H-243 2.31 <30 20 <5 1.7 <10 60 90 210 23.2 0.4 <10 10 1.07 650 <10 210 0.01 <20 <50 5 <50 20 0.11 70 <50 10 390 27

RL.H-244 2.24 <30 10 <5 1.8 <10 50 100 250 25.3 0.3 <10 <10 0.94 650 <10 220 0.02 <20 <50 5 <50 20 0.11 70 <50 10 750 30 3.3

RL.H-245 4.71 <30 30 <5 2.2 <10 70 40 220 12.1 0.6 20 20 2.31 880 <10 110 0.04 <20 <50 9 <50 40 0.28 90 <50 14 320 18

RL.H-246 5.62 30 50 <5 1.3 <10 80 70 170 18.6 0.6 <10 40 1.95 1130 <10 170 0.03 <20 <50 14 <50 50 0.32 120 <50 14 270 23

RL.H-247 3.96 <30 70 <5 2.9 <10 70 50 180 14.8 0.7 10 10 1.37 740 <10 130 0.03 <20 <50 9 <50 60 0.2 80 <50 13 450 19 1.6

RL.H-248 6.98 <30 60 <5 5.9 <10 250 40 100 10.7 0.5 10 20 3.63 1600 <10 100 0.08 <20 <50 34 <50 210 0.73 290 <50 22 180 <5

RL.H-249 6.75 <30 70 <5 3.9 <10 120 50 120 12.5 1.4 10 30 2.48 1130 <10 100 0.05 <20 <50 28 <50 70 0.58 230 <50 22 310 12

RL.H-250 2.72 <30 60 <5 4.2 <10 70 40 110 11 0.7 <10 10 1.34 1460 <10 80 0.02 <20 <50 11 <50 30 0.21 110 <50 8 260 9 0.8

RL.H-251 7.21 <30 90 <5 7.3 <10 130 40 120 10.3 0.7 <10 20 3.76 1980 <10 50 0.04 <20 <50 44 <50 70 0.72 350 <50 25 140 <5

RL.H-252 7.43 <30 110 <5 8.5 <10 130 50 140 11 1.6 <10 30 3.05 4890 <10 80 0.06 60 <50 38 <50 80 1.03 380 <50 35 500 <5

RL.H-253 7.12 <30 410 <5 0.8 <10 40 <10 <10 1.72 4.4 90 40 0.18 370 <10 <10 0.02 <20 <50 <5 <50 100 0.13 10 <50 80 50 <5

RL.H-254 6.87 <30 40 <5 9.1 <10 130 40 110 10.4 0.5 <10 20 3.25 2280 <10 60 0.06 <20 <50 35 <50 90 0.96 360 <50 35 130 <5

RL.H-255 6.88 <30 50 <5 9.5 <10 110 40 140 10 0.4 <10 20 2.76 2070 <10 70 0.06 <20 <50 34 <50 100 0.92 330 <50 34 100 <5

RL.H-256 7.14 <30 <10 <5 6.7 <10 120 50 140 11 0.1 <10 20 3.61 1720 <10 70 0.06 <20 <50 36 <50 170 0.99 360 <50 34 110 <5

RL H 257 7 4 <30 10 <5 7 6 <10 120 50 110 10 7 0 1 <10 20 3 42 1870 <10 70 0 06 <20 <50 37 <50 110 1 01 360 <50 35 120 <5RL.H-257 7.4 <30 10 <5 7.6 <10 120 50 110 10.7 0.1 <10 20 3.42 1870 <10 70 0.06 <20 <50 37 <50 110 1.01 360 <50 35 120 <5

RL.H-258 7.37 <30 60 <5 8.1 <10 130 40 110 11 0.2 <10 20 3.46 2110 <10 70 0.07 <20 <50 36 <50 90 0.99 360 <50 34 120 <5

RL.H-259 7.49 <30 260 <5 8.3 <10 140 50 120 10.5 0.6 <10 20 2.85 1920 <10 60 0.07 <20 <50 36 <50 110 0.98 360 <50 33 150 <5 <0.3

RL.H-260 7.57 <30 140 <5 7 <10 140 40 120 10.4 0.4 <10 20 3.47 1980 <10 60 0.07 <20 <50 37 <50 100 0.99 380 <50 33 110 <5

RL.H-261 7.58 <30 180 <5 6.7 <10 270 50 90 9.39 0.5 10 20 4.13 1860 <10 130 0.08 <20 <50 34 <50 270 0.92 340 <50 29 120 <5

RL.H-262 7.74 <30 200 <5 7.8 <10 240 40 70 7.93 0.7 10 40 3.54 1760 <10 120 0.07 <20 <50 31 <50 330 0.83 290 <50 28 110 <5

RL.H-263 7.79 <30 80 <5 8.2 <10 130 40 120 10.4 0.7 <10 20 2.97 1840 <10 60 0.07 <20 <50 38 <50 100 1.02 370 <50 34 90 <5

RL.H-264 6.01 460 1510 <5 2.7 60 370 30 25800 6.69 2.4 20 20 1.84 930 1260 250 0.13 7790 80 12 120 390 0.32 150 <50 17 8920 1260

RL.H-265 5.96 <30 100 <5 10.1 <10 100 30 170 7.92 1 <10 20 3.35 2110 <10 50 0.05 20 <50 26 <50 90 0.7 260 <50 27 170 7

RL.H-266 6.72 <30 150 <5 3.9 <10 80 30 140 8.27 2 20 30 1.82 890 <10 70 0.05 <20 <50 20 <50 70 0.56 200 <50 23 250 <5

RL.H-267 4.21 <30 130 <5 2 <10 90 50 200 18.3 1.5 20 30 1.07 850 <10 130 0.04 <20 <50 8 <50 40 0.26 90 <50 14 180 5 0.8

RL.H-268 0.76 <30 20 <5 2.6 <10 30 50 260 17 0.2 <10 <10 1.53 1210 <10 120 0.02 <20 <50 <5 <50 20 0.04 30 <50 6 180 5 1

RL.H-269 4.53 <30 90 <5 4.9 <10 120 40 270 15 0.6 10 30 2.18 3600 <10 110 0.03 <20 <50 18 <50 70 0.31 140 <50 17 300 8

RL.H-270 7.75 <30 150 <5 8.2 <10 320 40 80 9.03 0.5 10 30 4.93 1640 <10 140 0.04 <20 <50 36 <50 170 0.65 300 <50 21 110 <5

RL.H-271 7.68 <30 330 <5 6.3 <10 240 40 210 7.31 2.6 <10 50 1.76 1970 <10 130 0.03 <20 <50 43 <50 110 0.51 290 <50 19 60

RL.H-272 8.69 <30 140 <5 7.4 <10 250 50 290 8.55 2.7 <10 30 2 2200 <10 140 0.03 <20 <50 49 <50 90 0.58 300 <50 22 70

RL.H-273 7.89 <30 160 <5 5.6 <10 260 50 3010 8.83 2.4 <10 40 1.79 1730 <10 130 0.03 <20 <50 42 <50 80 0.55 300 <50 17 70

RL.H-274 7.06 <30 130 <5 4.2 <10 210 180 1330 14.2 2.2 <10 30 1.75 1300 <10 220 0.03 <20 <50 30 <50 50 0.49 260 <50 15 60 95 2.1

RL.H-275 7 <30 530 <5 1.5 <10 20 <10 <10 1.57 4.3 90 40 0.17 320 <10 <10 0.01 <20 <50 <5 <50 100 0.12 10 <50 79 110 <5 <0.3

RL.H-276 8.36 <30 140 <5 9.6 <10 230 50 300 7.23 2.4 <10 40 2.44 2090 <10 140 0.03 <20 <50 35 <50 70 0.56 290 <50 20 50

RL.H-277 9.71 <30 180 <5 5.1 <10 300 70 290 7.89 3.1 <10 50 1.76 1480 <10 190 0.03 <20 <50 47 <50 80 0.65 350 <50 21 60

RL.H-278 7.99 <30 660 <5 6.4 <10 90 40 70 7.46 1.8 30 60 4.68 1070 <10 70 0.29 <20 <50 30 <50 1070 0.86 310 <50 24 80 <10 6

RL.H-279 8.07 <30 640 <5 6.6 <10 100 40 80 7.74 1.7 30 50 4.93 1100 <10 70 0.3 <20 <50 31 <50 1060 0.91 320 <50 25 80 <10 <5

RL.H-280 8.19 <30 70 <5 4.5 <10 310 50 120 9.29 0.3 <10 20 3.42 2780 <10 120 0.04 <20 <50 38 <50 140 0.7 310 <50 22 210

第 5 页，共 9 页

Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd

Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323

Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5

Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb

Richardson Lake 2011 Assay Results

RL.H-281 7.14 <30 280 <5 7.1 <10 420 60 240 8.96 0.5 30 20 4.9 2280 <10 210 0.12 <20 <50 26 <50 470 0.57 220 <50 19 130 5 <0.3

RL.H-282 8.1 <30 300 <5 3.9 <10 360 50 130 8.77 0.6 20 40 3.84 2400 <10 200 0.09 <20 <50 34 <50 270 0.68 280 <50 22 270

RL.H-283 8.73 <30 70 <5 2 <10 320 50 110 9.83 0.2 <10 40 2.43 2890 <10 120 0.04 <20 <50 42 <50 70 0.77 330 <50 24 490

RL.H-284 8.73 <30 240 <5 2.4 <10 330 80 250 10.5 0.3 <10 30 1.75 2750 <10 160 0.04 <20 <50 38 <50 40 0.77 360 <50 23 320 <5 0.3

RL.H-285 8.63 <30 240 <5 2.4 <10 350 80 210 11 0.3 <10 20 1.69 2800 <10 170 0.04 <20 <50 31 <50 30 0.78 370 <50 21 170

RL.H-286 6.94 90 540 <5 0.7 20 30 20 4150 4.49 4.4 20 10 0.84 500 160 30 0.08 1940 60 11 250 250 0.33 150 <50 16 2380

RL.H-287 8.07 <30 80 <5 2.8 <10 280 90 440 12.7 0.2 <10 20 1.9 2810 <10 170 0.04 <20 <50 29 <50 40 0.74 350 <50 23 140

RL.H-288 7.6 <30 70 <5 5.5 <10 210 40 120 7.68 0.1 <10 <10 2.55 3010 <10 80 0.04 <20 <50 45 <50 60 0.77 340 <50 25 90

RL.H-289 7.93 <30 40 <5 3.8 <10 150 50 110 13.8 <0.1 <10 30 2.39 3360 <10 80 0.06 <20 <50 40 <50 90 1.03 400 <50 36 150

RL.H-290 5.38 <30 250 <5 2.5 <10 100 50 160 12.1 1 <10 40 1.79 2170 <10 80 0.05 <20 <50 27 <50 90 0.67 260 <50 24 150 6 <0.3

RL.H-291 8.07 <30 820 <5 2.4 <10 30 <10 <10 1.85 2.1 10 20 0.58 420 <10 <10 0.06 <20 <50 <5 <50 680 0.17 30 <50 <5 40

RL.H-292 6.85 <30 560 <5 1.8 <10 130 30 310 6.06 2.4 20 20 1.21 500 <10 80 0.07 <20 <50 10 <50 340 0.26 80 <50 13 1460

RL.H-293 5.47 <30 180 <5 1.1 <10 60 60 250 12.6 1.4 10 30 1.12 1170 <10 130 0.04 <20 <50 14 <50 60 0.43 140 <50 19 370 10 0.5

RL.H-294 8.04 <30 40 <5 5.7 <10 130 40 70 11.4 0.2 <10 20 3.43 2570 <10 70 0.06 <20 <50 36 <50 120 0.97 360 <50 34 130

RL.H-295 7.64 <30 50 <5 5.3 <10 140 50 110 10.4 0.2 <10 20 3.66 2300 <10 60 0.07 <20 <50 37 <50 110 1.01 380 <50 33 140

RL.H-296 8.37 <30 700 <5 5.4 <10 140 50 130 10.6 1.4 <10 50 2.89 1730 <10 80 0.07 <20 <50 43 <50 100 1.11 410 <50 37 120

RL.H-297 7.14 <30 470 6 0.7 <10 <10 <10 <10 1.61 4.3 90 40 0.18 350 <10 <10 0.02 <20 <50 <5 <50 110 0.12 10 <50 79 50

RL.H-298 8.05 <30 170 <5 3.4 <10 100 40 100 12.2 1.3 10 30 2.46 1420 <10 60 0.11 <20 <50 42 <50 110 1.22 280 <50 42 140

RL.H-299 6.37 <30 130 <5 6.7 <10 40 30 60 10.7 1.2 10 20 2.73 2390 <10 30 0.1 <20 <50 35 <50 100 1.03 170 <50 48 110

RL.H-300 6.48 <30 80 <5 5.7 <10 40 30 50 12.2 0.6 <10 10 2.7 2200 <10 20 0.11 <20 <50 35 <50 100 1.06 160 <50 48 130

RL.H-301 5.8 <30 90 <5 3.9 <10 80 30 110 11.2 0.7 10 60 2.1 1230 <10 60 0.07 <20 <50 19 <50 80 0.55 110 <50 29 220 5 <0.3

RL.H-302 7.03 <30 160 <5 0.7 <10 80 40 110 13.1 1.4 20 50 1.33 610 <10 130 0.04 <20 <50 13 <50 80 0.36 110 <50 21 410 6 <0.3

RL.H-303 3.96 <30 70 <5 3.8 <10 110 30 220 13.1 0.6 <10 10 1.5 1820 <10 100 0.02 <20 <50 13 <50 80 0.33 130 <50 18 320 <5 <0.3

RL.H-304 7.67 <30 100 <5 4.5 <10 240 40 130 11.4 0.9 <10 30 4.66 1710 <10 120 0.03 <20 <50 35 <50 80 0.6 280 <50 22 120

RL.H-305 6.85 <30 90 <5 4.4 <10 50 30 70 10.9 1 10 40 2.88 1570 <10 50 0.11 <20 <50 37 <50 60 1.11 160 <50 49 110

RL.H-306 5.33 <30 120 <5 0.3 <10 110 60 210 13.4 1.6 10 30 0.92 530 <10 120 0.03 <20 <50 16 <50 50 0.33 130 <50 15 1130 6 1.4

RL.H-307 6.38 <30 140 <5 0.4 <10 70 40 130 8.85 1.4 20 60 1.44 430 <10 110 0.03 30 <50 10 <50 50 0.23 90 <50 14 350

RL.H-308 6.14 470 1550 <5 2.6 60 370 30 26200 6.7 2.5 20 20 1.87 900 1260 260 0.12 8060 90 12 120 390 0.32 150 <50 18 9180

RL.H-309 7.09 <30 80 <5 2.4 <10 50 50 250 12.7 0.6 10 70 2.14 1290 <10 60 0.08 20 <50 30 <50 80 0.88 150 <50 40 220

RL.H-310 7.09 <30 90 <5 4.4 <10 40 40 80 12.3 0.6 10 20 2.47 1740 <10 30 0.11 <20 <50 36 <50 70 1.09 160 <50 50 180

RL.H-311 6.93 <30 20 <5 5 <10 40 40 40 12.6 <0.1 10 <10 2.17 1720 <10 20 0.11 <20 <50 36 <50 90 1.11 150 <50 53 150

RL.H-312 9.11 <30 270 <5 1.3 <10 160 30 110 5.23 3.3 20 20 1.6 1030 <10 80 0.03 <20 <50 21 <50 60 0.46 170 <50 15 170

RL H 313 8 47 <30 270 <5 0 5 <10 150 40 160 7 03 3 20 20 1 5 980 <10 100 0 03 <20 <50 22 <50 30 0 44 170 <50 16 250RL.H-313 8.47 <30 270 <5 0.5 <10 150 40 160 7.03 3 20 20 1.5 980 <10 100 0.03 <20 <50 22 <50 30 0.44 170 <50 16 250

RL.H-314 7.74 <30 390 <5 2 <10 200 30 110 6.6 2.4 20 20 2.21 1370 <10 110 0.05 <20 <50 19 <50 240 0.42 150 <50 14 310 5 <0.3

RL.H-315 7.23 <30 420 <5 3.6 <10 310 40 100 8.54 1.3 20 20 3.57 1930 <10 140 0.08 <20 <50 25 <50 380 0.53 220 <50 17 230

RL.H-316 8.85 <30 690 <5 4.1 <10 250 40 700 7.09 2.2 20 30 2.42 930 <10 80 0.07 <20 <50 24 <50 370 0.44 200 <50 20 530 8 <0.3

RL.H-317 7.91 <30 900 <5 4.7 <10 90 40 230 6.36 1.4 20 20 2.46 980 <10 50 0.14 <20 <50 17 <50 840 0.45 180 <50 18 140

RL.H-318 7.92 <30 690 <5 5.9 <10 230 30 190 6.87 0.9 20 20 3.96 1280 <10 70 0.14 <20 <50 24 <50 950 0.5 210 <50 20 110

RL.H-319 6.89 <30 430 6 0.7 <10 20 <10 <10 1.58 4.2 90 40 0.17 340 <10 <10 0.02 <20 <50 <5 <50 110 0.12 10 <50 89 50

RL.H-320 7.44 <30 80 <5 10.2 <10 270 30 130 5.86 1.2 <10 40 4.82 1970 <10 70 0.02 <20 <50 38 <50 80 0.39 250 <50 16 150

RL.H-321 6.96 <30 80 6 10.2 <10 210 30 300 5.97 1.5 <10 50 4.48 2080 <10 60 0.04 <20 <50 34 <50 70 0.54 250 <50 21 160

RL.H-322 7.42 <30 120 <5 4.9 <10 130 40 310 5.84 1.5 <10 30 2.81 1020 <10 60 0.05 <20 <50 34 <50 70 0.94 320 <50 35 70

RL.H-323 8.22 <30 170 6 5.6 <10 170 40 180 9.02 2.7 <10 60 3.96 1250 <10 70 0.09 <20 <50 48 <50 70 1.45 440 <50 38 110

RL.H-324 8.17 <30 720 <5 5.9 <10 110 30 100 7.12 1.8 30 40 4.27 1020 <10 60 0.26 <20 <50 28 <50 1140 0.8 290 <50 24 80 <5 <10 <5

RL.H-325 8.29 <30 760 <5 6 <10 130 30 80 7.01 2 30 30 4.25 1020 <10 70 0.27 <20 <50 27 <50 1150 0.79 290 <50 23 80 <5 <10 <5

RL.H-326 7.61 <30 70 <5 7.8 <10 190 50 110 13.4 0.6 <10 40 2.55 5140 <10 120 0.04 <20 <50 38 <50 50 0.71 330 <50 25 190

RL.H-327 7.96 <30 80 <5 8 <10 200 60 100 11.2 0.6 <10 40 2.43 4470 <10 120 0.04 <20 <50 39 <50 90 0.74 330 <50 24 140

RL.H-328 8.81 <30 170 <5 6.9 <10 230 60 190 8.11 0.3 <10 30 2.13 3300 <10 150 0.04 <20 <50 41 <50 140 0.81 360 <50 25 100

