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0102.9546

RECONNAISSANCE GEOPHYSICAL SURVEYS VINCENT TOWNSHIP-CLAIMS #8^5986-84-5990 CAYUGA SYNDICATE

-1-

I INTRODUCTION; The following pages are a concise attempt to

present the results of Geophysical surveys completed on Claims

#845986 to #845990 inclusive,within Vincent Township. Included

here is the location and present holders of the property,instruments

used,with a brief explaination of field procedures,previous surveys

done on the property,and finally an interpretation of the results.

Also enclosed with this report are seperate profiles of each

line,as well as a complete map of each survey.

-2-

HOLDERS of CLAIMS; The, report presented here was written by

the technical personal of the Cayuga Syndicate,which is

headquartered at 360 Main St. ,V/innipeg,Manitoba. This organization

are the present holders of this property.

LOCATION: The claims surveyed are located in the north-east

sector of Vincent Township(NTS Map 42E12) and are registered as

#8/15986 to #845990 respectively,within the Thunder Bay Mining

District(Fig.l). The claims are accessible by way of Highway #11 and

various foot trails.

EQUIPMENT and PROCEDURE; The geophysical methods used on

these claims were of the reconnaissance type,that is ground based

magnetometer and VLF-EM. The surveys were conducted between June

and August 1986.

The instruments used were a Geometrics portable proton

magnetometer,model G-8l6 and a Geonics EM16 VLF-EM system.

Specifications for both instruments are given in figures 2 and 3.

A Geometrics G-856B portable magnetometer was used as a magnetic

base station.

As this report is concerned basically with recording data

for assessment purposes,no attempt will be made to probe the

theoretical aspects of the Magnetic or Electromagnetic methodology

or equipment design. A list of suitable references is supplied to

the reader wishing to pursue this line of thought.

A brief procedure used in these surveys is as follows.

For the magnetic survey,the first step is to get the base station

functioning. The base station is necessary to correct for diurnal

and micropulsation time variations. The base station is tuned in

order to acquire the best magnetic signal. This magnetic base was

-3-

found to be 60300 Gammas. The sychronization of the base clock

with the operators field clock and a time interval for readings

is then established. This interval was 60 seconds. Finally the

Auto switch is activated and the diurnal station monitor is

operational. The operator then proceeds down the line,takes and

records a reading at the station to the nearest minute. The

stations are at 25 meter intervals along north-south trending

lines,which are 100 meters apart. The total number of stations

for all five claims is 331.

The VLF-EM survey is performed by first orientating the

instrument perpendicular to the survey line in order to establish

a transmitting station for the best coupling effect. In this case

the transmitter is NAA originating from Cutler,Maine at a

frequency of 2^.0 kHz. The transmitter direction is determined

when the sound intensity is at a minimum. The next move is to

orientate the reference coil along magnetic lines,by slowly

moving the instrument back and forth until minimum sound intensity

and adjust the Out of Phase(Quadrature) component dial to further

minimize the sound. Read and record the number on the inclinometer

and the Out of Phase component dial. The operator must always face

north or in the case of north-south trending strike,one must face

west. This is necessary in order for the polarities to remain

constant through every line.

PREVIOUS WORK: As far as can be ascertained no published

evidence is available of prior work executed on these particular

claims. In the field however,there is evidence that some trenching

was done some time ago.

-i).-

I INTERPRETATION; The magnetic profiles (Fig. 4-2?) indicate

in general,a low magnetic response. There are points which show

major peaks both high and low. The magnetic anomalies that are

present imply that the structure causing them,is narrow and steeply

dipping. The structure seems to trend along strike,that is in a

east-west direction and is located,in general between lines 0+00

and 18+00 West,covering a width of 100 meters,from stations 0+00

to 1+00 South. There is a southern magnetic anomaly located between

stations 4+00 and 5+00 South,along lines 18+00 to 23+00 West. The

magnetic anomalies do not correspond exactly to the VLF conductors

noted below,but they are adjacent and thus they are most likly the

result of the same geological structure.

The VLF survey shows two conductive bodies trending

roughly in a east-west direction. The northern response is found

from line 0+00 and trends north-westerly to line 18+00 West and

probably continues further beyond the boundary of these claims in

the same general direction. This conductor seems to weaken toward

the eastern portion of the property.

The southern conductor is found between lines 14+00

and 23+00 West (Fig.28-43). It trends in a east-west direction and

most likly continues further east. The two conductors are

approximately 200 meters apart. These conductors are very similar

in response,in that both the Inphase and Out Phase components show

in general,a complementary repetative pattern through all lines. The

profiles also suggest that the dip of the southern conducting

structure is relatively steep and to the north. The response

signal is in general of moderate strength and sharp,hinting at a

shallow structure in depth. The northern conductor has relatively

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physical characteristics as the southern response,implying

that both conductors are the result of parallel geologic features.