RL.H-329 6.4 <30 100 <5 11.2 <10 160 70 1170 14.2 0.5 <10 50 2 5330 <10 110 0.03 <20 <50 34 <50 100 0.58 300 <50 23 190

RL.H-330 7.35 80 540 <5 0.8 20 40 20 4300 4.74 4.6 20 10 0.89 550 160 30 0.09 2030 70 12 250 260 0.35 160 <50 17 2570

RL.H-331 8.94 <30 190 <5 5.7 <10 220 60 160 6.87 0.4 <10 30 2.06 2670 <10 130 0.06 <20 <50 42 <50 150 0.8 360 <50 23 100

RL.H-332 7 <30 90 <5 7.8 <10 80 50 170 13.4 0.3 <10 40 3.14 5090 <10 60 0.05 400 <50 46 <50 70 0.84 410 <50 36 160

RL.H-333 7.03 <30 100 <5 7 <10 60 50 160 11.2 0.5 <10 40 2.75 4270 <10 60 0.05 <20 <50 45 <50 80 0.86 400 <50 33 150

RL.H-334 7 <30 20 <5 8.3 <10 70 50 240 12.2 0.2 <10 30 2.42 4360 <10 60 0.05 <20 <50 45 <50 70 0.81 390 <50 34 180

RL.H-335 7.78 <30 320 <5 8.5 <10 280 60 300 9.06 1.5 <10 40 3.86 1720 <10 140 0.03 <20 <50 39 <50 100 0.43 260 <50 18 160

RL.H-336 7.64 <30 140 <5 9 <10 300 40 130 7.57 1 <10 30 3.87 1470 <10 130 0.02 <20 <50 37 <50 80 0.45 270 <50 17 100

第 6 页，共 9 页

Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd

Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323

Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5

Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb

Richardson Lake 2011 Assay Results

RL.H-337 7.34 <30 230 <5 7.8 <10 310 90 210 9.92 1.4 <10 50 4.55 1340 <10 140 0.03 <20 <50 34 <50 80 0.45 260 <50 16 210

RL.H-338 6.9 <30 160 <5 0.7 <10 60 <10 60 0.73 3.9 30 10 0.08 200 <10 <10 0.01 30 <50 <5 <50 80 0.06 <10 <50 7 20

RL.H-339 7.17 <30 170 <5 8.6 <10 240 30 210 6.9 1.4 <10 50 3.19 1700 <10 100 0.03 <20 <50 29 <50 110 0.36 210 <50 15 140

RL.H-340 6.92 <30 360 <5 0.6 <10 30 <10 30 1.09 4 20 10 0.08 210 <10 <10 <0.01 30 <50 <5 <50 110 0.05 <10 <50 6 20

RL.H-341 7.12 <30 460 6 0.7 <10 20 <10 40 1.38 4.6 90 40 0.15 330 <10 <10 0.01 <20 <50 <5 <50 90 0.12 10 <50 83 60

RL.H-342 8.28 <30 120 <5 12.7 <10 360 40 100 8.23 1.3 <10 40 2.82 2470 20 110 0.03 <20 <50 40 <50 110 0.48 290 <50 17 130

RL.H-343 8.55 <30 230 <5 9 <10 340 50 140 7.67 2.4 <10 50 2.48 1500 <10 150 0.03 <20 <50 43 <50 110 0.53 300 <50 16 120

RL.H-344 6 <30 120 <5 9.8 <10 1060 20 280 8.1 1.3 <10 40 3.85 1760 <10 160 0.03 720 <50 33 <50 130 0.3 210 <50 13 200

RL.H-345 0.74 <30 <10 <5 3.3 <10 30 <10 1100 >30 0.2 <10 <10 0.57 540 20 220 <0.01 <20 <50 <5 <50 <10 0.03 50 <50 <5 60

RL.H-346 6.97 <30 620 <5 3.5 <10 440 20 110 6.16 1.7 20 30 2.56 1040 <10 70 0.07 <20 <50 17 <50 600 0.25 110 <50 11 140

RL.H-347 4.62 <30 700 <5 1.4 <10 80 70 730 23.7 1.7 30 20 0.92 710 <10 140 0.06 <20 <50 <5 <50 530 0.15 60 <50 6 90

RL.H-348 0.93 <30 80 <5 1.4 <10 70 40 870 >30 0.3 <10 <10 0.59 430 <10 270 0.02 <20 <50 <5 <50 60 0.05 50 <50 <5 50

RL.H-349 4.1 <30 150 <5 4.5 <10 720 20 790 20.3 0.7 <10 20 2.96 1300 <10 170 0.01 <20 <50 17 <50 180 0.17 130 <50 9 160

RL.H-350 7.69 <30 1220 <5 1.9 <10 90 <10 60 2.98 3 40 60 1.04 490 <10 50 0.07 <20 <50 <5 <50 810 0.19 50 <50 7 50

RL.H-351 0.46 <30 <10 <5 1.3 <10 40 50 1160 >30 <0.1 <10 <10 0.55 580 <10 250 <0.01 <20 <50 <5 <50 10 0.02 50 <50 <5 110 25 2.8

RL.H-352 5.89 410 1510 <5 2.6 60 370 30 24700 6.74 2.4 20 20 1.85 950 1240 250 0.11 7750 90 12 110 350 0.32 140 <50 17 9120 1240 76.5

RL.H-353 3.61 <30 10 <5 0.8 <10 50 <10 300 7.16 1.7 <10 <10 0.38 500 30 30 <0.01 20 <50 <5 <50 20 0.04 20 <50 7 70

RL.H-354 0.78 <30 10 <5 1.6 <10 40 10 210 9.13 0.1 <10 <10 0.72 830 20 40 0.02 <20 <50 <5 <50 20 0.04 30 <50 6 90

RL.H-355 1.4 <30 20 <5 2.6 <10 40 30 390 15.2 0.1 <10 <10 1.21 1250 <10 50 0.02 <20 <50 <5 <50 50 0.08 40 <50 6 190 12 0.9

RL.H-356 2.2 <30 20 <5 1.8 <10 60 10 460 18.9 0.3 <10 10 1.39 2130 <10 80 0.02 <20 <50 5 <50 50 0.13 50 <50 8 260 23 0.9

RL.H-357 3.7 <30 70 <5 5.8 <10 720 50 160 9.29 0.4 <10 20 3.7 1190 <10 120 0.03 <20 <50 22 <50 130 0.17 140 <50 10 150

RL.H-358 5.41 <30 40 <5 3.6 <10 1120 40 270 14.9 0.7 <10 50 6.01 1740 <10 260 0.03 <20 <50 30 <50 80 0.24 190 <50 13 290

RL.H-359 2.77 <30 <10 <5 1.9 <10 80 80 410 24.1 0.2 <10 90 1.9 1830 <10 80 0.03 <20 <50 6 <50 60 0.18 80 <50 13 480 10 0.5

RL.H-360 7.28 <30 80 <5 6.1 <10 860 40 140 7.78 0.6 <10 50 6.41 1980 <10 120 0.02 <20 <50 45 <50 90 0.29 250 <50 16 170

RL.H-361 7.78 <30 100 <5 5.7 <10 790 40 150 7.02 0.9 <10 60 5.83 2110 <10 130 0.02 <20 <50 47 <50 110 0.3 250 <50 17 180

RL.H-362 1.6 <30 <10 <5 1.5 <10 90 110 260 26.1 0.2 <10 10 1.23 1060 <10 170 <0.01 <20 <50 <5 <50 10 0.1 60 <50 6 210

RL.H-363 7.02 <30 380 8 0.7 <10 30 <10 30 1.96 4.5 80 40 0.17 400 <10 <10 0.01 <20 <50 <5 <50 80 0.12 10 <50 75 50

RL.H-364 1.98 <30 50 <5 2.4 <10 30 60 350 >30 0.4 <10 10 1.02 1330 <10 170 0.02 <20 <50 <5 <50 40 0.12 70 <50 9 260

RL.H-365 2.66 <30 40 <5 2.1 <10 60 20 390 19.8 0.5 <10 30 1.43 1080 <10 110 <0.01 <20 <50 6 <50 40 0.17 80 <50 9 320 7 0.6

RL.H-366 1.05 <30 10 <5 1.9 <10 60 <10 100 8.49 0.3 <10 10 0.73 1140 20 40 <0.01 <20 <50 <5 <50 10 0.05 30 <50 <5 150

RL.H-367 6.63 <30 200 <5 0.7 <10 40 <10 50 1.5 3.9 20 <10 0.16 360 <10 <10 0.01 20 <50 <5 <50 80 0.06 <10 <50 5 30

RL.H-368 6.72 <30 320 <5 0.7 <10 30 <10 60 1.18 4 30 <10 0.06 300 <10 <10 0.01 30 <50 <5 <50 110 0.05 <10 <50 5 20

RL H 369 1 74 <30 30 <5 3 3 <10 60 <10 170 15 1 0 6 <10 <10 1 31 1880 <10 70 0 02 <20 <50 <5 <50 30 0 07 40 <50 9 110RL.H-369 1.74 <30 30 <5 3.3 <10 60 <10 170 15.1 0.6 <10 <10 1.31 1880 <10 70 0.02 <20 <50 <5 <50 30 0.07 40 <50 9 110

RL.H-370 0.7 <30 <10 <5 2.2 <10 30 360 320 >30 0.1 <10 <10 0.6 2060 <10 110 0.02 <20 <50 <5 <50 10 0.04 60 <50 9 210

RL.H-371 0.42 <30 <10 <5 2.3 <10 40 40 290 >30 0.1 <10 <10 0.51 1840 <10 120 <0.01 <20 <50 <5 <50 10 0.02 40 <50 7 90

RL.H-372 0.25 <30 <10 5 4.4 <10 20 40 390 >30 <0.1 <10 <10 0.36 1770 <10 220 0.02 <20 <50 <5 <50 20 0.02 50 <50 8 230 9 0.8

RL.H-373 0.49 <30 <10 <5 2.1 <10 140 70 310 >30 0.2 <10 <10 0.42 2450 <10 200 0.01 <20 <50 <5 <50 10 0.03 60 <50 7 100 11 0.8

RL.H-374 7.24 100 600 <5 0.8 20 50 20 4330 4.85 4.9 20 10 0.86 550 170 30 0.09 2130 80 12 270 260 0.35 170 <50 17 2690

RL.H-375 0.21 <30 <10 <5 3 <10 90 <10 150 27 <0.1 <10 <10 0.98 2340 <10 140 <0.01 <20 <50 <5 <50 10 0.01 40 <50 6 180

RL.H-376 0.37 <30 <10 <5 4.7 <10 50 20 330 >30 <0.1 <10 <10 1.4 1390 <10 140 <0.01 20 <50 <5 <50 <10 0.03 60 <50 15 60

RL.H-377 0.42 <30 <10 <5 3.1 <10 30 10 370 >30 <0.1 <10 <10 0.76 1000 <10 210 <0.01 <20 <50 <5 <50 <10 0.03 60 <50 9 150

RL.H-378 0.75 <30 30 <5 2.9 <10 30 30 350 >30 0.1 <10 <10 0.94 5450 <10 180 <0.01 <20 <50 <5 <50 <10 0.04 60 <50 11 590 26 1.2

RL.H-379 1.01 <30 50 <5 1.9 <10 20 60 320 >30 0.3 <10 <10 0.63 5210 <10 140 0.01 <20 <50 <5 <50 20 0.06 50 <50 7 160

RL.H-380 0.86 <30 40 <5 2.2 <10 20 40 470 >30 0.3 <10 <10 0.91 3670 <10 170 <0.01 <20 <50 <5 <50 20 0.03 50 <50 6 200

RL.H-381 0.56 <30 <10 <5 2.1 <10 20 110 480 >30 0.1 <10 <10 0.89 2180 <10 130 0.01 <20 <50 <5 <50 <10 0.03 50 <50 6 110

RL.H-382 0.4 <30 <10 <5 2.2 <10 20 160 640 >30 <0.1 <10 <10 0.97 2780 <10 110 0.02 30 <50 <5 <50 <10 0.02 50 <50 8 130 14 1

RL.H-383 0.75 <30 <10 <5 3.2 <10 10 110 260 >30 <0.1 <10 <10 1.4 3120 <10 100 <0.01 <20 <50 <5 <50 <10 0.04 50 <50 11 250

RL.H-384 0.58 <30 20 <5 1.9 <10 20 160 250 >30 0.2 <10 <10 0.28 3340 <10 120 0.01 <20 <50 <5 <50 20 0.03 50 <50 <5 130 15 0.6

RL.H-385 6.9 <30 510 8 0.9 <10 20 <10 40 2.63 4.5 80 40 0.17 450 <10 10 0.02 <20 <50 <5 <50 90 0.12 10 <50 78 50 <5 <0.3

RL.H-386 0.94 <30 50 <5 2 <10 20 110 220 >30 0.4 <10 <10 0.33 4610 <10 140 0.01 <20 <50 <5 <50 20 0.05 50 <50 <5 250

RL.H-387 1.38 <30 50 <5 3.2 <10 20 80 260 >30 0.4 <10 <10 0.6 4810 <10 140 <0.01 <20 <50 <5 <50 20 0.07 60 <50 7 1060

RL.H-388 1.11 <30 30 <5 2.2 <10 20 120 270 >30 0.3 <10 <10 0.33 6540 <10 150 0.01 <20 <50 <5 <50 20 0.05 50 <50 5 240 21 0.8

RL.H-389 1.42 <30 50 <5 2.5 <10 20 90 270 >30 0.5 <10 <10 0.47 6560 <10 130 <0.01 <20 <50 <5 <50 20 0.07 50 <50 5 170

RL.H-390 4.55 <30 130 <5 4.2 <10 50 10 170 16.9 1.3 10 10 1.45 1410 <10 80 0.03 <20 <50 8 <50 60 0.22 80 <50 16 220

RL.H-391 6.26 <30 230 7 4.2 <10 60 <10 130 12.2 2 20 20 1.13 1290 <10 60 0.05 <20 <50 14 <50 70 0.31 100 <50 16 110 8 <0.3

RL.H-392 4.98 <30 150 7 2.9 <10 50 30 180 18 1.7 <10 10 0.9 1840 <10 100 0.03 <20 <50 13 <50 70 0.23 90 <50 16 110 11 0.4

第 7 页，共 9 页

Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd

Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323

Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5

Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb

Richardson Lake 2011 Assay Results

RL.H-393 2.28 <30 30 5 2.3 <10 30 160 160 >30 0.3 <10 <10 0.77 1870 <10 80 0.02 30 <50 5 <50 10 0.17 70 <50 10 70 25 0.5

RL.H-394 2.1 30 10 7 2.5 <10 40 130 340 >30 0.2 <10 <10 0.86 3090 <10 160 0.02 <20 <50 <5 <50 10 0.13 100 <50 10 120

RL.H-395 6.02 <30 130 8 4.9 <10 140 10 130 14.2 1.4 10 <10 1.66 2650 <10 90 0.03 <20 <50 18 <50 40 0.38 140 <50 18 330

RL.H-396 6.13 450 1490 8 2.7 60 380 30 24900 6.94 2.4 20 20 1.88 1030 1250 260 0.14 7770 80 12 120 340 0.34 150 <50 17 9140

RL.H-397 5.91 <30 150 7 4.7 <10 590 10 120 10.5 1.6 10 10 1.63 2810 <10 80 0.03 <20 <50 18 <50 50 0.3 130 <50 19 230

RL.H-398 5.95 <30 170 8 3.7 <10 70 10 110 9.63 1.4 10 10 0.97 1950 <10 60 0.02 <20 <50 17 <50 60 0.33 120 <50 18 380 5 0.3

RL.H-399 7.14 <30 310 7 4.1 <10 80 10 70 7.39 1.9 20 10 1.02 2330 <10 50 0.04 <20 <50 17 <50 80 0.43 140 <50 21 430

RL.H-400 3.78 <30 80 6 3.3 <10 80 <10 150 24.6 0.6 <10 10 1 2530 <10 130 0.02 <20 <50 10 <50 30 0.24 100 <50 12 250

RL.H-401 1.6 <30 <10 <5 2 <10 50 10 210 >30 <0.1 <10 <10 0.67 2030 <10 190 0.02 <20 <50 <5 <50 <10 0.1 80 <50 8 360

RL.H-402 1.34 <30 <10 7 1.3 <10 40 130 150 >30 0.1 <10 <10 0.43 1390 <10 110 0.03 <20 <50 <5 <50 20 0.1 70 <50 6 80 9 0.4

RL.H-403 1.9 <30 40 7 2 <10 30 110 80 >30 0.6 <10 <10 0.56 2330 <10 70 0.02 <20 <50 <5 <50 20 0.09 60 <50 9 140

RL.H-404 6.74 <30 90 8 0.6 <10 30 <10 50 1.83 3.7 20 <10 0.08 280 <10 20 <0.01 <20 <50 <5 <50 60 0.05 10 <50 <5 20

RL.H-405 1.55 <30 30 6 2.8 <10 30 70 120 >30 0.4 <10 <10 0.4 2610 <10 50 0.02 30 <50 <5 <50 20 0.06 50 <50 8 150 12 <0.3

RL.H-406 0.49 30 <10 6 1.8 <10 30 100 80 >30 <0.1 <10 <10 0.56 3870 <10 60 0.01 <20 <50 <5 <50 <10 0.03 60 <50 10 50

RL.H-407 7.25 <30 400 12 0.8 <10 20 <10 30 1.55 4.4 80 40 0.18 390 <10 10 0.04 20 <50 <5 <50 90 0.13 10 <50 86 60

RL.H-408 0.12 <30 <10 <5 0.4 <10 70 <10 40 1.66 <0.1 <10 <10 0.04 410 <10 30 0.02 <20 <50 <5 <50 <10 0.01 <10 <50 <5 40 <5 1.4

RL.H-409 0.09 30 <10 <5 0.3 <10 100 <10 20 0.82 <0.1 <10 <10 0.05 270 <10 40 <0.01 <20 <50 <5 <50 <10 <0.01 <10 <50 <5 20

RL.H-410 0.26 40 <10 <5 1.2 <10 20 120 70 >30 <0.1 <10 <10 0.33 2480 <10 40 <0.01 <20 <50 <5 <50 <10 0.02 50 <50 5 60

RL.H-411 0.43 <30 <10 5 2.1 <10 10 100 160 >30 <0.1 <10 <10 0.63 4770 <10 60 0.02 <20 <50 <5 <50 10 0.02 60 <50 10 60

RL.H-412 0.75 <30 <10 <5 2 <10 40 70 80 27.1 <0.1 <10 <10 0.5 3250 <10 30 <0.01 <20 <50 <5 <50 20 0.04 50 <50 8 60

RL.H-413 0.82 <30 <10 5 3 <10 20 70 160 >30 <0.1 <10 <10 1.45 8530 <10 140 0.01 <20 <50 5 <50 <10 0.04 80 <50 19 100

RL.H-414 0.4 <30 <10 7 3.6 <10 80 <10 140 11.4 <0.1 <10 <10 0.91 6840 <10 40 <0.01 <20 <50 <5 <50 10 0.02 30 <50 10 60

RL.H-415 0.47 40 <10 6 2.3 <10 <10 100 120 >30 <0.1 <10 <10 0.89 7730 <10 70 0.01 <20 <50 <5 <50 10 0.03 60 <50 13 90

RL.H-416 0.5 40 30 6 2 <10 20 100 150 >30 0.1 <10 <10 0.57 4260 <10 60 0.02 <20 <50 <5 <50 10 0.03 60 <50 10 80 <5 0.5

RL.H-417 0.19 <30 <10 <5 2.6 <10 20 70 150 >30 <0.1 <10 <10 0.76 3230 <10 80 <0.01 <20 <50 <5 <50 <10 0.01 60 <50 11 50

RL.H-418 7.45 100 550 7 0.8 20 60 10 4250 4.91 4.6 10 10 0.89 560 170 30 0.11 2100 70 11 260 240 0.36 160 <50 18 2640 332 48.3

RL.H-419 0.24 <30 <10 <5 2.9 <10 50 30 90 21.7 <0.1 <10 <10 0.81 4090 <10 60 <0.01 <20 <50 <5 <50 <10 0.02 50 <50 12 80

RL.H-420 0.11 <30 10 <5 1.1 <10 40 10 140 25.8 <0.1 <10 <10 0.23 1810 <10 90 <0.01 <20 <50 <5 <50 <10 <0.01 40 <50 <5 40

RL.H-421 0.42 30 <10 <5 1.7 <10 30 60 230 >30 <0.1 <10 <10 0.42 5290 <10 90 0.01 <20 <50 <5 <50 10 0.03 60 <50 7 90 12 1

RL.H-422 0.31 <30 <10 <5 2.4 <10 40 10 90 15.4 <0.1 <10 <10 0.73 5500 <10 60 <0.01 <20 <50 6 <50 <10 0.02 40 <50 9 50

RL.H-423 0.67 30 30 <5 5 <10 40 50 590 29.1 0.1 <10 <10 0.62 5470 <10 70 0.01 <20 <50 <5 <50 50 0.03 60 <50 11 50

RL.H-424 1.21 <30 20 5 10.3 <10 20 60 340 >30 <0.1 <10 <10 0.44 4890 <10 80 0.02 <20 <50 <5 <50 90 0.04 50 <50 10 120

RL H 425 0 34 <30 10 <5 0 8 <10 50 20 50 9 49 <0 1 <10 <10 0 25 2880 <10 30 <0 01 <20 <50 <5 <50 <10 0 02 20 <50 <5 50RL.H-425 0.34 <30 10 <5 0.8 <10 50 20 50 9.49 <0.1 <10 <10 0.25 2880 <10 30 <0.01 <20 <50 <5 <50 <10 0.02 20 <50 <5 50

RL.H-426 0.43 50 <10 <5 3.6 <10 10 100 70 >30 <0.1 <10 <10 0.79 3680 <10 50 <0.01 <20 <50 <5 <50 20 0.02 60 <50 10 60

RL.H-427 0.76 <30 10 <5 2.1 <10 20 50 180 >30 0.1 <10 <10 0.56 4760 <10 110 0.02 <20 <50 <5 <50 10 0.05 70 <50 9 90 <5 0.9

RL.H-428 6.51 <30 180 6 0.6 <10 10 <10 50 1.13 3.5 20 <10 0.08 260 20 <10 <0.01 <20 <50 <5 <50 70 0.06 <10 <50 5 20

RL.H-429 7.11 <30 370 10 0.7 <10 20 <10 50 1.66 4.2 70 40 0.16 390 <10 10 0.02 20 <50 <5 <50 80 0.13 10 <50 78 80

RL.H-430 1.14 30 30 <5 1.9 <10 50 80 140 >30 0.2 <10 <10 0.79 11000 <10 60 0.01 <20 <50 <5 <50 20 0.07 60 <50 13 90

RL.H-431 0.59 <30 20 <5 2 <10 40 70 170 >30 <0.1 <10 <10 0.67 4110 <10 40 0.01 <20 <50 <5 <50 20 0.03 50 <50 9 60

RL.H-432 0.43 40 10 <5 1.9 <10 40 70 110 >30 <0.1 <10 <10 0.59 2690 <10 50 0.01 <20 <50 <5 <50 10 0.02 50 <50 7 50

RL.H-433 0.24 <30 <10 <5 1.1 <10 70 20 40 17.9 <0.1 <10 <10 0.25 2310 <10 20 0.02 <20 <50 <5 <50 <10 0.02 30 <50 <5 20

RL.H-434 0.65 40 <10 6 2.4 <10 20 80 90 >30 <0.1 <10 <10 0.82 7100 <10 50 0.02 <20 <50 <5 <50 10 0.03 60 <50 14 70

RL.H-435 0.57 <30 <10 <5 1.7 <10 20 70 120 >30 <0.1 <10 <10 0.67 6490 <10 50 0.01 <20 <50 <5 <50 <10 0.03 50 <50 8 80 9 0.7

RL.H-436 1.05 30 30 <5 1.8 <10 10 80 160 >30 0.2 <10 <10 0.75 6830 <10 70 0.01 <20 <50 <5 <50 10 0.06 60 <50 8 80

RL.H-437 7.08 <30 270 6 1.1 <10 40 <10 30 1.97 3.1 10 30 0.29 680 10 10 0.02 100 <50 <5 <50 130 0.12 30 <50 7 100

RL.H-438 6.89 30 340 7 0.6 <10 20 <10 40 1.16 4 20 10 0.12 450 <10 <10 0.02 40 <50 <5 <50 150 0.06 10 <50 <5 40

RL.H-439 6.59 <30 130 7 7.7 <10 210 50 240 16.1 0.3 <10 30 3.4 4490 <10 120 0.04 <20 <50 30 <50 70 0.57 250 <50 23 330

RL.H-440 6.08 420 1460 7 2.7 60 360 30 24900 6.75 2.3 20 20 1.89 940 1270 270 0.13 7880 80 12 120 340 0.33 150 <50 18 9170

RL.H-441 7.47 <30 130 10 9.1 <10 230 40 290 11.3 0.3 <10 30 3.24 4860 <10 110 0.05 <20 <50 42 <50 80 0.69 320 <50 26 110

RL.H-442 6.5 <30 80 9 7.4 <10 530 60 280 13.4 0.4 <10 30 3.9 4300 <10 180 0.04 <20 <50 39 <50 50 0.57 290 <50 23 160

RL.H-443 7.13 <30 90 8 8.6 <10 120 50 170 15.6 0.2 <10 40 3.73 6280 <10 100 0.04 <20 <50 42 <50 60 0.58 320 <50 25 270

RL.H-444 6.89 <30 20 10 7.2 <10 170 50 370 15.1 0.2 <10 40 3.34 5650 <10 100 0.05 <20 <50 41 <50 70 0.71 350 <50 30 380

RL.H-445 5.89 <30 70 8 6.3 <10 100 40 200 12.6 0.7 <10 50 2.86 4370 <10 60 0.03 <20 <50 35 <50 40 0.69 350 <50 29 110 <5 <0.3

RL.H-446 7.5 <30 130 8 6.3 <10 70 50 250 12.3 1.6 <10 100 2.71 4180 <10 100 0.07 <20 <50 45 <50 40 0.94 420 <50 33 130

RL.H-447 7.68 <30 100 8 8.9 <10 30 40 230 12.4 1.4 <10 30 3.15 5370 <10 60 0.06 <20 <50 47 <50 50 0.95 430 <50 36 150

RL.H-448 4.23 <30 60 7 5.4 <10 60 30 190 7.7 0.6 <10 30 1.93 3160 <10 40 0.07 <20 <50 27 <50 30 0.51 260 <50 22 170

第 8 页，共 9 页

Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd

Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323

Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5

Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb

Richardson Lake 2011 Assay Results

RL.H-449 8.47 <30 130 9 8.4 <10 30 50 240 13.6 1.3 <10 60 3.15 6040 <10 60 0.04 <20 <50 52 <50 60 1.03 460 <50 40 160

RL.H-450 1.06 <30 20 <5 1.5 <10 70 10 140 2.39 0.3 <10 10 0.48 1170 <10 30 0.02 20 <50 5 <50 20 0.11 70 <50 6 30

RL.H-451 7.08 <30 440 12 0.8 <10 20 <10 170 1.47 4.3 70 40 0.18 400 10 10 0.02 30 <50 <5 <50 90 0.13 20 <50 81 90

RL.H-452 2.18 <30 40 11 3.5 <10 70 20 150 5.4 0.2 <10 10 1.23 2320 <10 30 0.03 <20 <50 12 <50 30 0.24 140 <50 12 60

RL.H-453 2.4 <30 70 7 5.8 <10 170 40 210 6.88 0.1 <10 20 2.73 3240 <10 100 0.02 <20 <50 13 <50 100 0.2 130 <50 11 60 <5 <0.3

RL.H-454 1.89 <30 100 6 2 <10 270 30 160 3.15 0.2 <10 20 2.16 930 <10 120 0.04 <20 <50 7 <50 150 0.16 80 <50 7 40 <5 <0.3

RL.H-455 0.12 <30 <10 5 0.4 <10 70 <10 30 0.57 <0.1 <10 <10 0.07 170 <10 10 <0.01 <20 <50 <5 <50 <10 <0.01 10 <50 <5 10

RL.H-456 5.84 <30 170 8 6.6 <10 340 70 710 13.4 0.5 <10 40 5.06 3680 <10 250 0.08 <20 <50 32 <50 240 0.59 280 <50 24 120 <5 <0.3

RL.H-457 5.2 <30 100 6 6.4 <10 860 70 2580 11.8 0.6 10 70 5.74 3290 <10 300 0.07 110 <50 22 <50 50 0.36 170 <50 17 470

RL.H-458 N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. <5 4.8

第 9 页，共 9 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 633682.998 East: Original Units: M North: North: 5438207.218 North: Storage: Markham Elevation: Elevation: 497.124 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

TypeFFFFFF

Page 1 of 12

Control Drilling: Cutting Sampled: YesGeophysics:

Deviation Tests

Target: VETM anomaly supported by Geotech reportComments: ZK1 returned 147 ppb Au over a 6.57 metre core length from 21.35 to 27.92 metres including 236 ppb Au over a 2.62 metre core length from 21.35 to 23.97 metres.This anomalous gold intersection lies within siltstone-magnetite-richargillite metasedimentary unit containing foliation parallel pyrrhotite bands and disseminations.

Contractor: TOPRANKSpotted by: ShawnCoord Type:Surveyed Date: Logged by: ShawnRe-logged by: Water Source: Water Line: Left in hole: Casing + Shoe

CHINA METALLURGICAL EXPLORATION CORP. Diamond Drill Hole Report

Casing

Completed: 13-March-11Logged: 14-March-11Wedged: NoWedged from:

Capped: YesCemented: No

Hole Number: ZK1

Project Number:

Other

Distance(m)

89.488.487.7

133.20154.53

Length: 163.68 metersStarted: 10-March-11

LocationTownship: Richardson Lake AreaClaim No: 4248129NTS:

Length: 9.75 metersPulled: No

DrillingAzimuth: 90Dip: -45

16-Nov-12

Azimuth11.28 79.541.76 93.972.24 93.6

102.72

0B

From To From To

ZK1 01 Overburden 0 9.75 9.75 Overburden\casing. 9.55-9.75m,K-feldspar granite,light flesh red color,medium-coarse grained,not see the contact with the underlying volcanic rocks,probably is float.

ZK1 02Pyrrhotite meta-basalt

9.75 20.05 10.3 9.7 94

Dark,fine-grained,rare porphyritic texture,amygdaloidal structure,diameter of amygdaloid is <1mm,calcspar filling,composed of pyroxene and a small amount of quartz and biotite. The rock development epidotization, pyrrhotite, partial see a small amount of pyrite and chalcopyrite. Pyrrhotite veinlets were banded, some of them were small lumpy, the width of pyrrhotite stringer was about 1-5mm, fine-grained, content was about 5%, partial up to 20%; pyrite, chalcopyrite distributed localy, mainly in rock fracture surface as fine-grained, often coexist with pyrrhotite, content is <1%. 14.15-15.53m, rock crushing. 13.26m ,a little bit chalcopyrite.

RL.H-1 9.75 11.28 1.53 0.93 61 390 70 2100 280 <10 670 100

RL.H-2 12.68 1.40 1.40 100 260 60 1680 260 <10 730 90

RL.H-3 14.08 1.40 1.40 100 370 60 2050 220 <10 700 80

RL.H-4 15.43 1.35 1.35 100 260 60 930 250 <10 690 70

RL.H-5 16.8 1.37 1.37 100 520 80 1460 350 <10 680 120

RL.H-6 18.17 1.37 1.37 100 370 60 1290 270 <10 710 90

RL.H-7 19.05 0.88 0.88 100 380 50 1000 240 <10 700 80

RL.H-8 20.05 1.00 1.00 100 330 40 830 290 <10 760 100

RL.H-9 21.35 1.30 1.30 100 100 <20 150 80 <10 120 30

RL.H-10 22.7 1.35 1.35 100 110 <20 290 80 <10 160 40

RL.H-12 23.97 1.27 1.27 100 170 20 440 150 <10 253 <0.3 300 70

RL.H-13 25.33 1.36 1.30 96 280 <20 510 100 <10 240 50

RL.H-14 26.52 1.19 1.14 96 100 <20 260 60 <10 200 30

RL.H-15 27.92 1.40 1.40 100 310 <20 970 120 <10 63 0.3 140 50

Moppm

Auppb

Agg/t

Assay Results

Cuppm

Pbppm

Znppm

Nippm

Length of

core （m）

Recovery

factor（%）

Thickness

（m）

Length of core （m）

Recovery

factor（%）

DescriptionHole No.

No.Rock/Ore

type Crppm

Location (m)

Gray-dark gray, fine-grained to aphanitic structure, banded structure, composed of pyroxene, hornblende and quartz and biotite. Magnetic to weak magnetic, magnetic minerals are mainly magnetite and pyrrhotite. Generally developed pyrrhotite, magnetite , locally developed pyrite and minor chalcopyrite. Pyrrhotite were mainly distributed as irregular banded veinlets and lumpy shape, content was about 5-50%; magnetite was distributed as black banded vein; partial can see some pyrite and chalcopyrite, and often coexist with pyrrhotite. Development of the chlorite and(or) epidotization. Two group joint,30°and 50°to core axis. 20.05-29.57m，iron formation,pyrrhotite were mainly distributed as irregular banded veinlets,the width of veinlets were about 5-30mm, 60°to core axis，content was >70%，some pyrrhotite were in banded veinlets,contnt was about 5-10%；26.65-26.75m,10cm width massive pyrrhotite。 29.57-32.61m，banded,veined pyrrhotite, about 20%;31.70m,a little bit lumpy chalcopyrite were distributed in pyrrhotite.

32 61-39 76m Intensive distribution of irregular banded veined and lumpy

Coppm

Drill Log of Hole #RLP-11-01

Depth（m）

Sample log

Sample No.

Length（m）

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-16 29.57 1.65 1.65 100 40 <20 80 30 <10 40 <10

RL.H-17 30.86 1.29 1.20 93 200 30 880 160 <10 320 70

RL.H-18 32.26 1.40 1.30 93 330 40 590 100 <10 220 50

RL.H-19 33.66 1.40 1.33 95 550 60 1130 170 <10 43 0.6 230 90

RL.H-20 34.92 1.26 1.20 95 1960 30 870 140 <10 180 80

RL.H-21 36.09 1.17 1.14 97 610 50 1610 200 <10 220 110

RL.H-23 37.41 1.32 1.32 100 370 40 1010 140 <10 300 80

RL.H-24 38.71 1.30 1.30 100 560 50 1580 230 <10 31 1 110 120

RL.H-25 39.76 1.05 1.05 100 690 50 1160 210 <10 110 120

RL.H-26 40.91 1.15 1.15 100 100 <20 90 30 <10 30 20

RL.H-27 42.29 1.38 1.35 98 100 <20 120 40 <10 40 20

RL.H-28 43.51 1.22 1.15 94 150 <20 630 110 <10 290 50

RL.H-29 44.81 1.30 1.23 94 440 30 1100 170 <10 31 <0.3 300 80

RL.H-30 45.91 1.10 1.10 100 240 <20 180 180 <10 130 60

RL.H-31 46.91 1.00 1.00 100 540 <20 530 160 <10 250 50

RL.H-32 47.85 0.94 0.94 100 290 <20 240 130 <10 310 40

RL.H-34 49.07 1.22 1.22 100 130 <20 210 90 <10 140 30

RL.H-35 50.42 1.35 1.35 100 360 <20 950 120 <10 76 <0.3 190 40

RL.H-36 51.87 1.45 1.44 99 370 <20 350 100 <10 240 30

RL.H-37 53.26 1.39 1.38 99 40 <20 80 50 <10 60 10

RL.H-38 54.56 1.30 1.30 100 10 <20 50 70 <10 170 <10

RL.H-39 56.01 1.45 1.45 100 30 <20 80 100 <10 310 10

RL.H-40 57.34 1.33 1.33 100 70 <20 140 50 10 140 10

03ZK1 86.5720.05Iron

Formation

32.61 39.76m，Intensive distribution of irregular banded,veined and lumpy pyrrhotite,about 50-70%；32.86m、34.56m、38.93m see minor chalcopyrit. 39.76-42.29m，sulphide <5%. 42.29-47.85m，banded pyrrhotite,30%；45.80m,a little bit lumpy chalcopyrit. 47.85-57.34m，content of pyrrhotite was about 10%. 57.34-63.95m，content of sulphide was about 40%,mainly pyrrhotite,irregular banded and lumpy；62.23m intensive distribution of irregular banded and veined pyrrhotite. 63.95-66.90m，sulphide <5%. 66.90-74.13m，aphanitic-glassy, black, banded pyrrhotite development,local see lumpy Prr, content was about 20%; 70.00m ,the pyrite and pyrrhotite coexist distribution. 74.13-81.04m，pyrrhotite,minor pyrite,content of sulphide was about 20%；75.70m,Py=1/5 Po. 81.04-86.57m，aphanitic-glassy，pyrrhotite about 10%，minor pyrite,Py=1/10 Po.

9965.6466.52

第 1 页，共 19 页

From To From To

Moppm

Auppb

Agg/t

Assay Results

Cuppm

Pbppm

Znppm

Nippm

Length of

core （m）

Recovery

factor（%）

Thickness

（m）

Length of core （m）

Recovery

factor（%）

DescriptionHole No.

No.Rock/Ore

type Crppm

Location (m)Coppm

Drill Log of Hole #RLP-11-01

Depth（m）

Sample log

Sample No.

Length（m）

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-41 58.74 1.40 1.40 100 230 20 290 170 <10 29 0.3 90 50

RL.H-42 60.05 1.31 1.31 100 680 30 440 260 <10 350 170

RL.H-43 61.25 1.20 1.20 100 430 20 310 190 <10 470 40

RL.H-45 62.55 1.30 1.30 100 480 20 2000 260 <10 61 0.6 460 110

RL.H-46 63.95 1.40 1.40 100 390 <20 1320 160 <10 150 90

RL.H-47 65.5 1.55 1.55 100 180 <20 170 130 <10 380 50

RL.H-48 66.9 1.40 1.40 100 100 <20 250 170 <10 410 50

RL.H-49 68.11 1.21 1.20 98 310 <20 640 140 <10 550 70

RL.H-50 69.19 1.08 1.06 98 140 <20 670 130 <10 680 50

RL.H-51 70.39 1.20 1.15 96 130 <20 240 150 <10 30 <0.3 420 70

RL.H-52 71.58 1.19 1.14 96 130 <20 190 110 <10 210 40

RL.H-53 72.91 1.33 1.30 98 100 20 250 130 <10 41 <0.3 230 40

RL.H-54 74.13 1.22 1.22 100 140 <20 180 170 <10 420 30

RL.H-56 75.29 1.16 1.16 100 190 <20 130 170 <10 140 50

RL.H-57 76.59 1.30 1.30 100 210 <20 260 190 50 19 0.3 130 110

RL.H-58 77.79 1.20 1.20 100 80 <20 140 70 <10 100 20

RL.H-59 78.94 1.15 1.15 100 70 <20 50 70 <10 20 20

RL.H-60 80.04 1.10 1.10 100 120 <20 100 130 <10 100 20

RL.H-61 81.08 1.04 1.04 100 130 <20 130 140 <10 28 <0.3 70 40

RL.H-62 82.28 1.20 1.20 100 110 <20 190 120 <10 90 20

RL.H-63 83.48 1.20 1.20 100 60 <20 160 140 <10 310 40

RL.H-64 84.94 1.46 1.46 100 90 <20 190 140 <10 23 <0.3 190 40

RL.H-65 86.57 1.63 1.60 98 70 <20 140 110 <10 170 30

RL.H-67 87.91 1.34 1.30 98 70 <20 130 70 <10 120 30

RL.H-68 89.03 1.12 1.10 98 110 <20 110 200 <10 190 50

04meta-

andesite86.57 102.72ZK1 16.15 15.91 99

Gray to dark green,medium to fine grained,massive structure,mineral compositionare mainly amphibole, feldspar and a small amount of quartz, biotite,scattereddistribution Prr and Py,general development of the chlorite and epidotization. One group joint,50°to core axis.