From the geological evidence,there seems to be,contained

within the volcanic flows a thin belt of Iron Formation. This zone

is observable at random locations on surface between line 10+00 and

17+00 West and approximatly between stations 50 to 100 South. This

formation contains some sulphides but its magnetic susceptibility

is low. A few meters south of these exposures is found,again at

random shear zones containing up to 53d pyrite. These shear zones

are in line with an apparent topographic lineament. Both of these

structures may account for the geophysical responses encountered

on the northern portion of these claims. Therefore a possible fault

structure trending in general in a east-west direction maybe

contained within this property.

The southern conductor is not quite as obvious. Some

Carbonized Iron rich rock was observed near station J++00 South on

line 16+00 West. This may have some strike length to it. There are

also many intrusive rocks within this southern region,and the

anomaly may be a result of a lithological change.

CONCLUSIONS; The anomalous zones within these claims

will be explored in more detail in up coming field seasons. This

v/ill involve trenching and X-ray drilling. It seems however that

a major concentration of economic minerals is not likly in this

type of environment,as the large discoveries seem to occur in

general near volcanic-sedimentary contacts. This property is near

some major showings and it is for this reason that it v/ill also be

examined in future exploration programs.

Respectively Submitted

2M

4w4^^^^ * G^V^VmS' i

Scale: l cm. s 7.84 M.(A) .s 13.7 km.,___________ ^"'^ J1 fX * j.......*""* \ J-^J1 ri r ___ __ __ JBJ.

showing position of Vincent Township J ~ Mining district and location of claims

[within, township. ^^—^^—————

Map within

(B)

Fig 2

SPECIFICATIONS

Sensitivity: 1 gamma throughout range

Range: 20,000 to 90,000 gammas (worldwide)

Tuning: Multi-position switch with signal amplitude indi cator light on display

Gradient Exceeds 300 gammas/ft (increased gradient to!- Tolerance: erance to 800 gammas/ft upon request)

Sampling Rate: Manual push-button, one reading each 6 seconds

Output: 5 digit numeric display with readout directly in gammas

Power Requirements:

Temperature Range:

Accuracy (Total Field):

Twelve self-contained 1.5 volt "O" cell, univer sally available flashlight-type batteries. Charge state or replacement signified by flashing indi cator light on display.

Battery TypeAlkalinePremium Carbon ZincStandard Flashlight

Number of Readings over 10,000 over 4,000 over 1,500

NOTE: Battery life decreases with low temper ature operation.

Console and sensor: -40" to *850 C

Battery Pack: O" to *50"C (limited use to -15 0 C; lower tempera ture battery belt opera tion optional)

l gamma through O0 to *50"C temperature range

Sensor: High signal, noise cancelling, interchangeably mounted on separate staff or attached to carry ing harness

Size: Console: 3.5 x 7 x 10.5 inches (9 x 18 x 27 cm) Sensor: 4.5 x 6 inches (11 x 15 cm) Staff: l inch diameter x 8 tt lenght

(3 cm x 2.44 m)

Weight:Console (w/barteries): Sensor A signal cable: Aluminum staff:.

Lbs. 5,5 4

Total: 11.5

Kgs.2.41.80.9

TT

Fig 3

EM16 SPECIFICATIONS

MEASURED QUANTITY

SENSITIVITY

RESOLUTION

OUTPUT

OPERATING FREQUENCY

OPERATOR CONTROLS

POWER SUPPLY

DIMENSIONS

WEIGHT

In-phase and quad-phase components of vertical magnetic field as a percentage of horizontal primary field, (i.e. tangent of the tilt angle and ellipticity) .

In-phase : 150S; Quad-phase : 4(H

Nulling by audio tone. In-phase indication from mechanical inclino meter and quad-phase from a graduated dial.

15-25 kHz VLF Radio Band. Station selection done by means of plug-in units .

On/Off switch, battery test push button, station selector switch, audio volume control, quadrature dial, inclinometer.

6 disposable 'AA 1 cells.

42 x 14 x 9cm

Instrument: 1.6 kg Shipping : 4 . 5 kg

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Profiles VINCENT TOWNSHIP Glaims ^845986-8-^5990

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#845986-845990-

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LEGENDHorizontal Scale- loOcm= 50 Meters Vertical Scale - 1.Ocm* 200 Gammas Magnetic Base - 60300 Gammas

62600-

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63600-

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LEGENDHorizontal Scale- l.Ocm* 50 Meters Vertical Scale - l.Ocm^ 200 Gammas Magnetic Base - 60300 Gammas

62600-

62000

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61000

60600 .

60200-

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59000

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Maroetic ProfilesVINCENT TOWNSHIP claims #84598J^845990, ____________JEGENDHorizontal Scale- loOcn^ 50 Meters Vertical Scale - l.Ocm* 200 Gammas Magnetic Base - 60300 Gammas

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63600

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Mafmetic Profiles VINCENT TOWNSHIP Claims #845986-8^5990

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62600

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V.L.F. ProfilesVINCENT TOWNSHIP Claims #845986-90 LEGEND——————————

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REFERENCES

Anderson, E.O.I9?li VLF-EM Geophysical Method; Special Report.Cominco Ltd., 8p.