86.58-88.28m，lumpy Po, 5%；92.49m,minor Py。

ZK1 05 lamprophyre 102.72 104.02 1.3 1.3 100 Dark gray,porphyritic texture,massive structure,mineral composition are mainly feldspar,hornblende and biotite, phenocrysts were biotite.

ZK1 06meta-

andesite104.02 130.15 26.13 26.13 100

Gray to dark green,medium to fine grained,massive structure,mineral composition are mainly amphibole, feldspar and a small amount of quartz and biotite.

ZK1 07 lamprophyre 130.15 131.93 1.78 1.78 100 Dark gray,porphyritic texture,massive structure,mineral composition are mainly feldspar,hornblende and biotite, phenocrysts were biotite.

ZK1 08meta-

andesite131.93 163.68 31.75 31.6 100

Gray to dark green,medium to fine grained,massive structure,mineral composition are mainly amphibole, feldspar and quartz .Chlorite and epidotization were common.

86.58 88.28m，lumpy Po, 5%；92.49m,minor Py。

第 2 页，共 19 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 633404.587 East: Original Units: M North: North: 5438233.876 North: Storage: Markham Elevation: Elevation: 501.69 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

TypeFFF

Page 2 of 12

68.58 85.1114.30 84.3

Deviation TestsDistance(m)

25.91 86.6Azimuth

Geophysics: Target: VETM anomaly supported by Geotech reportComments: ZK2 intersected 5-10% wispy Po veinlets and minor Cpy from 36.15m to 37.35m that may explain the targeted EM conductor. Limited assays returned no significant gold or base metal content.

Control Drilling: Cutting Sampled: Yes

Wedged from: Water Line: Left in hole: Casing + Shoe

Logged: 17-March-11 Re-logged by: Wedged: No Water Source:

Started: 13-March-11 Cemented: No Surveyed Date: Completed: 16-March-11 Logged by: Shawn

Length: 123.44 meters Capped: Yes NTS: Coord Type: Dip: -45 Pulled: No Claim No: 4248129 Spotted by: Shawn

OtherAzimuth: 70 Length: 1.11 meters Township: Richardson Lake Area Contractor: TOPRANK

Drilling Casing Location

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK2

Diamond Drill Hole Report Project Number:

16-Nov-12

1B

From To From To

ZK2 01 Overburden 0 1.11 1.11 0 0 Overburden\casing.

RL.H-69 13.58 14.74 1.16 1.16 100 120 <20 90 130 <10 280 50

RL.H-70 15.94 1.20 1.20 100 130 <20 90 120 <10 <5 <0.3 270 50

RL.H-71 19.36 20.38 1.02 1.02 100 170 <20 80 140 <10 270 50

RL.H-72 21.48 1.10 1.10 100 360 <20 180 120 <10 100 70

RL.H-316 36.15 37.35 1.20 1.20 100 700 <20 530 80 <10 8 <0.3 250 40

RL.H-317 38.10 0.75 0.75 100 230 <20 140 50 <10 90 40

RL.H-318 39.10 1.00 1.00 100 190 <20 110 70 <10 230 30

ZK2 03 lamprophyre 68.3 71.79 3.49 3.49 100 Dark gray to dark, porphyritic texture and massive structure, mineral composition are plagioclase, hornblende and biotite, phenocrysts were biotite.

RL.H-73 91.08 92.23 1.15 1.15 100 150 <20 80 80 <10 360 50

RL.H-74 121.87 123.44 1.57 1.40 89 120 <20 80 50 <10 <5 <0.3 90 30

Drill Log of Hole #RLP-11-02

Hole No.

No.Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery

factor（%）

Description

Sample log Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Recovery

factor（%）

Cuppm

Pbppm

Znppm

Coppm

67.19 67.19 100

Gray to gray-green, fine-grained texture and massive structure, main mineral composition are amphibole, feldspar, biotite. General development of the chlorite ,epidotization and silification. Calcite veins are common , showed a single vein or stockwork distribution, vein width is about 0.1-4cm. Pyrrhotite is occasionally to find. Two group joint,25°and 40°to core axis. 13.72m，small amounts of pyrite. 19.81m,silicified quartz vein, also see a little bit pyrrhotite,the content is about <1%. 33.90-47.32m, the rock was gray white to gray, the content of light colored and dark colored minerals are almost same; in 34.87m and 40.15m see some pyrrhotite in the rock joint. 47.32-52.00m, gray-green rocks, porphyritic texture, 50.09m see pyrrhotite, the content is about 5%. 57.64m,4cm wide calcite vein

Nippm

Moppm

Auppb

Agg/t

ZK2meta-

andesite1.11 68.302

Crppm

ZK2 123.4471.79meta-

andesite04

Gray to gray-green, fine to medium grained texture and massive structure, main mineral composition are amphibole, feldspar, quartz and biotite. General development of the chlorite ,epidotization and silification. Calcite and quartz veins are common.Pyrrhotite is occasionally to find. 78.08-87.29m，gray white to gray，silification， medium to fine grained,pyrrhotite is occasionally to see. 91.72m,lumpy pyrrhotite. 96.36m,strong epidotization,chlorite and silification 112.78-113.18m，calcite veins filled between volcanic fragments. 111.35-111.45m，111.60-111.75m ,strong silification. 122.42-122.72m，strong silification,also see some calcite veins. 122.99-123.44m，calcite veins filled between volcanic fragments.

9951.0951.65

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

第 3 页，共 19 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 633025.454 East: Original Units: M North: North: 5438170.008 North: Storage: Markham Elevation: Elevation: 510.101 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

TypeFFF

Page 3 of 12

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK3

Diamond Drill Hole Report Project Number:

Drilling Casing Location OtherAzimuth: 60 Length: 7.02 meters Township: Richardson Lake Area Contractor: TOPRANKDip: -55 Pulled: No Claim No: 4248129 Spotted by: ShawnLength: 150.88 meters Capped: Yes NTS: Coord Type: Started: 16-March-11 Cemented: No Surveyed Date: Completed: 19-March-11 Logged by: ShawnLogged: 20-March-11 Re-logged by: Wedged: Water Source: Wedged from: Water Line:

Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:

Target: VETM anomaly supported by Geotech reportComments: ZK3 intersected minor to moderate Po veinlets from 7.02m to 10.67m that might explain the targeted EM conductor. Assays returned no significant gold or base metal content within the iron formation although the zinc content is somewhatanomalous.

Deviation TestsDistance(m)

16-Nov-12

Azimuth36.58 62.386.87 59.4

128.02 61.3

2B

From To From To

ZK3 01 Overburden 0 7.02 7.02 0 0 Overburden\casing.

RL.H-75 7.67 9.17 1.50 1.50 100 1350 <20 80 190 <10 160 130

RL.H-76 10.67 1.50 1.50 100 130 <20 120 160 <10 210 50

ZK3 03meta-

andesite10.67 21.61 10.94 10.94 100

Gray-green to gray-white, fine-grained texture and massive structure, main mineral composition are amphibole, feldspar and a little quartz and biotite. General development of the chlorite ,epidotization. Occasionally to see pyrrhotite,the content is <1%. 10.67-11.87m,gray white to gray, medium-fine grained,the content of light colored and dark colored minerals are almost same;11.25m,al little bit pyrrhotite. 16.96m,17.60m,some pyrrhotite are distributed in calcite veins.

ZK3 04 lamprophyre 21.61 24.95 3.34 3.34 100 Dark gray, porphyritic texture and massive structure, mineral composition are plagioclase, hornblende and biotite, phenocrysts were biotite.

meta-andesite

3.6510.677.02

Crppm

Coppm

Gray to gray-green, fine-grained texture and massive structure, main mineral composition are amphibole, feldspar, quartz and a little biotite. General development of the chlorite ,epidotization. Generally developed pyrrhotite, distributed as irregular veinlets and lumpy shape in rocks cracks,also see some calcite veins. 7.02-7.67m,meta-andesite,occasionally to see pyrrhotite. 8.02-8.42m,see more pyrrhotite, irregular veins,the content is about 20%. 8.42-10.67m,occasionally to see pyrrhotite in rock joints，the content is about 2%.

100

Nippm

Moppm

Auppb

Agg/t

Sample log Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Recovery factor（%）

Cuppm

Pbppm

Znppm

Drill Log of Hole #RLP-11-03

Hole No.

No.Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery

factor（%）

Description

24.95 80.02 55.07 54.65

02ZK3Pyrrhotite

meta-andesite

ZK3 05

3.65

99

Gray to gray-green, medium-fine grained texture and massive structure, main mineral composition are amphibole, feldspar and a little quartz and biotite. General development of the chlorite ,epidotization,rock cracks are filled with calcite as veins,vein width is about 2-6mm,also see some quartz veins. Occasionally to see sulphide as scattered specks,the content is <1%. Two group joints,25°and 40°to core axis. 24.95-32.68m，fine grained,contain a little bit biotite. 32.68-55.89m，medium-fine grained,more biotite;35.45-35.47m and 47.64-47.65m ,white quartz veins. 55.89-80.02m，fine grained,a little bit biotite;66.71-68.18m，calcite veins

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-78 78.72 80.02 1.30 1.30 100 190 <20 100 100 <10 180 40

RL.H-79 81.22 1.20 1.20 100 460 <20 290 90 <10 150 50

RL.H-80 82.52 1.30 1.30 100 630 30 1360 110 <10 29 2.1 80 120

RL.H-81 83.82 1.30 1.30 100 620 30 630 80 <10 22 1.6 210 60

RL.H-82 85.16 1.34 1.33 99 710 40 1380 90 <10 100 70

RL.H-83 86.47 1.31 1.30 99 320 <20 210 90 <10 190 60

RL.H-84 87.68 1.21 1.20 99 170 <20 70 50 <10 60 40

RL.H-85 88.68 1.00 1.00 100 130 <20 110 70 <10 60 30

RL.H-86 89.59 0.91 0.91 100 290 <20 110 100 <10 21 0.8 110 30

RL.H-87 90.52 0.93 0.93 100 70 <20 110 430 <10 800 40

RL.H-89 91.83 1.31 1.30 99 670 30 1230 90 <10 80 90

RL.H-90 92.96 1.13 1.12 99 990 30 1610 120 <10 90 100

RL.H-91 94.01 1.05 1.02 97 560 30 1660 100 <10 64 0.8 70 60

RL.H-92 95.45 1.44 1.40 97 70 <20 170 20 <10 60 <10

RL.H-93 96.61 1.16 1.10 95 160 <20 200 20 <10 20 10

RL.H-94 97.87 1.26 1.20 95 220 <20 680 130 <10 30 30

RL.H-95 99.06 1.19 1.13 95 280 <20 1600 110 <10 60 40

RL.H-96 100.08 1.02 1.00 98 310 30 1550 140 <10 90 40

RL.H-97 101.10 1.02 1.00 98 470 <20 880 140 <10 12 <0.3 120 50

RL.H-98 102.11 1.01 1.00 99 260 <20 190 80 <10 60 30

RL.H-100 103.46 1.35 1.35 100 130 <20 140 90 <10 110 30

RL.H-101 104.86 1.40 1.40 100 620 <20 350 100 <10 100 40

RL.H-102 106.29 1.43 1.40 98 300 <20 770 120 <10 100 60

RL.H-103 107.80 1.51 1.48 98 150 <20 90 130 <10 140 60

RL.H-104 109.10 1.30 1.27 98 260 <20 60 80 <10 70 20

Dark gray to dark, fine-grained to aphanitic texture and banded structure, main mineral composition are amphibole, feldspar, quartz and a little biotite.Magnetic to weak magnetic，magnetic minerals are mainly magnetite and pyrrhotite. Generally developed pyrrhotite, pyrite and minor chalcopyrite. Sulphide are mainly distributed as banded veins and lumpy shape，the content is about 10-40%，the width of veins is about 1-5mm，some is up to 40mm，the bands are 45°to core axis. 81.96m，Po and Py，lumpy,banded vein. 83.71m,30mm Po vein. 88.66-89.42m,wide sulphide banded veins,densely distributed,the content is about 40%. 89.59-90.52m,contain some lamprophyre, occasionally sulfide 90.52-102.11m,Po and minor Clp,the content of sulphide is about 15%，;100.44m Po=10Py. 102.11-106.29m,the content of sulphide is anout 10%. 106.29-107.80m,gray andesite,vesicular and amygdaloidal structure，occasionally to see sulphide. 107.80-113.99m,the content of sulphide is anout 5%，banded veins.

9933.53

filled between volcanic fragments.

06ZK3 33.97113.99Iron

Formation80.02

第 4 页，共 19 页

From To From To

Crppm

Coppm

Nippm

Moppm

Auppb

Agg/t

Sample log Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Recovery factor（%）

Cuppm

Pbppm

Znppm

Drill Log of Hole #RLP-11-03

Hole No.

No.Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery

factor（%）

Description

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-105 110.40 1.30 1.30 100 180 <20 190 70 <10 60 30

RL.H-106 111.65 1.25 1.25 100 390 <20 910 120 <10 36 0.4 80 50

RL.H-107 112.75 1.10 1.10 100 210 <20 140 130 <10 120 60

RL.H-108 113.99 1.24 1.24 100 40 <20 60 90 <10 80 30

RL.H-109 115.19 1.20 1.20 100 40 <20 80 100 <10 120 30

RL.H-111 116.39 1.20 1.20 100 80 <20 100 130 <10 160 50ZK3 07

meta-andesite

113.99 150.88 36.89Gray to gray-green, medium to fine grained texture and massive structure, main mineral composition are amphibole, feldspar and few quartz and biotite. General development of the chlorite ,epidotization,calcite veins are common to see.

36.55 99

第 5 页，共 19 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 635010.358 East: Original Units: M North: North: 5440603.521 North: Storage: Markham Elevation: Elevation: 540.182 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

TypeFFF

Page 4 of 12

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK4

Diamond Drill Hole Report Project Number:

Drilling Casing Location OtherAzimuth: 250 Length: 2.02 meters Township: Richardson Lake Area Contractor: TOPRANKDip: -60 Pulled: No Claim No: 4252244 Spotted by: ShawnLength: 177.39 meters Capped: Yes NTS: Coord Type: Started: 23-May-11 Cemented: No Surveyed Date: Completed: 26-May-11 Logged by: ShawnLogged: 27-May-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:

Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:

Target: VETM anomaly supported by Geotech reportComments: The drill hole intersected approximately 176 metres of mafic metavolcanic rocks at least portions of which are pillowed .

Deviation TestsDistance(m)

16-Nov-12

Azimuth38.10 243.483.82 247.6

129.54 250

3B

From To From To

ZK4 01 Overburden 0.00 2.02 0.00 2.02 0 Overburden\casing.

RL.H-439 54.04 55.41 1.07 1.05 98 240 <20 330 120 <10 210 50

RL.H-441 89.92 90.82 0.90 0.90 100 290 <20 110 110 <10 230 40

RL.H-442 91.66 0.84 0.84 100 280 <20 160 180 <10 530 60

RL.H-443 114.13 115.58 1.45 1.41 97 170 <20 270 100 <10 120 50

RL.H-444 117.00 1.42 1.38 97 370 <20 380 100 <10 170 50

RL.H-445 139.88 141.08 1.20 1.20 100 200 <20 110 60 <10 <5 <0.3 100 40

RL.H-446 142.33 1.05 1.05 100 250 <20 130 100 <10 70 50

RL.H-447 161.54 162.54 1.00 1.00 100 230 <20 150 60 <10 30 40

RL.H-448 163.42 0.88 0.88 100 190 <20 170 40 <10 60 30

RL.H-449 164.47 1.05 1.05 100 240 <20 160 60 <10 30 50

RL.H-450 165.62 1.15 1.15 100 140 20 30 30 <10 70 10

RL.H-452 166.62 1.00 1.00 100 150 <20 60 30 <10 70 20

RL.H-453 167.82 1.20 1.20 100 210 <20 60 100 <10 <5 <0.3 170 40

RL.H-454 168.72 0.90 0.90 100 160 <20 40 120 <10 <5 <0.3 270 30

RL.H-455 169.77 1.05 1.04 99 30 <20 10 10 <10 70 <10

RL.H-456 171.00 1.23 1.23 100 710 <20 120 250 <10 <5 <0 3 340 70

Crppm

Coppm

Nippm

Moppm

Auppb

Agg/t

Sample log Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Recovery

factor（%）

Cuppm

Pbppm

Znppm

Drill Log of Hole #RLP-11-04

Hole No.

No.Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery

factor（%）

Description

2.02meta-

andesite02

Gray to dark green, fine-grained texture and massive structure, main mineral composition are amphibole and quartz. Quartz and calcite veins are common to see as irregular distribution. Occasionally to see pyrrhotite,the content is <1%. Two group joints,20°and 40°to core axis. 42.45-42.65m，strong silicification,white color. 48.97m,20mm width calcite vein. 54.04-55.39m,weak magnetic,strong epidotization,develop pyrrhotite veins,40°to core axis,the content is about 5%. 59.44-60.14m，develop pyrrhotite,weak magnetic,the content is about 2%. 78.27-78.50m，white quartz veins,also some calcite veins. 86.00m,lumpy pyrrhotite. 89.92-91.66m,weak magnetic,develop pyrrhotite veins,the content is about 5%. 100.61-103.01m，mafic intrusive rock,medium grained,more biotite,a little bit sulphide. 114.13-117.00m，weak magnetic,strong epidotization,the content of pyrrhotite is about 5%. 130.64m,20mm width pyrrhotite vein. 139.88-142.13m，weak magnetic,strong silicification,the content of pyrrhotite is about 5%. 151.72-155.22m,white quartz vein,occasionally to see sulphide.

99160.52159.84

169.77 7.22 7.23 100

ZK4

ZK4

quzrtz vein and stong

silicification meta-andesite

162.5403

162.54

White,strong silicification,develop quartz veins,chlorite and epidotization,weak magnetic,the content of pyrrhotite is about 2%. 162.54-163.07m，quartz vein,epidotization,Po=2%. 163.07-164.47m，strong silicification meta-andesite,weak magnetic,Po=2%. 164.47-169.77m，quartz vein and silicification meta-andesite,Po=2%.

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H 456 171.00 1.23 1.23 100 710 <20 120 250 <10 <5 <0.3 340 70

RL.H-457 172.36 1.36 1.36 100 2580 110 470 300 <10 860 70

RL.H-458 176.21 177.39 N.A. N.A. N.A. N.A. N.A. <5 4.8 N.A. N.A.

ZK4 04meta-

andesite169.77 175.91 5.74 6.14 93

Gray to dark green, fine-grained texture and massive structure, main mineral composition are amphibole and quartz.169.77-172.36m，Po=5%, irregular veins.

light flesh red color,medium-fine grained,main mineral composition are quartz and felspar.176.21-177.39m，the core look like sand,only collect some of them as sample.

177.39 0.66 1.48 45ZK4 05 granite 175.91

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 634089.253 East: Original Units: M North: North: 5440803.821 North: Storage: Markham Elevation: Elevation: 510.628 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

TypeFFF

Page 5 of 12

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK6

Diamond Drill Hole Report Project Number:

Drilling Casing Location OtherAzimuth: 90 Length: 0.22 meters Township: Richardson Lake Area Contractor: TOPRANKDip: -60 Pulled: No Claim No: 4252243 Spotted by: ShawnLength: 141.73 meters Capped: Yes NTS: Coord Type: Started: 18-May-11 Cemented: No Surveyed Date: Completed: 20-May-11 Logged by: ShawnLogged: 21-May-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:

Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:

Target: VETM anomaly supported by Geotech reportComments: The drill hole intersected approximately 77 metres of chert-sulphide iron formation from 39.1 metres to 116.31 metres flanked by mafic volcanics.

Deviation TestsDistance(m)

16-Nov-12

Azimuth38.10 128.883.82 101.4

129.54 105.5

4B

From To From To

ZK6 01 Overburden 0.00 0.22 0.22 0.00 0 Overburden\casing.

ZK6 02meta-

andesite0.22 4.78 4.56 4.51 99

Grey green- grey,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization, sulfide is occasionally to find,the content is <1%.

ZK6 03K-feldspar granite

4.78 6.70 1.92 1.92 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar.Occasionally to see pyrrhotite,the content is <1%.

RL.H-335 11.39 12.44 1.05 1.05 100 300 <20 160 140 <10 280 60

RL.H-336 13.54 1.10 1.10 100 130 <20 100 130 <10 300 40

RL.H-337 14.62 1.08 1.08 100 210 <20 210 140 <10 310 90

RL.H-338 15.85 1.23 1.23 100 60 30 20 <10 <10 60 <10

RL.H-339 16.60 0.75 0.75 100 210 <20 140 100 <10 240 30

RL.H-340 18.06 1.46 1.46 10030 30 20 <10 <10 30 <10

RL.H-342 19.36 1.30 1.30 100 100 <20 130 110 20 360 40

RL.H-343 20.51 1.15 1.15 100 140 <20 120 150 <10 340 50

RL.H-344 21.66 1.15 1.15 100 280 720 200 160 <10 1060 20

RL.H-345 22.16 0.50 0.50 100 1100 <20 60 220 20 30 <10

RL.H-346 23.61 1.45 1.44 99 110 <20 140 70 <10 440 20

RL.H-347 24.54 0.93 0.92 99 730 <20 90 140 <10 80 70

RL.H-348 25.22 0.68 0.67 99 870 <20 50 270 <10 70 40

RL.H-349 26.26 0.94 0.93 99 790 <20 160 170 <10 720 20

RL.H-350 27.23 1.07 1.07 100 60 <20 50 50 <10 90 <10

RL.H-351 28.60 1.37 1.37 100 1160 <20 110 250 <10 25 2.8 40 50

RL.H-353 29.80 1.20 1.20 100 300 20 70 30 30 50 <10

RL.H-354 31.00 1.20 1.20 100 210 <20 90 40 20 40 1042.8618.06

meta-andesite

with06ZK6

100

Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar. 15.85-16.60m is neta andesite ,occasionally to see pyrrhotite,the content is <1%.

Grey-green to grey-white,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization.One group joint,70°to core axis,the core length is <0.6m。 The rock developed much pyrrhotite and pyrite,distributed as spot-like,irregular veinlets,heavily disseminated and massive,sulphide occur as subhedral to xenomorphic granular aggregates,the content is about 80%. 18.06-21.66m，Po and minor Py,occur as spot-like and irregular veinlets the content is about 2%. 21.66-22.16m,massive sulphide,Po and Py,the content of sulphide is >95%，and Py=5%. 22.16-23.61m，Po,occur as spot-like,PO=2%,silicification. 23.61-23.95m，massive sulphide,Po and Py,the content of sulphide is >95%，and Py=20%.

23 95-24 54m Po and a little bit Clp occur as spot-like and irregular10024.7224.80

0.92 100 Dark green,fine-grained,massive structure,Quartz and calcite veins are common to see as irregular distribution..Occasionally to see pyrrhotite.11.39-12.00m more Po and Py,the content is about 2%.

ZK6 05K-feldspar granite

14.62 18.06 3.44 3.44

ZK6 04meta-

andesite6.70 14.62 7.92

Drill Log of Hole #RLP-11-06

Hole No.

No.Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery

factor（%）

Description

Sample log Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Recovery

factor（%）

Cuppm

Pbppm

Znppm

Crppm

Coppm

Nippm

Moppm

Auppb

Agg/t

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H 354 31.00 1.20 1.20 100 210 <20 90 40 20 40 10

RL.H-355 32.00 1.00 1.00 100 390 <20 190 50 <10 12 0.9 40 30

RL.H-356 33.22 1.22 1.20 98 460 <20 260 80 <10 23 0.9 60 10

RL.H-357 34.49 1.27 1.25 98 160 <20 150 120 <10 720 50

RL.H-358 35.75 1.26 1.25 99 270 <20 290 260 <10 1120 40

RL.H-359 37.10 1.35 1.35 100 410 <20 480 80 <10 10 0.5 80 80

RL.H-360 38.10 1.00 1.00 100 140 <20 170 120 <10 860 40

RL.H-361 39.10 1.00 1.00 100 150 <20 180 130 <10 790 40

RL.H-362 40.00 0.90 0.90 100 260 <20 210 170 <10 90 110

RL.H-364 40.90 0.90 0.90 100 350 <20 260 170 <10 30 60

RL.H-365 41.79 0.89 0.89 100 390 <20 320 110 <10 7 0.6 60 20

RL.H-366 42.86 1.07 1.07 100 100 <20 150 40 20 60 <10

RL.H-367 44.36 1.50 1.50 100 50 20 30 <10 <10 40 <10

RL.H-368 45.86 1.50 1.50 100 60 30 20 <10 <10 30 <10

RL.H-369 46.92 1.06 1.06 100 170 <20 110 70 <10 60 <10

RL.H-370 47.80 0.88 0.88 100 320 <20 210 110 <10 30 360

RL.H-371 48.90 1.10 1.10 100 290 <20 90 120 <10 40 40

RL.H-372 50.10 1.20 1.20 100 390 <20 230 220 <10 9 0.8 20 40

RL.H-373 51.33 1.23 1.20 98 310 <20 100 200 <10 11 0.8 140 70

RL.H-375 52.59 1.26 1.22 97 150 <20 180 140 <10 90 <10

RL.H-376 53.82 1.23 1.20 98 330 20 60 140 <10 50 20

RL.H-377 55.08 1.26 1.25 99 370 <20 150 210 <10 30 10

RL.H-378 56.39 1.31 1.29 99 350 <20 590 180 <10 26 1.2 30 30

Dark-brassy to dark-bronze,sulphide are Py and Po, occur as subhedral to xenomorphic granular aggregates, and devloped as massive and dense disseminated,the content of sulfide is >80%, the content of pyrrhotite is slightly higher than pyrite. 45.86-46.92m，meta-andesite with Py and Po,silicification,sulphide is about 10%. 46.92-47.80m，masiive sulphide,>95%,the content of pyrrhotite is almost same to pyrite. 47.80-48.34m，meta-andesite with Py and Po,sulphide is about 10%. 48.34-51.33m，masiive sulphide,>95%, the content of pyrrhotite is slightly

3.00 3.00 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar.

massive to h il

42.8618.06with pyrrhotite and pyrite

06ZK6

ZK6 07K-feldspar granite

42.86 45.86

23.95 24.54m，Po and a little bit Clp, occur as spot like and irregular veinlets,the content of sulphide is about 10%. 24.54-25.22m，massive sulphide,Po and Py,the content of sulphide is >95%，and Py=10%. 25.22-26.16m，heavily disseminated sulphide,Po and minor Py，the content of sulphide is about 60%. 26.16-27.23m，medium-grained intermediate intrusive，grey to grey-white，mineral composition are amphibole,feldspar and quartz,development of the Po and Py as fine granular aggregates，about 3%. 27.23-28.60m，massive to heavily disseminated sulphide，Po and Py，the content of sulphide is about 80%，and Py=20%. 28.60-37.10m，the content of sulphide is about 30%，irregular veinlets，Py=Po. 37.10-39.10m，pot-like sulphide,about 2%. 39.10-41.79m，dense veinlets,the content of sulfhide is about 60%,Py=25.

41 79-42 86m pot-like and lumpy Po about 5% silicification

10024.7224.80

第 7 页，共 19 页

From To From To

Drill Log of Hole #RLP-11-06

Hole No.

No.Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery

factor（%）

Description

Sample log Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Recovery

factor（%）

Cuppm

Pbppm

Znppm

Crppm

Coppm

Nippm

Moppm

Auppb

Agg/t

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-379 57.64 1.25 1.25 100 320 <20 160 140 <10 20 60

RL.H-380 58.94 1.30 1.30 100 470 <20 200 170 <10 20 40

RL.H-381 60.18 1.24 1.24 100 480 <20 110 130 <10 20 110

RL.H-382 61.38 1.20 1.20 100 640 30 130 110 <10 14 1 20 160

RL.H-383 62.48 1.10 1.10 100 260 <20 250 100 <10 10 110

RL.H-384 63.63 1.15 1.15 100 250 <20 130 120 <10 15 0.6 20 160

RL.H-386 64.83 1.20 1.20 100 220 <20 250 140 <10 20 110

RL.H-387 66.13 1.30 1.30 100 260 <20 1060 140 <10 20 80

RL.H-388 67.13 1.00 1.00 100 270 <20 240 150 <10 21 0.8 20 120

RL.H-389 68.28 1.15 1.15 100 270 <20 170 130 <10 20 90

RL.H-390 69.48 1.20 1.20 100 170 <20 220 80 <10 50 10

RL.H-391 70.68 1.20 1.20 100 130 <20 110 60 <10 8 <0.3 60 <10

RL.H-392 71.98 1.30 1.30 100 180 <20 110 100 <10 11 0.4 50 30

RL.H-393 72.98 1.00 1.00 100 160 30 70 80 <10 25 0.5 30 160

RL.H-394 73.98 1.00 1.00 100 340 <20 120 160 <10 40 130

RL.H-395 75.28 1.30 1.30 100 130 <20 330 90 <10 140 10

RL.H-397 76.48 1.20 1.20 100 120 <20 230 80 <10 590 10

RL.H-398 77.72 1.24 1.24 100 110 <20 380 60 <10 5 0.3 70 10

RL.H-399 79.02 1.30 1.30 100 70 <20 430 50 <10 80 10

RL.H-400 79.82 0.80 0.80 100 150 <20 250 130 <10 80 <10

RL.H-401 80.72 0.95 0.95 100 210 <20 360 190 <10 50 10

RL.H-402 81.69 0.92 0.90 98 150 <20 80 110 <10 9 0.4 40 130

RL.H-403 82.46 0.77 0.75 98 80 <20 140 70 <10 30 110

ZK6 10K-feldspar granite

82.46 83.20 0.74 0.73 98 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar.

RL.H-404 83.20 0.74 0.73 98

50 <20 20 20 <10 30 <10

RL.H-405 84.45 1.25 1.25 100 120 30 150 50 <10 12 <0.3 30 70

RL.H-406 85.69 1.24 1.24 100 80 <20 50 60 <10 30 100

100

Grey-green to grey-white,fine-grained texture and massive structure,Po and Py,the sulphide is about 60%,occur as irregular veinlets,heavily disseminated and massive. 68.28-71.98m，Po,about 10%,irregular veinlets. 71.98-73.98m，Po and Py,dense disseminated,about 80%,the content of pyrrhotite is slightly higher than pyrite 73.98-79.25m，Po and minor Py,spot like and veinlets,about 10%。 79.25-80.77m，dense disseminated to masiive sulphide,Po and minor Py,about 70%。 80.77-82.46m，dense disseminated to masiive sulphide,Py and minor Po,about 70%。

22.29 99 higher than pyrite. 51.33-51.70m，meta-andesite with Py and Po,sulphide is about 20%. 51.70-52.02m，masiive sulphide,>95%, the content of pyrrhotite is slightly higher than pyrite. 52.02-52.59m，meta-andesite with Py and Po,silicification,sulphide is about 2%. 52.59-68.28m，massive to dense disseminated,sulphide,>90%, the content of pyrrhotite is slightly higher than pyrite.

ZK6 09

meta-andesite

with pyrrhotite and pyrite

68.28 82.46 14.18 14.15

ZK6heavily

disseminated sulfide

08 45.86 68.28 22.42

RL.H-408 86.74 1.05 1.05 100 40 <20 40 30 <10 <5 1.4 70 <10

RL.H-409 87.89 1.15 1.15 100 20 <20 20 40 <10 100 <10

RL.H-410 88.89 1.00 1.00 100 70 <20 60 40 <10 20 120

RL.H-411 89.92 1.03 1.03 100 160 <20 60 60 <10 10 100

RL.H-412 91.06 1.14 1.14 100 80 <20 60 30 <10 40 70

RL.H-413 91.77 0.71 0.71 100 160 <20 100 140 <10 20 70

RL.H-414 92.48 0.71 0.71 100 140 <20 60 40 <10 80 <10

RL.H-415 93.80 1.32 1.32 100 120 <20 90 70 <10 <10 100

RL.H-416 95.00 1.20 1.20 100 150 <20 80 60 <10 <5 0.5 20 100

RL.H-417 96.01 1.01 1.01 100 150 <20 50 80 <10 20 70

RL.H-419 97.26 1.25 1.25 100 90 <20 80 60 <10 50 30

RL.H-420 98.10 1.15 1.15 100 140 <20 40 90 <10 40 10

RL.H-421 99.64 1.23 1.23 100 230 <20 90 90 <10 12 1 30 60

RL.H-422 100.89 1.25 1.25 100 90 <20 50 60 <10 40 10

RL.H-423 102.11 1.22 1.22 100 590 <20 50 70 <10 40 50

RL.H-424 103.21 1.10 1.10 100 340 <20 120 80 <10 20 60

RL.H-425 104.41 1.20 1.20 100 50 <20 50 30 <10 50 20

RL.H-426 105.16 0.75 0.75 100 70 <20 60 50 <10 10 100

RL.H-427 106.28 1.12 1.12 100 180 <20 90 110 <10 <5 0.9 20 50

ZK6 12K-feldspar granite

106.28 108.00 1.72 1.72 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar.

RL.H-428 108.00 1.72 1.72 100

50 <20 20 <10 20 10 <10

RL.H-430 109.22 1.22 1.22 100 140 <20 90 60 <10 50 80

Py and Po,the content of sulfide is about 70%,the content of Py is slightly higher than Po. 83.20-85.69m,massive sulfide,Py and minor Po,>95. 85.69-87.89m,meta-andesite with Py and Po,silicification,sulphide is about 5%. 87.89-89.92m,massive sulfide,Py and minor Po,>90. 89.92-91.06m，meta-andesite with Py and Po,sulphide is about 10%. 91.06-91.77m，massive sulfide,Py and minor Po,>90. 91.77-92.48m，sulphide is about 10%. 92.48-99.64m，dense disseminated to masiive sulphide,>80%，Py and Po,Po=30%. 99.64-101.48m，sulphide is about 40%,Po=Py. 101.48-102.21m，dense disseminated to masiive sulphide, about 60%， 102.21-102.73m，sulphide is about 25%. 102.73-103.46m，dense disseminated to masiive sulphide,>80%. 103.46-104.41m，sulphide is about 5%. 104.41-106.28m，ense disseminated to masiive sulphide,>90%，Py = Po

Sulphid ur m ii t d n di min t d P nd P th nt nt f P i

ZK6

heavily disseminated to massive

sulfide

11 83.20 106.28 23.08 23.06 100

第 8 页，共 19 页

From To From To

Drill Log of Hole #RLP-11-06

Hole No.

No.Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery

factor（%）

Description

Sample log Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Recovery

factor（%）

Cuppm

Pbppm

Znppm

Crppm

Coppm

Nippm

Moppm

Auppb

Agg/t

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-431 110.42 1.20 1.20 100 170 <20 60 40 <10 40 70

RL.H-432 111.83 1.41 1.41 100 110 <20 50 50 <10 40 70

RL.H-433 112.96 1.13 1.13 100 40 <20 20 20 <10 70 20

RL.H-434 114.03 1.07 1.07 100 90 <20 70 50 <10 20 80

RL.H-435 115.15 1.12 1.11 99 120 <20 80 50 <10 9 0.7 20 70

RL.H-436 116.31 1.16 1.14 98 160 <20 80 70 <10 10 80

RL.H-437 117.35 1.04 1.02 98 30 100 100 10 10 40 <10

RL.H-438 118.35 1.00 1.00 100 40 40 40 <10 <10 20 <10100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar.Sulfide is occasionally to find,One group joint,40°to core axis.

116.31 141.73 25.42 25.35

108.00

massive to heavily

disseminated sulfide

13ZK6

ZK6 14K-feldspar granite

Sulphide occur asmasiive to dense disseminated，Po and Py，the content of Py is slightly higher than Po. The content of sulphide is >80%； 108.00-111.83m，massive sulfide,>90. 111.83-112.96m,meta-andesite with Py and Po,irregular veinlets,sulphide is about 10%. 112.96-116.31m，dense disseminated to masiive sulphide, the content of sulfide is >90%；

998.278.31116.31

第 9 页，共 19 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 634713.398 East: Original Units: M North: North: 5441172.069 North: Storage: Markham Elevation: Elevation: 507.698 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

Type

Page 6 of 12

Drilling Casing Location

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK7

Diamond Drill Hole Report Project Number:

OtherAzimuth: 55 Length: 1.30 meters Township: Richardson Lake Area Contractor: TOPRANKDip: -50 Pulled: No Claim No: 4252244 Spotted by: ShawnLength: 124.05 meters Capped: Yes NTS: Coord Type: Started: 4-April-11 Cemented: No Surveyed Date: Completed: 6-April-11 Logged by: ShawnLogged: 7-April-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:

Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:

Target: VETM anomaly supported by Geotech reportComments: The drill hole also intersected another much narrower (1 metre) interval of metasediment with pyrrhotite bands and lamination from 32.40 to 33.65 metres. Pyrrhotite stringers were also locally intersected in the mafic metavolcanics in theupper portion of the drill hole.

AzimuthDeviation Tests

Distance(m)

16-Nov-12

The date was lost by drilling company.

5B

From To From To

ZK7 01 Overburden 0.00 1.30 1.30 0.00 0 Overburden\casing.

RL.H-280 1.30 2.40 1.10 1.10 100 120 <20 210 120 <10 310 50

RL.H-281 3.60 1.20 1.20 100 240 <20 130 210 <10 5 <0.3 420 60

RL.H-282 4.90 1.30 1.30 100 130 <20 270 200 <10 360 50

RL.H-283 6.12 1.22 1.20 98 110 <20 490 120 <10 320 50

RL.H-284 7.22 1.10 1.08 98 250 <20 320 160 <10 <5 0.3 330 80

RL.H-285 8.23 1.01 1.00 98 210 <20 170 170 <10 350 80

RL.H-287 9.40 1.17 1.17 100 440 <20 140 170 <10 280 90

RL.H-288 10.50 1.10 1.10 100 120 <20 90 80 <10 210 40

RL.H-289 28.77 29.87 1.10 1.10 100 110 <20 150 80 <10 150 50

RL.H-290 30.81 0.94 0.94 100160 <20 150 80 <10 6 <0.3 100 50

RL.H-291 31.81 1.00 1.00 100<10 <20 40 <10 <10 30 <10

RL.H-292 32.81 1.00 1.00 100310 <20 1460 80 <10 130 30

RL.H-293 33.81 1.00 1.00 100

250 <20 370 130 <10 10 0.5 60 60

RL.H-294 34.91 1.10 1.10 100 70 <20 130 70 <10 130 40

RL.H-295 36.11 1.20 1.20 100 110 <20 140 60 <10 140 50

RL.H-296 43.51 44.81 1.30 1.30 100 130 <20 120 80 <10 140 50

RL.H-298 46.01 1.20 1.20 100 100 <20 140 60 <10 100 40

RL.H-299 46.91 0.90 0.90 100 60 <20 110 30 <10 40 30

RL.H-300 47.91 1.00 1.00 100 50 <20 130 20 <10 40 30

RL.H-301 49.01 1.10 1.10 100 110 <20 220 60 <10 5 <0.3 80 30

Drill Log of Hole #RLP-11-07

Hole No.