Beck,A.E.Physical Principals of Exploration Methods i Macmillan Press Ltd.}23&P.1981.

Breiner,S.I973i Applications Manual For Portable Magnetometers i

Geometrics,Sunnyvale,California. 58p.

Dobrin.M.B.I960i Geophysical Prospecting} Mcgraw-Hill ,New York, i(46p.

Fraser,D.C.19691 Contouring of VLF-EM Data? Geophysics, Volume 34,No. 6

P.958-967.

Grant,F.S..West,G.F.1965' Interpretation Theory in Applied Geophysics; McGraw-Hill,

New York.

Telford,W.M.,Geldart,L.P..Sheriff,R.E..Keys,D.A.1976i Applied Geophysics; Cambridge University Press; 860p.

Ward,S.H.,1967t The Electromagnetic Method,pp. 22^-372, in Mining Geophysics

Volume 2,eds. D.A. Hansen, R.E. MacDougall, G.R. Rogers, J.S. Sumner and S.H. Ward, Society of Exploration Geophysicists, Tulsa,Oklahoma.

CERTIFICATE

I, Brian Docherty.of 563 Ridge Road, Ridgeway,Ontario, do hereby certify as follows:

That my qualifications to write a report of this nature is a result of the following academic achievements and related professional experience.

1) I am a graduate of Geological Sciences from BrockUniversity at St. Catherines,Ontario, received in 1977. I have taken advanced cources (3rd year level) in Exploration Geophysics from the University of Western, London, Ontario*

2) I have been directly involvsd in all aspects ofExploration Geoscience,including diamond drill programs both surface and underground,as." acquired from full time employment with companies as Amok, Canada and Asamera Inc. I am also familiar and experienced with various Geophysical and Geochemical systems and the interpretation of their results.

3) I have a direct relationship with the regions ofinterest, and will be directly involved in all aspects of its' exploration and future development. That this report is the result of extensive evaluation and synthesis of published geological and geophysical reports,considerable field work and the expertise acquired throughout the past years by the author.

Dated at Ridgeway, Ontario, this 12th day of November, 198b.

Brian Docherty, B.Se.

\

CORRECTED MAGNETIC VALUES IN GAMMAS VINCENT TOWNSHIP -CLAIMS NO. 845986-845990

LINE NO. 23 W.

STATION-SOUTH

0255075j. 001251 50.1. 7520022525027530032535037540042545047550 C'525550575600

61265606376062160847605736053160389604 0 1603736070160447605376053560493604296094 i603156200460803606076075660603606986065561479

CORRECTED MAGNETVINCENT TOWNSHIP

LINE NO. 1 7 w.

22 W.

6079760558603816O4456035960414604826053060568605206039860442602366049160141604836082360543605816059060407607606057900

1C VALUES IN-CLAIMS MO.

16 W.

21 W.

6090560484604256O386603876040260343604066054360506604256052660265605596063560697606446O81460883608196035160807000

GAMMAS845986

15 W

"""""""20" w.

6055260356603796053460105601666017660185603666024760141600736005460008601736023960291602086193660065602660000

-845990

14 W.

19 W.

"~~6Ql31~~"~~

603196034660404604296028560238602676024660328602246019760268602846101560972613816092860601000000

13 W.

STATION-SOUTH

025507510012515017520022525027530032535O375400425450

6 1 5 1 860335602866031360439604056023960405604646048160396603126045460489

......... 5904360133605816027960825

6050360686606456041260470603326031660594605546009360056603576045560344606066017360222603850

606246134459991603306041360268602766036760399603656049660336603656005360184600346036200

60656606296115462782604506028960523604 1 3603576030O6049060455605076064161336607596O84600

6057260476610326068560033603376070200607466139300O00o00

IS

618686040260482604686035160352603176036260397604206O475603226O315603716038160595603206046661006OOOOOO

12 W.

606486080860274603566038561295OOO603116029960427OOOOo o o

CORRECTED MAGNETIC VALUES IN GAMMAS VINCENT TOWNSHIP1 -CLAIMS NO. 845986--845990

LINE; NO,, 1 1 w. 10 W. 9 W.""""""""""i ""w.

7 W. 6 W.

STATION-SOUTH

02550751 001251 50175200225250

614746097260630589050000598386025160430

CORRECTED MAGNETVINCENT TOWNSHIP

LINE NO,, 5 W.

606.1.1605056079860798598370060325605 1 16041060297

1C VALUES IN•••••CLAIMS NO.

4 W.

606786052060829610116053100605176060 16032960267

GAMMAS

610216089660798611116051760895605666038860336603590

60553604266141860939605316067160672604 1 56079700

613966052260531606086.1.94760512604366075660518606080

845986-845990

3 W. 2 W. 1 W. 0

STATION-SOUTH

02550751 001251 50175200

6066560677604026039160281603816064960523604.1.6

603796105260467604776067260162606376045960428

610306135860800605696099.1.61372587756047960568

606496101560666603666202161697602506097260546

60883615706073560295609336057160230608276O464

60284614326040461120611526O68360576608436O638

BOIL SAMPLE LOCATIONS VINCENT TOWNSHIP-CLAIMS NO. 845986-845990

LINE NO.23 W. 22 W. 21 20 W. 19 W. 18 W. 17 W.

0+00

04-25

0-1-50

0+75

l 4-00

1+25

1+50

1+75

2+00

2+25

2+50

2+75

3+00

3+25

3+50

3+75

4+00

4+25

4+50

4+75

5+00

5+25

5+50

6+OO

VS-120 VB-93

VS-138 VS-130 VS-121 VS-113VS-101

VS-139 VS--131 VS-122

VS-107 VS--94

VS-114 VS-102

V8-10B VS-95

VS--132 VS-115 VS-103

VS--14Q VS-109 VS-96

VS-133 VS-123 VS--H6 VS-104

VS-141 VS-110

VS--134 VS--124 VS-117

V8-111 VS-105 VS-97

VB-137

VS-144

VS--125

VS-106 VS-98

VS-126 VS-112

VS-135 VS-127

VS-136 VS-128

VS-119

VS-129

VS-99

VS-i43 VS-118 VS-100

SOIL SAMPLE LOCATIONS VINCENT TOWNSHIP-CLAIMS NO. 845986-845990

LINE NO.16 W. 15 W. 14 W. 13 W. 12 W, 11 W. 10 W.

0+00

0+25VS-51

0+50

0+75v VS-53

1+00 VS~8

14-2!

1+50

1+75

2+OC

2+25

2+5C

2+75

3+OC

3+25

3+5C

3+7!

4+OC

VS-84 VS-71 VS-65 VS-60VS-55 VS-50

VS-72 VS-66 VS-61 VS-S6

VS-85 VS-73 VS-67 VS-62VS-57 VS-52

VS-74 VS-68 VS-62 VS-S8

VS-78 VS-75 V8-69VS-63 VS-59 VS-54

VS-76 VS-70 VS-64

VS-77

VS-88

VB-89 VS-80

VS-81

VS-90 VS-B2

MS-91

VS-92 VS-83

SOIL SAMPLE LOCATIONS VINCENT TOWNSHIP-CLAIMS NO. B45986-84599Q

LINE NO.

o+oo

0+25

0+50

0+75

1+00

1+25

1 +50

1+75

2+00

2+25

9 W. 8 W. 7 W. 6 W. S W. 4 W.

VS--46 VS-42

VS-37

VS-47 VB-43 VS-33 V8-27

VS-48 VS-44 VS-38 VS-34VB-28

VS-49 V8-29

VS-39

VS-30

VS-40 VS-35 VS-31

VS-45 VS-36 VS-32

VS-41

3 W.

VS-20

VS-21

VS-22

VS-23

V8-24

VS-25

VS-26

SOIL SAMPLE LOCATIONS VINCENT TOWNSHIP-CLAIMS NO. 845986-845990

LINE NO.2 W

0+00

0+25

0+50

0+75

1 +00

1+25

1 +50

1+75

2+00

VS-

VS-

VS--

VS-

VS-

VS-

m

14

15

16

17

18

19

1 W.

VS-7

VS-8

VS-9

VS-10

VS--11

VS-12

VS--13

0

VS-1

VS-2

VS-3

VS-4

VS--5

VS-6

42E12NEei87 2.9546 V INCENT 020

GEOLOGICAL SURVEY

Vincent Township Claim # TB 845986 - TB845990

inclusive Cayuga Syndicate

(1)PROPERTY EXPLORED:

PROPERTY OWNER:

PREVIOUS WORK:

DATE OF SURVEY:

GEOLOGICAL SURVEY PERFORMED AND INTERPRETED:

LOCATION AND ACCESS:

TOPOGRAPHY AND VEGETATION:

GLACIATION:

GEOLOGY

Vincent Township (claim numbers: TB845986,TB845990,TB845987,TB845988)

Cayuga Syndicate, 19-360 Main St., Winnipeg, Manitoba R3C 3Z3.

No publi shed material.

July 3 - 20, 1986.

J.A. Hyslop

The area of study is located in the north - east corner of Vincent Township, between Nezah and Clist Lakes. Access to property is by foot trail, (see figure 1).

These five and valley The vertic metres in general ea Outcrop is at least 7 area. The of spruce, aspen that particular segment of

claims exhibit a ridge type of topography,

al cliffs are up to 10 height and trend in a st - west alignment.plentiful and occupies

SI o f the total surface forest cover consists alder, cedar and final ly occurs in open parkland,

ly in the south - western the claim group.

Field observation of glacial strae, at location Line 16+50 West,station 225 South, indicates an east-west alignment of glacial movement. Boulder trains are present in the south-west portion of property, particularly west of Line 20+00 West.