No.Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery

factor（%）

Description

Sample log Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Recovery

factor（%）

Cuppm

Nippm

Moppm

Pbppm

Znppm

Auppb

Agg/t

Crppm

Coppm

29.87 20.47 20.44 100

Grey to grey-white,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar，quartz and biotite,development of the chlorite，epidotization and silicification. Calcite and quartz veins are common to see.The content of sulphide is <1%.

Grey to grey green，fine-grained texture and massive structure,main mineral composition are amphibole,feldspar，quartz and biotite,development of the chlorite，epidotization and silicification.Po and Py occur as spot-like and irregular veinlets,subhedral to xenomorphic granular,the content is about 2-6%. Two group joint,20°and 40°to core axis.

998.038.109.401.30

meta-andesite

with pyrrhotite and pyrite

meta-andesite

9.40

02ZK7

ZK7 04

ZK7 03

ZK7 05meta-

andesite 33.81 44.81 11.00

3.94 10033.81

Grey to dark-green,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar，quartz and biotite,development of the chlorite，epidotization. The rock developed pyrrhotite and pyrite,locally developed minor chalcopyrite.Sulphide occur as banded veinlets and irregular veinlets,the length of the vein is aboout 1-10mm。The content of sulphide is about 10%，Po=Py,and the content of Clp is<1%。The banded vein is 50°to core axis. 30.53m occur a little bit chalcopyrite.

meta-andesite

with pyrite and

pyrrhotite

29.87 3.94

11.00 100 Grey to grey-green,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar，quartz,dark minerals are directional arrangement,50°to core axis.

Grey to grey-green fine-grained texture and massive structure main mineral

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-302 49.91 0.90 0.90 100 110 <20 410 130 <10 6 <0.3 80 40

RL.H-303 50.90 0.99 0.99 100 220 <20 320 100 <10 <5 <0.3 110 30

RL.H-304 52.00 1.10 1.10 100 130 <20 120 120 <10 240 40

RL.H-305 53.10 1.10 1.10 100 70 <20 110 50 <10 50 30

RL.H-306 54.20 1.10 1.10 100 210 <20 1130 120 <10 6 1.4 110 60

RL.H-307 55.40 1.20 1.20 100 130 30 350 110 <10 70 40

RL.H-309 56.40 1.00 1.00 100 250 20 220 60 <10 50 50

RL.H-310 57.27 0.87 0.87 100 80 <20 180 30 <10 40 40

RL.H-311 58.27 1.00 1.00 100 40 <20 150 20 <10 40 40

RL.H-312 74.59 75.59 1.00 1.00 100 110 <20 170 80 <10 160 30

RL.H-313 76.79 1.20 1.20 100 160 <20 250 100 <10 150 40

RL.H-314 77.79 1.00 1.00 100 110 <20 310 110 <10 5 <0.3 200 30

RL.H-315 78.74 0.95 0.95 100 100 <20 230 140 <10 310 40

12.46

66.78

ZK7

meta-andesite

with pyrite and

pyrrhotite

06 44.81 57.27 12.46

100

100

Grey to grey green,fine grained texture and massive structure,main mineral composition are amphibole,feldspar，quartz and biotite.Development of the chlorite，epidotization and silicification.Sulphide occur as banded veinlets and irregular veinlets,is about 20%,P0=Py.The banded vein is 60°to core axis. 44.81-50.90m,Py and Po,Py=4Po;49.85m a little bit Clp. 50.90-57.27m,Po and Py，Po=3Py.

Grey to grey-green,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar，quartz and biotite.Development of the chlorite，epidotizatiohe and silicification.Calcite and quartz veins are common to see.The content of sulphide is <1%。 75.77m,pyrite vein,about 2mm length； 76.11m,pyrite vein,about 5mm length； 76.87m,pyrite vein,about 5mm length； 81.74m,quartz vein,about 6mm length； 95.50m,quartz vein,about 5mm length；

ZK7 07meta-

andesite 57.27 124.05 66.78

第 10 页，共 19 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 634409.031 East: Original Units: M North: North: 5441157.381 North: Storage: Markham Elevation: Elevation: 511.544 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

Azimuth Dip Type61.3 53 F64.3 52.5 F64.9 51.7 F64.8 51.4 F

Page 7 of 12

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK8

Diamond Drill Hole Report Project Number:

Drilling Casing Location OtherAzimuth: 65 Length: 2.59 meters Township: Richardson Lake Area Contractor: TOPRANKDip: -55 Pulled: No Claim No: 4252243 Spotted by: ShawnLength: 150.88 meters Capped: Yes NTS: Coord Type: Started: 15-May-11 Cemented: No Surveyed Date: Completed: 17-May-11 Logged by: ShawnLogged: 18-May-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:

Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:

Target: VETM anomaly supported by Geotech reportComments: The drill hole intersected approximately 3.5 metres of metasediment with magnetite bands from 36.8 metres to 40.35 metres flanked by mafic volcanics cut by intermittent granite dykes.

141.73

Deviation TestsDistance(m)

16-Nov-12

38.1083.82

129.54

6B

From To From To

ZK8 01 Overburden 0.00 2.59 2.59 0.00 0 Overburden\casing.

ZK8 02meta-

andesite2.59 15.46 12.87 12.82 100

Dark grey green to grey, fine-grained,massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization.Quartz veins are common and occur as irregular veinlets.One group joint, 40°to core axis.The core length are between 0.4 to 1.0m.

ZK8 03K-feldspar granite

15.46 17.61 2.15 2.15 100 Grey and light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.One group joint, 40°to core axis.

RL.H-326 41.15 42.30 1.15 1.15 100 110 <20 190 120 <10 190 50

RL.H-327 43.55 1.25 1.25 100 100 <20 140 120 <10 200 60

ZK8 05K-feldspar granite

50.29 52.64 2.35 2.35 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.

RL.H-328 58.69 60.00 1.31 1.30 99 190 <20 100 150 <10 230 60

RL.H-329 60.65 0.65 0.64 99 1170 <20 190 110 <10 160 70

RL.H-331 61.91 1.26 1.25 99 160 <20 100 130 <10 220 60

ZK8 07K-feldspar granite

91.21 98.64 7.43 7.38 99 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.The rock are broken.

RL.H-332 114.30 115.58 1.28 1.25 98 170 400 160 60 <10 80 50meta-

38.5791.21ZK8 06meta-

andesite

Grey green to grey,fine-grained,massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization . Quartz and calcite veins are common and occur as irregular veinlets. Two group joint,20°and 50°to core axis.The core length are between 0.2 to 1.2m. Pyrrhotite is occasional to find,the content is <1%.62.00-62.65m,alittle bit Clp and Po cccur together.

9932.2852.64

Dark grey green,fine-grained,massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization .

ZK8 04meta-

andesite17.61

Pbppm

Description

Dark grey to grey,fine-grained,massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization . Quartz and calcite veins are common and occur as irregular veinlets.One group joint, 40°to core axis.The core length are between 0.2 to 1.2m. 31.82-31.90m,white quartz vein； 36.25-50.29m,strong epidotization,occur as small banded veins. Pyrrhotite is occasional to find,the content is <1%.

Recovery

factor（%）

50.29 32.68 32.24 99

Auppb

Nippm

Moppm

Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Recovery

factor（%）

Cuppm

Znppm

Crppm

Coppm

Drill Log of Hole #RLP-11-08

Hole No.

No.Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Agg/t

Sample log

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-333 116.65 1.07 1.05 98 160 <20 150 60 <10 60 50

RL.H-334 117.85 1.20 1.18 98 240 <20 180 60 <10 70 50

ZK8 09K-feldspar granite

143.56 147.31 3.75 3.75 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.The core length are between 0.4 to 1.0m.

ZK8 10meta-

andesite147.31 150.88 3.57 3.57 100

Grey to grey green,fine-grained,massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization .

metaandesite

08ZK8 143.5698.64 Quartz and calcite veins are common.The content of Po is <1%. 114.30-117.85m，Po>1%. 132.58-136.24m，Granite and meta-andesite.

10044.7544.92

第 11 页，共 19 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 634321.713 East: Original Units: M North: North: 5443331.717 North: Storage: Markham Elevation: Elevation: 502.892 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

Type

Page 8 of 12

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK9

Diamond Drill Hole Report Project Number:

Drilling Casing Location OtherAzimuth: 270 Length: 1.51 meters Township: UPPER SCOTCH LAKE AREA Contractor: TOPRANKDip: -65 Pulled: No Claim No: 4252236 Spotted by: ShawnLength: 133.20 meters Capped: Yes NTS: Coord Type: Started: 30-March-11 Cemented: No Surveyed Date: Completed: 1-April-11 Logged by: ShawnLogged: 2-April-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:

Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:

Target: VETM anomaly supported by Geotech reportComments: The 16.7 metres of granite intersected at the end of ZK9 may represent the main body of the Norway Lake pluton; the 10.5 metres of mafic metavolcanic immediately uphole of this granite exhibits deformation and biotite-chlorite alterationindicative of a contact metamorphic aureole.

Deviation TestsDistance(m) Azimuth

16-Nov-12

The date was lost by drilling company.

7B

From To From To

ZK9 01 Overburden 0.00 1.51 1.51 0.00 0 Overburden\casing.

RL.H-227 12.38 13.43 1.05 1.05 100 90 130 760 100 <10 8 220 40

RL.H-228 14.63 1.20 1.20 100 120 110 1150 70 <10 12 90 20

RL.H-229 15.83 1.20 1.20 100 190 <20 550 80 <10 18 0.6 100 30

RL.H-230 17.13 1.30 1.30 100 120 <20 2640 110 <10 36 130 40

RL.H-232 18.37 1.24 1.24 100 150 <20 600 120 <10 11 1.4 170 40

RL.H-233 19.37 1.00 1.00 100 210 20 70 150 <10 16 2.1 110 60

RL.H-234 20.42 1.05 1.05 100 60 <20 100 50 <10 7 50 10

RL.H-235 21.62 1.20 1.20 100 40 <20 140 30 <10 6 70 10

RL.H-236 22.82 1.20 1.20 100 80 <20 390 40 <10 13 60 10

RL.H-237 23.87 1.05 1.05 100 140 <20 360 100 <10 15 1.8 30 30

RL.H-238 25.12 1.25 1.25 100 110 <20 110 80 <10 10 60 30

RL.H-239 26.27 1.15 1.15 100 220 20 570 170 <10 21 70 70

RL.H-240 27.37 1.10 1.10 100 260 <20 1330 170 <10 26 2.2 70 70

RL.H-241 28.57 1.20 1.20 100 360 40 730 200 <10 26 100 80

RL.H-243 29.57 1.00 1.00 100 210 <20 390 210 <10 27 60 90

RL.H-244 30.77 1.20 1.20 100 250 <20 750 220 <10 30 3.3 50 100

RL.H-245 31.97 1.20 1.20 100 220 <20 320 110 <10 18 70 40

RL.H-246 33.17 1.20 1.20 100 170 <20 270 170 <10 23 80 70

RL.H-247 34.27 1.10 1.10 100 180 <20 450 130 <10 19 1.6 70 50

RL.H-248 35.51 1.24 1.24 100 100 <20 180 100 <10 <5 250 40

RL.H-249 36.91 1.40 1.40 100 120 <20 310 100 <10 12 120 50

RL.H-250 38.16 1.25 1.25 100 110 <20 260 80 <10 9 0.8 70 40

RL H-251 39 46 1 30 1 30 100 120 <20 140 50 <10 <5 130 40

Depth（m） Thickness

（m）

Length of core （m）

Agg/t

Sample log

Recovery

factor（%）

Cuppm

Znppm

Crppm

Coppm

Drill Log of Hole #RLP-11-09

Hole No.

No.Rock/Ore

type

Recovery

factor（%）

13.43 11.92 11.92 100

Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Auppb

ZK9 02meta-

andesite1.51

Pbppm

Description

Grey green to grey, fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite, epidotization and silicification.Pyrrhotite is occasional to find,the content is <1%,occur as xenomorphic granular. One group joint, 60°to core axis.The core length are <0.4m.

Nippm

Moppm

10024.7338.16ZK9meta-

andesite with Po

03 13.43

Grey green to grey, fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite, epidotization and silicification. Generally developed pyrrhotite, locally developed minor pyrite and chalcopyrite.Pyrrhotite occur as subhedral to xenomorphic granular,distributed as irregular veinlets,also spot-like, lumpy and disseminated,the content is 5-20%. One group joint, 60°to core axis.The core length are <0.5m. 13.43-25.12m，Po occur asirregular veinlets,lumpy and spot-like,the content is about 5%.18.50m,a little bit Clp. 25.12-38.16m，distributed Po,the content is about 20%. 31.46m,32.94m and 33.76m,a little bit Clp.

24.73

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-251 39.46 1.30 1.30 100 120 <20 140 50 <10 <5 130 40

RL.H-252 40.66 1.20 1.20 100 140 60 500 80 <10 <5 130 50

RL.H-254 41.76 1.10 1.10 100 110 <20 130 60 <10 <5 130 40

RL.H-255 42.96 1.20 1.20 100 140 <20 100 70 <10 <5 110 40

RL.H-256 44.16 1.20 1.20 100 140 <20 110 70 <10 <5 120 50

RL.H-257 45.51 1.35 1.35 100 110 <20 120 70 <10 <5 120 50

RL.H-258 46.71 1.20 1.20 100 110 <20 120 70 <10 <5 130 40

RL.H-259 47.85 1.14 1.14 100 120 <20 150 60 <10 <5 <0.3 140 50

RL.H-260 49.05 1.20 1.20 100 120 <20 110 60 <10 <5 140 40

RL.H-261 50.15 1.10 1.10 100 90 <20 120 130 <10 <5 270 50

RL.H-262 51.09 0.94 0.94 100 70 <20 110 120 <10 <5 240 40

RL.H-263 52.09 1.00 1.00 100 120 <20 90 60 <10 <5 130 40

RL.H-265 53.29 1.20 1.20 100 170 20 170 50 <10 7 100 30

RL.H-266 54.35 1.06 1.06 100 140 <20 250 70 <10 <5 80 30

RL.H-267 55.70 1.35 1.35 100 200 <20 180 130 <10 5 0.8 90 50

RL.H-268 57.00 1.30 1.30 100 260 <20 180 120 <10 5 1 30 50

RL.H-269 58.00 1.00 1.00 100 270 <20 300 110 <10 8 120 40

RL.H-270 59.17 1.17 1.17 100 80 <20 110 140 <10 <5 320 40

ZK9 06K-feldspar granite

59.17 61.35 2.18 2.18 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.

38.16

meta-andesite

with minor Po

meta-andesite with Po

52.09 59.17

Grey green to grey, fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite, epidotization.Calcite veins are common,the length of vein is between 2 to 10mm. Pyrrhotite is occasional to find,the content is <1%.

10013.9304

Grey white to grey green,fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and silicification. Generally developed pyrrhotite, locally developed minor chalcopyrite.Pyrrhotite occur as irregular veinlets and lumpy,the content is 5-10%. 56.20m,56.44m,56.90m and 56.96m,a little bit Clp. 58.00-59.17m,Po<1%。

7.087.08 100

ZK9

ZK9 05

13.9352.09

第 12 页，共 19 页

From To From To

Depth（m） Thickness

（m）

Length of core （m）

Agg/t

Sample log

Recovery

factor（%）

Cuppm

Znppm

Crppm

Coppm

Drill Log of Hole #RLP-11-09

Hole No.

No.Rock/Ore

type

Recovery

factor（%）

Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Auppb

Pbppm

DescriptionNippm

Moppm

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

ZK9 07meta-

andesite 61.35 116.20 54.85 54.70 100

Grey to dark grey green,fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and calcite veins. Two group joint,30°and 60°to core axis.The core length are between 0.3 to 1.0m. 78.83m and 83.73m,white quartz veins,the length is 17mm and 12mm.

ZK9 08K-feldspar granite

116.20 133.20 17.00 17.00 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.

第 13 页，共 19 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 636738.912 East: Original Units: M North: North: 5445230.614 North: Storage: Markham Elevation: Elevation: 514.427 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

TypeFFF

Page 9 of 12

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK10

Diamond Drill Hole Report Project Number:

Drilling Casing Location OtherAzimuth: 110 Length: 3.70 meters Township: UPPER SCOTCH LAKE AREA Contractor: TOPRANKDip: -55 Pulled: No Claim No: 4252235 Spotted by: ShawnLength: 123.44 meters Capped: Yes NTS: Coord Type: Started: 23-March-11 Cemented: No Surveyed Date: Completed: 25-March-11 Logged by: ShawnLogged: 26-March-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:

Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:

Target: VETM anomaly supported by Geotech reportComments: The 13.74 metres of quartz monzonite/granite intersected at the end of ZK10 may represent the main body of the Chill Lake Lake pluton.

Deviation TestsDistance(m)

16-Nov-12

Azimuth36.58 98.985.34 109.6

114.30 108.1

8B

From To From To

ZK10 01 Overburden 0.00 3.70 3.70 0.00 0 Overburden\casing.

RL.H-112 10.67 11.77 1.10 1.10 100 40 <20 100 90 <10 160 40RL.H-113 13.02 1.25 1.25 100 70 <20 150 110 <10 310 50RL.H-114 14.46 1.44 1.40 97 90 <20 140 110 <10 300 50RL.H-115 15.85 1.39 1.30 94 160 <20 170 110 <10 310 50RL.H-116 17.07 1.22 1.15 94 60 <20 170 110 10 300 40RL.H-117 18.29 1.22 1.20 98 80 <20 100 110 20 <5 <0.3 280 50RL.H-118 19.66 1.37 1.35 98 60 <20 110 110 10 310 50RL.H-119 20.66 1.00 1.00 100 50 <20 180 110 30 280 40

ZK10 04 massive sulfide 20.66 20.99 0.33 0.33 100 Brass-yellow hue,massive sulphide,Py=90%,Po=2%,a little bit Clp. RL.H-120 20.99 0.33 0.33 100

840 <20 50 100 70 130 100RL.H-122 22.06 1.07 1.07 100 230 <20 150 70 140 <5 <0.3 170 20RL.H-123 23.31 1.25 1.25 100 150 <20 120 90 <10 <5 <0.3 210 40RL.H-124 24.66 1.35 1.35 100 80 <20 180 120 20 330 50RL.H-125 26.00 1.34 1.34 100 90 <20 150 110 <10 280 40RL.H-126 26.94 0.94 0.94 100 <10 <20 30 10 <10 10 <10RL.H-127 27.94 1.00 1.00 100 <10 <20 30 <10 <10 100 <10RL.H-128 28.96 1.02 1.02 100 40 <20 160 90 <10 260 40RL.H-129 30.20 1.24 1.24 100 100 <20 120 100 30 270 40RL.H-130 31.50 1.30 1.30 100 90 <20 180 80 <10 250 30

RL.H-131 32.60 1.10 1.10 100 2200 <20 290 140 80 34 1.4 60 120

RL.H-133 33.52 0.92 0.92 100 5540 40 300 120 110 20 4.6 60 100RL H 134 35 05 1 53 1 53 100

Drill Log of Hole #RLP-11-10

Hole No. No. Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery factor（%）

Description

Sample log Assay Results

Sample No.