(1) Lithology: The major rock type observed on the property are andesite flows with a slight variance to the andesitic -basalt composition in localized outcrops. These flow rocks range in colour from gray to medium green,however, the altered greener shades are more numerous. The grain size of these are generally aphanitic to fine grained.however, in the southwestern sector of the grid network starting at Line 15+00 West, medium to coarse grained rocks are more plentiful. Pillow salvages were observed with greatest frequency east along the cliff face starting at Line 5+00 West, station 125 South. These pollowed lavas tend to be more mafic in composition and therefore grade into a andesitic-basatlt.

2M

Scale:

—""

(A)

^ 7.8^ M.(A) ^ 15.7 km.(B

Map showing position of Vincent Township within Mining district and location of claims withih. township.

Bf

(B)

(3)

rare gray fine - grained felsic flow rock was noted at the southern end of Line 10+00 West. It is probably rhyodacitic in composition. Chemical sediments ate present, usually in thin beds sandwiched between the volcanic flows. The black.aphanitic shalls are restricted to a narrow stratigraphic horizons with no measurable strike length and random distributions.A more complex sequence of deep water sediments occurs as iron formation Alternating bands mainly of gray chert, beige sandstone, mudstone, graphite and magnetite {commonly altered to sulphides). Hematite and limonite were also present. This particular sedimentary sequence has a measurable strike length of at least 400 metres. The width does vary,however, it is the widest and most pronounced at station 75 South Line 13+00 West where quartz was later injected. The more recent intrusive rocks include both the medium grained diabase dikes and the more massive and coarser textured gabbroic rocks. These intrusives are restricted to the south-western segment of the grid. Some of these coarse grained intrusive rocks could actually be the centre of volcanic flows. The steplike joint pattern is a common characteristic of these intrusive rocks.

(2) Metamorphism: The volcanic flows and sediments have indergone regional metamorphism to the degree of greenschist facies. These moderately chloritized sequence of rocks (particularly the volcanics) have had their original depositional textures disturbed. This dis turbance has made field determinations of certain features rather difficult. For example, the pillowed lavas are frequently distorted thereby making top determinations impossible. These rocks, for the most part, have a good foliation, -trending approximately east-west. The dip of these rocks is steeply to the north.

{3) Structure: The only fold observed was that at the pit. {location Line 13+00 West station 75 South).Shearing is present on the north shore of the lake - in central grid. This shear is rather weak,however, strike length and width i s rather substanti al.Shearing was also observed at the southern ends of lines 15+00, 16+00 and 17+00 West. A higher percentage of iron - carbonate is present along with this shear zone.No major faulting was observed,however, due to the neighbouring sheared volcanics on the north shore of the lake and the alignment of the lake, a definite lineament does exist.

(4) Mineralization: There are a number of dis-continuous barren quartz veins of varying widths distributed randomly throughout the property,however, only one bears any significant sulphide mineralization. This quartz vein is seen cutting across both iron formation and the surrounding volcanics at location Line 13+00 West, station 75 South.

CERTIFICATE

I, John A. Hyslop, residing at R.R.#1 Cayuga, Ontario NOA 1EO do hereby certify that:

1. I am a graduate geologist, with a honours B.SC. degree from Brock University, St. Catherines, Ontario, received in 1977.

2. I have praticed my profession as an exploration geologist continuously for eight years.

3. This report is based on my personal field examination of the area .

Dated at Cayuga, Ontario, this 5th day of November, 1986.

42E12NE8187 2 .9546 V INCENT 030

RECONNAISSANCE GEOCHEMICAL SURVEY VINCENT TOWNSHIP- CLAIMS #8^5986-8^5990 CAYUGA SYNDICATE

-1-

INTRODUCTION; The following pages are a consise attempt

to present the results of Geochemical surveys completed on

Claims #8^5986 to #8if5990 inclusive within Vincent Township.

Included here is the location and present ownership of the

property,a brief explaination of field procedures,previous surveys

performed on the property,and finally an interpretation of the

results. Also enclosed with this report are seperate maps of

particular elements of interest as well as a copy of the

certificate of analysis.

-2-

HOLDERS of CLAIMS; The report presented here was conceived

by the technical personal of the Cayuga Syndicate,which is

headquartered at 360 Main St. Winnipeg,Manitoba. This organization

are the present holders of this property,

LOCATION; The claims surveyed are located in the north-east

sector of Vincent Township(NTS Map if2Ei2) and are registered as

#845986 to #8*1-5990 respectively,within the Thunder Bay Mining

District(Fig,i). The claims are accessible by way of Highway #11

and various foot trails.

PRO C IMPURE; A brief procedure used in this survey is as follows.

Soil samples were acquired from the B-Horizon by means of a

aluminium trowel,at 25 meter stations,along north-south trending

lines which are 100 meters apart. The total number of samples

gathered was 1^4. If the B-Horizon was not present samples were not

taken,except where a possible transition zone might -exist,for

example an intermediately positioned soil situated below the A-Horizon

would be sampled if the B-Horizon was absent. All characteristics

of the sample site were copiously recordered,including thickness,

colour and texture of each horizon,amount of organic material etc.