Location (m) Length（m）

Length of core （m）

Recovery factor（%）

Cuppm

Pbppm

Znppm

Crppm

Coppm

11.77 Grey to grey green,development of the chlorite and epidotization;Py=2%,Py occur as ubhedral to xenomorphic granular aggregates.Two group joint, 60° and 80°to core axis.

Nippm

Moppm

Auppb

Agg/t

8.708.8920.66 98

ZK10

ZK10 03meta-

andesite with Py

11.773.70meta-andesite02

Grey green,development of the chlorite and epidotization,quartz veinlet,orientation arrangement; Py=2%,speckles and irregular veinlet; 21.21m,quartz veinlet(5cm),Py speckles; 21.67m,22.40m,quartz veinlet(3cm); 21.21-22.52m，Py speckles,the content is about 3%; 26.00-27.94m，grey white, felsic volcanics;

10010.5110.51

Grey,medium-fine grained,massive structure, the content of Py is <1%.One group joint, 60°to core axis.977.818.07

ZK10

ZK10 06 massive sulfide

31.5020.99meta-

andesite with Py

05

100 Brass-yellow hue,massive sulphide,Py=80%,Po=10%,a little bit Clp. 31.95-32.32m,meta-andesite with Py.31.50 33.52 2.02 2.02

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-134 35.05 1.53 1.53 100 190 <20 170 110 <10 300 40RL.H-135 36.15 1.10 1.10 100 260 <20 170 90 10 250 30RL.H-136 37.35 1.20 1.20 100 60 <20 120 100 30 310 40RL.H-137 38.70 1.35 1.35 100 350 <20 130 100 <10 260 30RL.H-138 39.97 1.27 1.27 100 120 <20 130 90 <10 290 40

RL.H-139 41.15 1.18 1.18 1001860 20 80 140 20 22 1.6 10 230

RL.H-140 42.05 0.90 0.90 1007560 40 260 430 60 30 80

RL.H-141 43.05 1.00 1.00 100 180 20 <10 <10 <10 <10 <10RL.H-142 44.00 0.95 0.95 100 180 30 50 <10 <10 30 <10

RL.H-144 45.04 1.04 1.04 100 1930 30 470 190 30 14 1.6 10 140

RL.H-145 46.29 1.25 1.25 100 3410 50 280 240 180 30 150

RL.H-146 47.74 1.45 1.45 100 4470 40 220 500 50 14 3.4 10 80RL.H-147 48.84 1.10 1.10 100 640 <20 260 60 <10 110 20RL.H-148 50.29 1.45 1.45 100 360 <20 170 30 <10 80 20RL.H-320 51.39 1.10 1.10 100 130 <20 150 70 <10 270 30RL.H-321 52.69 1.30 1.30 100 300 <20 160 60 <10 210 30RL.H-322 53.64 0.95 0.95 100 310 <20 70 60 <10 130 40RL.H-323 54.56 0.92 0.92 100 180 <20 110 70 <10 170 40

Grey green-grey,development of the chlorite ,epidotization and siliconization. Py=2%,speckles and irregular veinlet; 37.65-37.90m,Py speckles.

1006.456.45ZK10 07meta-

andesite with Py

33.52 39.97

42.05 2.08 2.08 100ZK10 08 massive sulfide 39.97

Brass-yellow hue,massive sulphide,Py=55%,Po=35%,a little bit Clp. 41.15-42.05m，Py=Po=45%；

41.23m,Py,Po and Clp.

ZK10 09 felsic volcanics 42.05 44.00 1.95 1.95 100 Grey white,fine-grained to aphanitic texture,massive structure,main mineral composition are

feldspar,quatz.a little bit sulphide in.

47.7444.00massive sulfide10

Brass-yellow hue,massive sulphide,Py,Po and a little bit Clp. 45.04-45.30m,more Po,Po=40%,Py=50%；

46.00-47.14m,Po=Py； 45.30-45.50m,grey white, felsic volcanics;

1003.743.74ZK10

Grey green-grey,development of the chlorite,epidotization and siliconization. 48.69-49.04m，52.60-52.74m，52.89-53.04m,grey white, felsic volcanics,a little bit Py in.1006.826.8254.5647.74

meta-andesite with

Py11ZK10

第 14 页，共 19 页

From To From To

Drill Log of Hole #RLP-11-10

Hole No. No. Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery factor（%）

Description

Sample log Assay Results

Sample No.

Location (m) Length（m）

Length of core （m）

Recovery factor（%）

Cuppm

Pbppm

Znppm

Crppm

Coppm

Nippm

Moppm

Auppb

Agg/t

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

ZK10 12 felsic volcanics 54.56 75.73 21.17 21.17 99

Grey white,fine-grained to aphanitic texture,massive structure.main mineral composition are feldspar,quatz.a little bit Py in,Py<1%. One group joint, 50°to core axis.； 74.02-74.38m,grey-green,meta-mafic volcanics.

ZK10 13 meta-andesite 75.73 109.78 34.05 34.05 100

Grey,grey green,fine-grained,a little bit Py in. 75.98-76.33m、77.51-77.73m、78.52-78.95m、80.35-81.57m、88.47-88.32m,grey white, felsic volcanics; 92.61-93.06m、93.36-94.16m、95.53-96.75m、100.30-101.15m、102.01-102.26m,yellowish pink,felsic volcanics; 102.6-104.29m,104.78-105.46m,yellowish pink,felsic volcanics； 107.18-107.50m,grey white, felsic volcanics;

ZK10 14 K-feldspar granite 109.78 123.44 13.66 13.66 100 Light flesh red, main mineral composition are K-feldspar,quatz and biotite.

第 15 页，共 19 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 636874.032 East: Original Units: M North: North: 5445451.449 North: Storage: Markham Elevation: Elevation: 507.698 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

TypeFF

Page 10 of 12

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK11

Diamond Drill Hole Report Project Number:

Drilling Casing Location OtherAzimuth: 120 Length: 2.27 meters Township: UPPER SCOTCH LAKE AREA Contractor: TOPRANKDip: -50 Pulled: No Claim No: 4252235 Spotted by: ShawnLength: 117.35 meters Capped: Yes NTS: Coord Type: Started: 25-March-11 Cemented: No Surveyed Date: Completed: 27-March-11 Logged by: ShawnLogged: 28-March-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:

Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: Yes

Deviation TestsDistance(m)

Geophysics: Target: VETM anomaly supported by Geotech reportComments: The approximately 30 metres of quartz monzonite/granite intersected at the end of ZK11 may represent the main body of the Chill Lake Lake pluton.

16-Nov-12

Azimuth47.24 125.4

102.11 118.9

9B

From To From To

ZK11 01 Overburden 0 2.27 0 2.27 0 Overburden\casing.

RL.H-149 15.31 16.51 1.20 1.20 100 40 <20 100 290 <10 480 40RL.H-150 17.71 1.20 1.20 100 200 <20 80 380 <10 320 100RL.H-151 18.86 1.15 1.15 100 200 <20 120 280 <10 320 80RL.H-152 19.81 0.95 0.95 100 290 70 220 330 20 340 80RL.H-153 21.11 1.30 1.30 100 250 20 310 290 30 230 50RL.H-155 22.31 1.20 1.20 100 570 30 160 230 40 6 0.6 220 50RL.H-156 23.61 1.30 1.30 100 370 <20 160 210 10 240 80RL.H-157 24.71 1.10 1.10 100 410 <20 150 270 <10 260 70RL.H-158 25.91 1.20 1.20 100 220 <20 160 370 <10 300 90RL.H-159 27.26 1.35 1.35 100 290 <20 180 420 <10 290 80RL.H-160 28.41 1.15 1.15 100 250 <20 140 420 <10 <5 0.3 270 120RL.H-161 29.66 1.25 1.25 100 240 <20 130 320 40 310 70RL.H-162 30.86 1.20 1.20 100 260 <20 70 300 20 190 40RL.H-163 32.00 1.14 1.14 100 130 <20 60 100 <10 90 10RL.H-164 33.10 1.10 1.10 100 710 <20 160 440 <10 210 130RL.H-166 34.40 1.30 1.30 100 320 <20 170 390 30 6 0.5 280 100RL.H-167 35.75 1.35 1.35 100 240 <20 260 270 <10 290 80RL.H-168 36.95 1.20 1.20 100 330 <20 190 420 20 270 150RL.H-169 38.10 1.15 1.15 100 210 <20 160 300 <10 310 70RL.H-170 39.35 1.25 1.25 100 270 <20 160 260 20 300 70RL.H-171 40.65 1.30 1.30 100 240 <20 140 270 <10 280 90

02

Grey to grey green,development of the chlorite,epidotization and some quartz vein.Py=<1%, scattered specks.One group joint, 50°to core axis. 7.47m,white quartz vein(7cm),a little bit Py in,Py=1%; 7.70m,white quartz vein(7cm)； 7.95m,white quartz vein(3.5cm),a little bit Py in,Py=1%;

10014.2414.2416.512.27meta-andesiteZK11

Grey to Grey green, development of the chlorite,epidotization and some quartz vein.Py=2-15%,Po=1-5%,a little bit Clp,the content <1%.One group joint, 55°to core axis. 16.51-19.81m,Py=2%,scattered specks,irregular veinlets; 19.81-44.84m.Py and a little bit Po,the content is about 6%；

44.84-47.74m.Py=1%,scattered specks； 47.74-50.29m,Py=3%, irregular veinlets； 50.29-54.89m.Py=2%；54.25m,54.41m,white quartz vein(2-3cm),a little bit Py in; 54.89-61.44m,Py=12%,Po=1%,irregular veinlets,in lumps and heavily disseminated; 61.44-70.83m,the content of sulphide is about 5%,Py and minor Po, irregular veinlets; 70.83-72.75m,felsic volcanics, grey-white and light flesh red,a little bit Py in; 72.75-82.97m,Py,Po and minor Clp, the content of sulphide is about 6%. 77.30m,a little bit Clp. 82.97-83.27m,massive sulphide,Py=90%；

83.27-83.57m,heavily disseminated Py, Py=40%; 83.57-83.63m,massive sulphide, Py, sulphide =95%; 83.63-84.58m,Py,irregular veinlets, sulphide=15%; 84.58-84.64m,massive sulphide, Py, sulphide >95%; 84.64-86.87m, Py irregular veinlets, sulphide=2%;

Drill Log of Hole #RLP-11-11

Hole No. No. Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery factor（%）

Description

Sample log Assay Results

Sample No.

Location (m) Length（m）

Length of core （m）

Recovery factor（%）

Cuppm

Pbppm

Znppm

Crppm

Coppm

Nippm

Moppm

Auppb

Agg/t

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-172 41.80 1.15 1.15 100 220 <20 180 260 <10 320 50RL.H-173 43.10 1.30 1.30 100 280 <20 140 270 <10 6 <0.3 310 90RL.H-174 44.20 1.10 1.10 100 280 <20 120 260 <10 310 60RL.H-175 44.84 0.64 0.64 100 260 <20 120 220 10 270 60RL.H-177 46.29 1.45 1.45 100 150 <20 110 70 <10 200 50RL.H-178 47.74 1.45 1.45 100 130 <20 100 70 <10 200 40RL.H-179 48.99 1.25 1.25 100 160 <20 120 80 <10 200 50RL.H-180 50.29 1.30 1.30 100 730 <20 130 180 10 12 0.5 240 80RL.H-181 51.44 1.15 1.15 100 160 <20 120 70 <10 190 40RL.H-182 52.59 1.15 1.15 100 100 <20 100 60 <10 180 30RL.H-183 53.74 1.15 1.15 100 90 <20 110 60 <10 180 40RL.H-184 54.89 1.15 1.15 100 140 <20 140 80 <10 170 40RL.H-185 56.09 1.20 1.20 100 500 <20 160 340 20 <5 0.6 280 80RL.H-186 57.39 1.30 1.30 100 1100 <20 320 540 60 19 1.7 90 190RL.H-188 58.39 1.00 1.00 100 280 <20 120 250 160 150 50RL.H-189 59.44 1.05 1.05 100 520 <20 470 340 40 150 60RL.H-190 60.44 1.00 1.00 100 280 <20 300 180 10 90 50RL.H-191 61.44 1.00 1.00 100 970 <20 160 510 120 7 1.7 50 130RL.H-192 62.48 1.04 1.04 100 170 <20 140 110 <10 210 40RL.H-193 63.73 1.25 1.25 100 280 <20 270 190 70 270 60RL.H-194 64.98 1.25 1.25 100 370 <20 150 180 <10 250 60RL.H-195 66.23 1.25 1.25 100 360 <20 200 240 <10 280 70

ZK11meta-

andesite with Py

03 10070.3670.3686.8716.51

第 16 页，共 19 页

From To From To

Drill Log of Hole #RLP-11-11

Hole No. No. Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery factor（%）

Description

Sample log Assay Results

Sample No.

Location (m) Length（m）

Length of core （m）

Recovery factor（%）

Cuppm

Pbppm

Znppm

Crppm

Coppm

Nippm

Moppm

Auppb

Agg/t

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-196 67.38 1.15 1.15 100 920 <20 210 370 <10 260 90RL.H-197 68.58 1.20 1.20 100 1210 <20 320 390 <10 8 0.9 260 140RL.H-199 69.78 1.20 1.20 100 1310 <20 210 380 <10 290 90RL.H-200 70.83 1.05 1.05 100 390 <20 120 160 <10 210 60RL.H-201 72.75 1.92 1.92 100 20 <20 10 <10 <10 20 <10RL.H-202 74.00 1.25 1.25 100 70 <20 130 120 <10 220 40RL.H-203 75.20 1.20 1.20 100 510 <20 190 530 20 10 0.3 100 110RL.H-204 76.40 1.20 1.20 100 290 <20 530 420 <10 670 140RL.H-205 77.72 1.32 1.32 100 1420 <20 290 340 <10 9 0.7 210 60RL.H-206 78.92 1.20 1.20 100 280 <20 210 190 <10 240 100RL.H-207 80.17 1.25 1.25 100 180 <20 460 260 <10 240 100RL.H-208 81.42 1.25 1.25 100 60 <20 170 180 <10 200 30RL.H-210 82.62 1.20 1.20 100 190 <20 220 210 <10 220 40RL.H-211 83.82 1.20 1.20 100 180 <20 1210 220 10 15 0.3 70 100RL.H-212 84.82 1.00 1.00 100 210 <20 380 160 10 40 70RL.H-213 85.82 1.00 1.00 100 150 <20 390 150 10 60 30RL.H-214 86.87 1.05 1.05 100 210 <20 100 190 <10 60 20RL.H-215 88.02 1.15 1.15 100 30 <20 40 10 <10 30 <10RL.H-216 89.32 1.30 1.30 100 30 <20 10 <10 <10 20 <10

ZK11 05 K-feldspar granite 90.73 117.35 26.07 26.62 98 Light flesh red, main mineral composition are K-feldspar,quatz and biotite.

93.80-94.30m、107.60-108.90m、110.85-111.20m,potassium alteration.

04ZK11 3.8690.7386.87meta-andesite

Grey green-grey,development of the chlorite,epidotization and siliconization. 88.02-89.32m,grey white, felsic volcanics.1003.86

第 17 页，共 19 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 636708.874 East: Original Units: M North: North: 5445441.67 North: Storage: Markham Elevation: Elevation: 511.544 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

TypeFF

Page 11 of 12

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK12

Diamond Drill Hole Report Project Number:

Drilling Casing Location OtherAzimuth: 110 Length: 2.95 meters Township: UPPER SCOTCH LAKE AREA Contractor: TOPRANKDip: -55 Pulled: No Claim No: 4252235 Spotted by: ShawnLength: 105.16 meters Capped: Yes NTS: Coord Type: Started: 27-March-11 Cemented: No Surveyed Date: Completed: 29-March-11 Logged by: ShawnLogged: 30-March-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:

Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: Yes

Deviation TestsDistance(m)

Geophysics: Target: VETM anomaly supported by Geotech reportComments: The drill hole intersected a 0.4 metre interval of metasediment or shear zone from 61.52 to 61.92 metres containing 20-30% py/po as disseminations/laminations within mafic metavolcanic sequence.

16-Nov-12

Azimuth44.20 114.583.82 116.8

10B

From To From To

ZK12 01 Overburden 0 2.95 0 2.95 100 Overburden\casing.

RL.H-217 4.57 5.85 1.28 1.25 98 100 <20 110 40 <10 40 50

RL.H-218 46.64 48.04 1.40 1.40 100 160 <20 110 100 <10 200 40

RL.H-219 60.52 61.52 1.00 1.00 100 100 <20 100 140 <10 300 50

ZK12 03meta-

andesite with Py and Po

61.52 61.92 0.40 0.40 100

Gray - gray green,fine-grained texture and massive structure, mineral composition mainly amphibole, albite and a small amount of quartz and biotite.Rock development pyritization, pyrrhotite, showed a fine hypautomorphic -xenomorphic, a concentrated veinlets distribution, local arranged in mass, pyrite and pyrrhotite content quite, each account for about 15% of the overall content of about 30%, sulfide.

RL.H-221 61.92 0.40 0.40 100 630 <20 110 190 20 7 1.1 390 90

RL.H-222 63.18 1.26 1.26 100 130 <20 140 250 <10 180 70RL.H-223 64.48 1.30 1.30 100 90 <20 160 170 <10 310 60RL.H-224 66.13 1.65 1.65 100 140 <20 90 110 <10 200 40RL.H-225 67.33 1.20 1.20 100 40 <20 40 90 10 <5 <0.3 120 20RL.H-226 68.58 1.25 1.25 100 120 <20 170 80 <10 50 30

Grey - dark green, fine-grained texture and massive structure,mineral composition mainly amphibole, albite and a small amount of quartz and biotite. Rock development chloritization epidotization, quartz veins and calcite veinlets, occasionally pyrite, content < 1%;66.13-72.83m, rock was gray, cryptocrystalline structure, development is strong silicification, occasionally sulfide, content < 1%;82.32-86.00m, rock is fine, with more black mica, mica particles visible black;99.36-101.81m, rock is fine, with more black mica.

10043.2443.24105.1661.9204

58.5061.522.95meta-andesite

ZK12

02ZK12

meta-andesite

Drill Log of Hole #RLP-11-12

Hole No. No. Rock/Ore

type

Depth（m） Thickness

（m）

Length of core （m）

Recovery factor（%）

Description

Sample log

Grey to dark-green,fine-grained texture and massive structure,main mineral composition are Hornblende, feldspar and small amounts of quartz and biotite.Rock development chloritization epidotization and silicification. Generally see vein quartz and calcite veinlets, pulse width of about 0.1-5.0cm, more irregular shape distribution;more quartz veinlets than calcite veinlets, quartz veins occasionally a small amount of pyrite and pyrrhotite.The core is in a short column ( < 0.5m ) - long column, development of two groups of joints, 40 tocore axis and 60 to core axis..The rock I see pyrite were mainly scattered, fine shape distribution, also see a few scattered magnetic pyrite, sulfur content < 1%;2.95-7.01m, rock shows fine structure; pyrite films can be see at 4.70m rock joints ,width about 1.5cm quartz vein at 3.7m, the distribution amount of pyrite and pyrrhotite.7.01-10.87m,almond structure , almond body mainly calcite and quartz;46.64-47.74m,pore structure and pyrite drain hole, see a little pyrite distribution, content of about 1%.

10058.57

Sample No.

Location (m) Length（m）

Length of core （m）

Recovery factor（%）

Cuppm

Coppm

Nippm

Moppm

Auppb

Agg/t

Assay Results

Pbppm

Znppm

Crppm

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

第 18 页，共 19 页

Project: RICHARDSON LAKE

Surface Hole: Yes Level:

Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 635309.305 East: Original Units: M North: North: 5443119.607 North: Storage: Markham Elevation: Elevation: 564.416 Elevation:

UTM Zone: NAD 15,ZONE Grid Name:

TypeFFF

Page 12 of 12

CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK13

Diamond Drill Hole Report Project Number:

Drilling Casing Location OtherAzimuth: 150 Length: 1.20 meters Township: UPPER SCOTCH LAKE AREA Contractor: TOPRANKDip: -45 Pulled: No Claim No: 4252237 Spotted by: ShawnLength: 147.52 meters Capped: Yes NTS: Coord Type: Started: 1-April-11 Cemented: No Surveyed Date: Completed: 3-April-11 Logged by: ShawnLogged: 4-April-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:

Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:

Target: VETM anomaly supported by Geotech reportComments:The hole intersected approximately 71 metres of mafic metavolcanic before intersecting approximately 76 metres of relatively unaltered and un-deformed weakly to moderately magnetic diorite .

Deviation TestsDistance(m)

16-Nov-12

Azimuth45.72 149.591.44 155

138.38 160.3

11B

From To From To

ZK11 01 Overburden 0.00 1.22 0.00 1.22 100 Overburden\casing.

RL.H-271 6.62 7.75 1.13 1.13 100 210 <20 60 130 <10 240 40

RL.H-272 8.80 1.05 1.05 100 290 <20 70 140 <10 250 50

RL.H-273 9.90 1.10 1.10 100 3010 <20 70 130 <10 260 50

RL.H-274 10.76 0.86 0.86 100 1330 <20 60 220 <10 95 2.1 210 180

RL.H-324 104.85 105.95 1.10 1.10 100 300 <20 50 140 <10 <10 <5 230 50

RL.H-325 107.25 1.30 1.30 100 290 <20 60 190 <10 <10 <5 300 70

RL.H-278 123.14 124.14 1.00 1.00 100 70 <20 80 70 <10 <10 6 90 40

Drill Log of Hole #RLP-11-13

Dark grey to black，medium-coarse grained,massive structure,main mineral composition are pyroxene and feldspar,the content of them are almost same.Fine-grained pyrite are occasional to find. 88.91-89.36m，quartz vein.

119 29-120 79m white quartz vein

Ptppb

Pdppb

147.52 56.61 56.61 100

Grey to grey-green,fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and silicification. The rock developed Py,Po and Clp,occur as ubhedral to xenomorphic granular aggregates,Py=3%，Po=5%，Clp=2%； 8.90m,Clp vein,the width is 4mm,the length is 7cm. 10.06m,more Clp,Po=10%,Clp=10%.

90.91 80.15

ZK11 05 gabbro 90.91

ZK11 04meta-

andesite10.76 80.15 100

Grey to grey-green,fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and silicification. Po is occasional to find,the content is < 1%. One group joint,45°to core axis.The core length are <0.5m. Calcite and quartz veins are common,the width is about 0.1-5cm. 47.50-49.80m、70.00-71.32m，the core are broken。

ZK11

ZK11 1001.961.9610.768.80

Grey to grey-green,fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and silicification. Calcite and quartz veins are common,the width is about 0.1-4cm. Pyrite is occasional to find,the content is about 1%.The core are broken,the length of the core are <0.4m.

1007.587.58

meta-andesite

with Py,Po and Clp

03

8.801.22meta-

andesite02

Thickness

（m）

Length of core （m）

Recovery

factor（%）

DescriptionHole No.

No.Rock/Ore

type

Depth（m）

Sample log Assay Results

Sample No.

Location (m)Length（m）

Length of

core （m）

Recovery

factor（%）

Cuppm

Pbppm

Znppm

Crppm

Coppm

Nippm

Moppm

Auppb

Agg/t

正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M

RL.H-279 125.14 1.00 1.00 100 80 <20 80 70 <10 <10 <5 100 40

119.29 120.79m,white quartz vein. 135.63-135.90m,quartz vein.

第 19 页，共 19 页

LEGEND

ARCHEAN

• Van Nostrand Stock Cornpos11l0D

14a Granite 14b Granodiorite J4c Mmronite

Features 14f Medium grained 14h lnequigranular 14j Biotite 14k Hornblende 14n Potassimn feldspar

phenocrysts

~Norway Lake Pluton ~Composition

13a Granite 13b Granodiorite 13c Tonalite !3d Mmronite 13e Quartz mmzonite 13f Diorite 13gMmmdiorite 13h Quartz diorite 13j Syenite Features 13k Pegmatitic 13mlll:e 13n Medium grained 13p Coan!e grained 13q Equigranular 13r Inequigranular 13s Biotite 13t Hornblende 13u Potassium feldspar phyric 13v Amphihclite xenoliths

Intrusive Mafic to Ultramafic Rocks OJmposition 9a Gabbro 9b Melanogabbro 9c Peridotite 9d Pyroxenite 9e Homblendite Features 9f Magnetite 9g Asbestos 9h Plagioclase phyric 9j Talcose 9k Actinolite 9m Serpentine

~ Synvolcanic Intrusive L____"_____j Mafic Rocks

Composition Sa Gabbro

• Chemical Meta­sedilrentary Rocks Sa Chert 5b Ferruginous chert 5c Oxide facies ironstone

(magnetite bearing) Sd Sulfide facies ironstone

(pyrite ± pyrrhotite bearing)

5e Silicate facies ironstone Sf Oastic ironstone

~ Oastic Meta­~ sedimentary Rocks

lithofacies 4a Slate, argillite 4b Mudstone 4c lithic wacke 4d lithic arenite 4e Quartz arenite 4f Polymictic conglorrnrate.

matrix supported 4g Polymictic conglomerate,

clast supported Features 4h Graded 4j l1llninated 4k Schistose 4m Gamet porphyroblasts 4n Chert

~Intermediate and Felsic L_____:'_____j Metavolcanic Rocks

Pyroclastic Deposits 3a Tuff Features 3f Quartz phyric

D Mafic Metavolcanic Rocks Lithofacies of Flows 2a Massive flows 2b PillOIWd flow.; 2c Autobreccia,

flow-top breccia, hyaloclastite breccia

2d Coan;e-grained flow 1o synvolcanic gabbroic

dikes and sillsd Pyroclastic Deposits 2e Tuff 2f Lapilli tuff Features 2g Dikes 2h Magnetite 2j Plagioclase phyric 2k Variolitic 2m Gamet porphyroblasts 2n Amygdaloidal 2p Schistose 2q Vesicular 2r Amphihclite 2s Hyaloclastite

• Ultramafic Meta­volcanic Rocks lithofacies of Flows la Massive flows 1 b Autobreccia, flow-top

breccia Pyroclastic Deposits

Features I d Spinifex textured

/ /

/

/ /

/

I

I

I

I

I

-<--@ I

RLP- 11 c::09 1 ~-~ -1

I

I

~ 4252234 50

D

SYMBOL

C2JRoad

1/~//1 Geologic boundary

~ Small bedrock ~exposure

I / / /I Fault, interpreted

1/l Strike and dip l___"_"'_J of schistosity

~ Pillov.ed flow, ~ facing knomWnknown

~ Volcanic bedding ~ facing known/unknown

0 Foliation, inclined

[1:2] Property boundary

I ~~-09 1 Location of DDH

RLP-11 -01

10m

20

30

40

50

60

70

80

90

100

110

120

130

140

150

160

Cu

o ~ N

00 00 00

Zn

0 "' 0 0

A I

IS) 1\.) .t:>. (J) 0 (Jl 0 (Jl 0 0 0 0 0 0 0 0

Ba

ON .l::>. G:lQ:I --"--" g........o...p.VJ .t::r. OlG:l-..JCXD Ol --"--" N ON.t:>.aJDOOOOOO 0 0 Ol 0

00000000 0 0 0 0 "'

OOl --" --"NNVJC OOOlOOlO C

00000(

480

470

460

450

440

430

420

410

400

STRIP LOG: RLP-11-01 Easting

633683.0

STRIP

Northing 5438207.2

RL 497.1

Azimuth 90.0

Dip -45.0

Depth 163.7

1 Rock_code PAT LABEL DESCRIPTION

And meta-andesite Bas-S Pyrrhotite meta-basalt IF Iron Formation Lamp lamprophyre Ovb Overburden

CME Corp. Richardson Lake Project

RLP-11-02

10m

20

30

40

50

60

70

80

90

100

110

120

ON 0

Ag Cu

o~

0 0 0

Zn AI Ba Ca Cr Co

o<n~

00 0

Fe K Sc Sr

0 (Jl ~

Ti v

OOl---"---"NNW OOOlOOlO

00000

RL

500

495

490

485

480

475

470

465

460

455

450

445

440

435

430

425

420

STRIP LOG: RLP-11-02 Easting

633404.6 Northing

5438233.9

STRIP

1 Rock_code

RL 501.7

PAT

Azimuth 70.0

LABEL

And Lamp Ovb

CME Corp.

Dip -45.0

Depth 123.4

DESCRIPTION

meta-andesite lamprophyre Overburden

Richardson Lake Project

RLP-11 -03

10m

20

30

40

50

60

70

80

90

100

110

120

130

140

150

Ag Cu

o~N

00 00 00

Zn A I Ba Ca Cr Co

0 N .t:>. G:l CO --" --" 0--"NW .l::>. OlG:l-.JOD Ol --" --" 0 f\.) 00000000 0 0 (Jl

00000000 0 0

OOl --"--" NNW OOOlOOlO

00000

STRIP LOG: RLP-11-03 Easting

633025.5 Northing

5438170.0

STRIP

1 Rock_code

RL 510.1

PAT

Azimuth 60.0

Dip -55.0

Depth 150.9

LABEL DESCRIPTION

And And-S

IF Lamp Ovb

meta-andesite meta-andesite with pyrrhotite and pyrite Iron Formation lamprophyre Overburden

CME Corp. Richardson Lake Project

STRIP LOG: RLP-11-04 Easting Northing RL Azimuth Dip Depth

635010.4 5440603.5 540.2 250.0 -60.0 177.4 RLP-11 -04 Ag Cu Zn AI Ba Ca Cr Co Fe K Mg Sc Sr Ti v

STRIP

1 Rock_code PAT LABEL DESCRIPTION 10m

530 And meta-andesite Gran2 granite

20 Ovb Overburden

520 QV-Sil quartz vein and stong silicification

30 meta-andesite

510

40

500

50

60 490

70 480

80 470

90

460

100

450

110

440 120

130

140 420

150

410

160

400

170

390

00 --"--" f\Jf\.)VJ G)~ =><>a) 0 --" NVJ .J::>. OlG:I-..Jm~N ON .t:>. G:ICO --" 0 --" NVJ .l::>. OlG:l-....JCXIJ!DOl --" 0 "' c; ~ NOO --"--" N 0 --" N VJ .t:>. OlCIJ:l c; "' 0J Q::>. F\.X.Jl .l::>. (J) 0 0 0 0 0 .....~Q-45~ --"--" 1'\JNVJ C

"' "' "' "'008 000 00 0 0000000000 0 0 "' "' 0 0 ocooo rv :.::.. meo f.SlOOlOOlO C 000 00 000000000 0 0 0 00000(

000

CME Corp. Richardson Lake Project

RLP-11 -06

10m

20

30

40

50

60

70

80

90

100

110

120

130

140

ON_,. =

Ag Cu Zn

~ = = = 0 --" NVJ .J::>. OlG:I-..JmCDN .t:>. (J) ())Q--P>..) .I» (J)....€0 --"--"9 N

0 0 0 0 0 N .t:>. ON .t:>. 0 0000000 0

0 0 0

v RL

510

500

490

480

470

460

450

440

430

420

410

STRIP LOG: RLP-11-06 Easting Northing RL Azimuth Dip Depth

634089.3 5440803.8 510.6 90.0 -60.0 141.7

STRIP

1 Rock_code PAT LABEL DESCRIPTION

And meta-andesite And-S meta-andesite with

pyrrhotite and pyrite - Gran K-feldspar granite (1:1~4',\"l HDS-MS heavily disseminated

to massive sulfide MS-HDS massive to heavily

disseminated sulfide - Ovb Overburden

CME Corp. Richardson Lake Project

RLP-11 -07

10m

20

30

40

50

60

70

80

90

100

110

120

ON 0

Ag Cu

o ~

0 0 0

Zn A I Ba Ca Cr

0 --" 1\JW .l::>. Ol 00000 00000

Co

o<n ~

00 0

STRIP LOG: RLP-11-07 Easting Northing RL Azimuth Dip Depth

634713.4 5441172.1 507.7 55.0 -50.0 124.1

STRIP

1 Rock_code PAT LABEL DESCRIPTION

And meta-andesite And-S meta-andesite with

pyrrhotite and pyrite - Ovb Overburden

CME Corp. Richardson Lake Project

STRIP LOG: RLP-11-08 Easting Northing RL Azimuth Dip Depth

634409.0 5441157.4 511.5 65.0 -55.0 150.9 RLP-11 -08 Ag Cu Zn AI Ba Ca Cr Co Fe K Mg Sc Sr Ti v RL __ __, __ __, --

510 STRIP

1 Rock_code PAT LABEL DESCRIPTION 10m

And meta-andesite 500 Gran K-feldspar granite

20 ---f---- f---- Ovb Overburden

490

30 --- --- --

40 480

50 470

60

460

70 --- --- --

450

80

90 440

100 --- -----

430

110

420

120

410 130 --------

140 400

150

0 "' ON 0 --" NVJ .l::>. OlG:I-..Jmt;eN ON .l::>. G:IC:0 --"--" 0 "' ..,. o<n~

0 "' --" --" NOO --" 0--"NW .l::>. OOl --"--"NNW~ 0 0 0 0 0 --'OOl --"--" f\Jf\.)(JJ ( 0 0 00 ON 0 0 00 0"' 0 "' OOlOOlOOlaill1IO N ~ G:IO:l OOOlOOlO C 0 0 00 0 0 0 00 00000( 0

CME Corp. Richardson Lake Project

RLP-11 -09

10m

20

30

40

50

60

70

80

90

100

110

120

130

ON-" 00

Ag Cu

00--" --" NNW G> --" (.n(n(.n(n8

0

Zn

0 "' 0 0

A I Ba Ca Cr

ISJ--" NVJ4>il0lm-..Jm--"rvw OOlOOlO 000 00000 000 0 0 0 0 0

Co

o<n~

00 0

Fe K

0 .t:>. anJl --"--" NNW~W.t:>. OOlOOlOOlailltDOO

0000

Ti v RL

500

490

480

470

460

450

440

430

420

410

400

390

STRIP LOG: RLP-11-09 Easting Northing RL Azimuth Dip Depth

634321.7 5443331.7 502.9 270.0 -65.0 133.2

STRIP

1 Rock_code PAT LABEL DESCRIPTION

And meta-andesite And-S meta-andesite with

pyrrhotite and pyrite Gran K-feldspar granite Ovb Overburden

CME Corp. Richardson Lake Project

RLP-11-10

10m

20

30

40

50

60

70

80

90

100

110

120

ON-" 00

Ag Cu Zn AI Ba --v---v---

L

I I I I I I I I I I I O --" NW.t::r.Olm-..Jmc;gf\JW.t::.

o=o o=o

OOl --"--" Nf\DOl OOOlOOl

0000

Sc Sr Ti v RL

STRIP LOG: RLP-11-10 Easting

636738.9 Northing

5445230.6 RL

514.4 Azimuth

110.0 Dip

-55.0 Depth 123.4

STRIP

1 Rock_code PAT LABEL DESCRIPTION

And meta-andesite And-S meta-andesite with

pyrrhotite and pyrite FV felsic volcanics Gran K-feldspar granite MS massive sulfide Ovb Overburden

CME Corp. Richardson Lake Project

RLP-11-11

10m

20

30

40

50

60

70

80

90

100

110

ON 0

Ag Cu

o ~ rv

00 00 00

Zn

~ = == = 0 --" NW.l::>.UlG:I-..Jm~NW .l::>.UlG:I

000000 000000

0 "'

505

500

495

490

485

480

475

470

465

460

455

450

445

440

435

430

425

420

~ ~ ~~~ ~ N ~ UD --" N W ~ Ul~~~~~~88§§8§8~ ~ ~ ~ 0

STRIP LOG: RLP-11-11 Easting

636874.0

STRIP

Northing 5445451.4

1 Rock_code

RL 507.7

PAT

Azimuth 120.0

LABEL

And And-S

Gran Ovb

Dip -50.0

Depth 117.3

DESCRIPTION

meta-andesite meta-andesite with pyrrhotite and pyrite K-feldspar granite Overburden

CME Corp. Richardson Lake Project

STRIP LOG: RLP-11-12 Easting Northing RL Azimuth Dip Depth

636708.9 5445441.7 511.5 110.0 -55.0 105.2 RLP-11-12 Au Ag Cu Zn AI Ba Ca Cr Co Fe K

510 STRIP

505 1 Rock_code PAT LABEL DESCRIPTION 10m

And meta-andesite 500 And-S meta-andesite with

20 495 pyrrhotite and pyrite - Ovb Overburden

490

30 485

480 40

475

50 470

465

60 460

455 70

450

80 445

440

90 435

430 100

425

ON 09--":-" o~ ON o __.. N w .t:>. Ol m -..J mc;ervw.t:>.Olm-..J ON.l::>.G:lQ:I--" 0--"NVJ.t:>. o<n~ 0 "' ;::; ~ NOO--"--"N 0 --" N W .t:>. OlanJl--"--"NNWUCJ::>..t>J ..,. Ol CXCl-@ 9 0 0 --'OOl--"--"NN VJC

0

"' "' 0 0 0000000 0 0000 00 0 "' "' 00l00l00l0(l1D 0 0

:5 :!9 ~"'"' OOOlOOlO C

0 0 0000000 0000 0 0 0 0 00000( 0 0 0

CME Corp. Richardson Lake Project

RLP-11-13 Ag Cu Zn

10m

20

30

40

50

60

70

80

90

100

110

120

130

140

0--"NVJ .l::>. 0\J 0 0 0 0 0 0 0 0 0 0 0000

AI Ba Ca

0 --" 1\JW .l::>. OlG:I-..Jmc;gJ>..:KJJ.t>.OlG:I-..JO:lO 1"0 .t:>. G:l CO --" 00000000 0 00000000

Cr

.t:>. CIJlJl --" --"NNVJUQ::>..to.X.Jl .t:>. G:l 00l00l00l0(11l00 0

0 0 0

550

545

540

535

530

525

520

51 5

510

505

500

495

490

485

480

475

470

STRIP LOG: RLP-11-13 Easting Northing RL Azimuth Dip Depth

635309.3 5443119.6 564.4 150.0 -45.0 147.5

STRIP

1 Rock_code PAT LABEL DESCRIPTION

And meta-andesite And-S meta-andesite with

pyrrhotite and pyrite Gab gabbro Ovb Overburden

CME Corp. Richardson Lake Project