Each sample was placed in a thick paper bag,numbered(VS1-VS1it4) and

dried naturally. When these preparations were completed the samples

were sent to a commercial laboratory for analysis. In this case the

laboratory is Chemex Labs Limited of Vancouver B.C. At the laboratory

the samples were dried then sieved through -80 mesh screen,then put

through Nitric-Aqua-Regia digestion,followed by Inductively Coupled

Plasma analysis. Since this method of digestion is considered incomplete

16 of the 30 elements analysed for,the values can only be sited as

semi-quantitative.

-3-

PREVIOUS WORK; As far as can be ascertained,no published evidence is available of prior geochemical work being executed on these particular claims. In the field,however,there is evidence that some trenching was done some time ago. There is no recording of any analysis results from this trenching.

INTERPRETATION; The soil horizons within these claims is in general quite well developed. There are 3 major zonings with some sub-zones. The A,-horizon found in this area is a peat type of overburden containing moss,lichens and similar types of vegetable cover,it is black in colour and has a fibrous feel due to the abundance of root material. The A^horizon is a fine pale white silt containing some root materiaK10^). This zone was not always found, and when located it varied in thickness from 0.5-12,0 cm. The thicker zones of this horizon were found in flat lying Birch groves,rarely was it found in other regions (ie) near swamps,outcrops etc. The B-horizon was reasonablely consistent throughout the grid. It was observed to be a yellow-brown to red coloured silt material. It frequently contained glacial erratics of variable diameters, (0.1-5.0 cm.) or fragments from the under lying bedrock. As in the case of the Arhorizon the B-horizon is best developed in flat lying Birch groves. Its' colour is more red-brown within the eastern part of the property,where it was mixed with much organic material from the Arhorizon. Soil in general was not well developed between lines 0+00 to 9+00 W. The s&il here,due to the presence of outcrop would most likely be a juvenile type soil rather than the more common mature type of soil. No samples were taken from line 8+00 W. as this particular line was immersed within a thick ceder swamp. The C-horizon was very rarely observed due to the fact that it was not the target horizon. When it was observed,it is found to be a pale yellow to brown silt to sand type of material,usually containing boulders or basement rock fragments. There were occasions where a light brown(beige) coloured,sandy textured material was found. It was always located in low lying regions and was usually moist,with many small rounded pebbles imbedded within it. This soil type could be a C-horizon or possibly,it is glaciofluvial material from a old river system.

-li

lt has been determined from past experience that in

glaciated terrains,the elements of Au,Ag,As,Hg, and Sb are the

primary pathfinders for gold deposits. In this survey the elements

of Au and Hg were riot analysed for and the values of the elements

Ag and Sb were so low that they are barely detectable and thus

resulted in a reiteration of less than readings and therefore

could not be used in any statistical manipulation. The Arsenic

values ranged from less than 5 to 30 ppm. The values recordered

as less than numbers were eliminated from any mathematical treatment

of data,but not necessarily from graphical representation. This

, rule applied to all elements considered significant. Secondary

elements of importance are Copper and Zinc. The values recordered

for Copper ranged from 1 to 306 ppm and for Zinc from 8 to 162 ppm.

Histograms for the elements Arsenic,Copper and Zinc(Fig.5-7) indicate

that the distribution of these elements,for the most part are skewed

toward the larger values,this is more apparent for Arsenic than Copper.

The background figure for these elements has been determined to be

5 ppm for Arsenic,2/1 ppm for Zinc,and 19 ppro for Copper. Anomalous

values were approximately found to be ^0 ppm for Arsenic,)62 ppm

for Zinc and)80 ppm for Copper. These ranges were established by means

of the 95th percentile,which suggests these values are indicative of

anomalous contents,with a high degree of probability.

The majority of the anomalous values occur within an.area

boarde'red by Line 3+00 and 1^+00 South,between stations 0+25 and 1+25"

West(Fig.2J-5). This region corresponds reasonably close to a

conductive zone outlined by the VLF-EM system. From a geological

perspective the anomalies are contained within mafic volcanic flows,

but the highest values are located within or in the vicinity of a

-5-

weakly banded Iron Formation. It seems reasonable to conclude

that there is a relationship between the observed Iron Formation

and the higher readings of Arsenic,Copper and Zinc sampled from the

B-Horizon. It is interesting to note,as where the interpreted

conductor travels,so goes these particular elements,as therev

are few high metal values in the western portion of the property,

as well as no conductive material present. The Iron Formation was not

visibily traced beyond line 11+00 South,but high element values

were found as far east as line 0+00. This poses the question,does

the Iron Formation continue further east,or are the anomalous metal

results dependent on another factor?. From the geology it is known

that there is a band of sheared schistose rock,that is prevalent

across line 1+00 West,where it is visible intermittently for 300

meters between lines 9+00 and 12+00 South, This shear zone is

adjacent to a interpreted topographic lineament. This leads to the

possibility of a small weak fault structure being in this sector.

If this hypothesis is true,it may be the reason for the interpreted

conductor and the presence of these elements.

CONCLUSIONS; The existence of a fault structure on

this property is conjectered on the basis of visible parallel shear -

zones and interpreted conductive zones. The relatively high values

of the various elements maybe related to this structure or may in

fact have more of a connection to the Iron Formation,as the largest

readings for all these elements are situated very close to this

lithologic unit. Therefore this alleged fault must be furthered

defined by means of a close spaced pedogeocheraical survey as well

as actual rock analysis. This may prove to be logisticly difficult,

as the interpreted lineament is obscured by lakes and swampland.Respectively Submitted

"li 1 ! Uriinr i***** ! M***^--lf!f!r^jIjij-rji-'r irn tp-| l — — —*~ "" "" ~~ i, Usosi^rsd-i-^^1-"-"—i jt-r~ i ij_i—rrl.—

l le uo talc*cclojf4!?^ - -^^J^^SMMBTJ *y w

Scale: 1 cm.s 7.8^ M.(A) cm.s 13.7

Map showing position of Vincent Township within Mining district and location of claims withih. township. ___________ (B)

Mtf.i?Une# 012 3 4 5' 6 7 89 10 11 12 13 14 15 16 17 18 19oôc

0+25

0+500+75

1+00

1+25

1+501+752+00

2+25 2 + 50

2+75

3+003+253+503+754+00

4+25

4+50

4^755-00

5-25

5+50

oo oooooooo oooo o ooooo oOOOOO O OO00OO OOÔ

o o oo o o o o ® 00 u

20 21 22

0 0o o oo o o

2 S

oo

oo o ooooooooo ooooo o /~^^^—^jooooo \o o o o o o o ^--î^

ooooo oo

Vincent TownshipN LEGEND1 O 0-5 ppm Arsenic

1 O 5-15 ppm ArseniclL (?) 1 5-30 ppm Arsenic

(8)30-45 ppm ArsenicQ i*45 ppm Arsenic

D O O 0^ _

}o o o o oy o0 0

oooooooooo

o ooo n

Geochemical Map of Arsenic ^B-Horizon (-80 mesh)

t

o

0 0

o o oo o o

0

o0

o0 0

0 00

o

o0

o

o

o

Line^0+00

0+25

0+500+75

1+00

1+25

1+501+752+002+252 + 50

2 + 75

3+00

3+253+503+754+00

4+25

4+50

4*752 f 00

012 3 4567 89 10 11• ® O O ® ® O C

Fig. 312 13 14 15 16 17 18 19 20 21 22 23

) O O O0 O O• * 0 00O®O ® 0000• ••00 o •ooo®® ® o ^ o .

0 0 ** ® O O ® *O O 0 O 0 ® C®000 O ^-— -^^J00 0 0 t \0 O 0 0 0 0 0 ^^---^f

O ® ® 0 0 06

Vincent TownshipN LEGENDl 'O 0-15 ppm Zinc

l O 15-30 ppm ZincL ® 30-45 ppm Zinc

(P 45-60 ppm Zinc0 60-99 ppm Zinc0 > 99 ppm Zinc

00 ® o ® o og) 0 O O O O Oi * o . o o o

.0.000 o oy o o o o— o o o

o o oo ® o o o o o o0 O O O

o o o0

0 0 00A rz\ /oGeochemical Map of Zinc w v^ v^-

B-Horizon,(-80 mesh) 0 00 0

oo

^50 o

Une# 012 3 i, 5 6V 89 10 11 12

0+00

0+25

0+50 0+75

1+00

H25

1+50H752nOO2.25

2+502+75

3+00

3+25 3+503+75Vi 00

4+25

4+50

4+755+00

5+25

5+50

® o o o o ® o o® ® (i) ® O O* ® 0 O O O O GOO

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O O O 0 0 \O O 0 G 0 ^ ® ^ — ,

0 G 0 00 G ^-^d)

Vincent TownshipH LEGEND1 O 0-20 ppm Copper

1 O 20-40 pprn Copper0 40-60 pprn Copper @) 60-80 ppm Copper0 8d-100 pprn Copper ^ >100 ppm Copper

13 14 15 160 O OO O(DO O 0 0(D O O Oe o

}® G 0

^ oO (Do0 0

o0 0

Geochemical Map of Copper B-Horizon (-80 mesh)

9

J''iLr .4 17 1819 20 2 i 22

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VINCENT. TOWNSHIP.

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Pfa

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eab 13. fl 20. a 40. a 60. a 80. a 100. a a00.a

COPPER (PPM).

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DOCHERTY.

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Aldescription Z

VS-0011-5-002VS-003VS-004ys-oosVS-006VS-007VS-008VS-009VS-010ys-oiiVS-012VS-013VS-014VS-015VS-016vs-017VS-018VS-019VS-020VS-021VS-022VS-023VS-024VS-025VS-026ys-02?•v'S-028VS-029VS-030VS-031VS-032VS-033'v'S-034ys-035VS-036VS-037VS-03SVS-039VS-040

3.871.111.101.921.481.491.933.123.911.101.922.171.032.770.971.520.951.331.513.592.171.462.322.792.781.660.943.011.210.731.691.991.683.201.303.322.761.203.073.66

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Bi Cappi Z

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12331588469291971531723263085204969268757

AA CERT, t : A8G183 73-001-AINVOICE * : 18618373DATE : 29-SEP-8GP.O. * : NONE

Cu Fe Ga K La Mq Hnppi Z ppi Z ppi Z ppi

71 9.62 10 0.11 10 1.44 94420 2.09 (10 0.02 10 0.23 13319 1.33 (10 0.01 10 0.20 10423 4.19 10 0.01 10 0.49 37113 1.41 (10 0.01 10 0.19 8220 1.78 (10 0.01 10 0.17 9121 3.77 10 (0.01 10 0.52 30064 7.17 10 0.02 (10 0.89 640

121 10.29 10 0.04 (10 1.45 100821 1.47 (10 0.01 10 0.25 13933 3.51 10 0.03 10 0.29 47317 1.97 10 0.03 10 0.37 24313 1.39 (10 0.01 10 0.17 6868 8.28 10 (0.01 10 1.06 126219 1.74 (10 0.01 10 0.20 11618 2.39 (10 0.01 10 0.27 20314 1.97 (10 0.01 10 0.21 40122 2.20 (10 0.01 10 0.32 20430 2.75 (10 0.02 10 0.41 30389 10.79 10 0.01 (10 1.33 85454 6.36 10 (0.01 10 0.67 107416 6.79 (10 0.01 (10 0.28 29042 5.73 (10 0.01 10 0.40 48S46 7.32 (10 0.02 (10 0.91 44635 7.41 (10 0.03 10 0.67 64119 3.20 (10 0.04 10 0.61 3522 1.72 (10 0.01 10 0.12 74

45 7.80 (10 0.02 10 0.84 15146 4.43 (10 0.02 (10 0.64 538

40 3.81 (10 0.01 (10 0.14 20823 1.90 (10 0.01 10 0.21 11437 3.78 (10 0.03 10 0.52 122227 1.71 (10 0.02 20 0.22 21445 8.46 10 0.01 10 1.04 106213 1.86 (10 (0.01 10 0.19 9697 6.92 10 0.01 10 1.00 103378 7.42 10 0.01 10 1.29 105113 2.00 (10 0.02 10 0.22 33690 6.85 10 0.02 10 0.95 100661 8.25 10 0.01 10 1.S8 1823

Mo Nappi Z

(1 (0.01(1 0.02(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 0.02(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01

values rGa,only

La ,be

eported forMg, K, Na,considered

AlSr ,as

, SbTl,

semiTi

a r, u

-quant

Be.a n d

i tat

Ca, Cr .V can

i ve .

COMMENTS :

Ni Pppi ppi

61 15015 15010 7013 16012 100

8 19023 11033 28079 20011 10023 45023 1407 90

34 40011 110

8 1909 1708 150

15 25022 34026 330

6 22018 35052 37031 35014 3005 90

34 32022 130

6 21011 24018 34020 13039 3809 130

28 32035 48011 22055 37035 330

PbPP"

6668466426884

1046664

(26462464Ttt

1010484246668

10

Sbppi

tttttttttttttttttttttttttttttttttttttttttttttttttttttttttt(5(5(5(5(5tttttttttttt

SrPP*

91385866339*7

99

12786771•7t

4665

11S556878465

108

106

liZ

0.420.100.100.170.090.090.220.160.460.110.110.100.090.270.100.100.080.120.110.090.390.110.200.070.130.170.110.230.120.090.100.110.090.330.100.230.340.110.120.25

11ppi

(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10

Uppi

(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10

VPP*

1914623

118293478

168268

37753736

2364759516055

3112461221341181947351

152144

47358734

21142

135157

43181178

UPPE

tttttttttttttttttttttttttttttttttttttttttttttttttttttttttttttttttttttttttttttttt

Ir,pps

76161238202436763422683414881432284234

10068287484926018

1064476368030

120M**

7280349096

_ ———

-.————————————————————— — :———————

———

— .———

—

TO : DOCHERTY.

5G3 RIDGERIDGEUAY,LOS 1NO

Staple Al description ~

VS-041VS-042

j VS-043VS-044VS-045VS-046VS-047'••3-048VS-049VS-050 VS-051VS-052VS-053VS-054US-055ys-056VS-057VS-058VS-059VS-060'.'S-061VS-062VS-063VS-064VS-065VS-066VS-067VS-068VS-069VS-070VS-071VS-072VS-073VS-074VS-075VS-076VS-077VS-078VS-079

,, VS-080

3.061.56 1.141.071.391.563.260.541.202.50 2.261.262.012.111.400.981.911.972.161.700.360.992.043.591.491.453.481.051.251.771.351.161.161.210.961.161.430.340.900.82

B R

R D

IAH AA

ONTARIO

Ag ppi

0.20.2 0.20.20.20.20.20.20.20.2 0.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.2

As PPi

1010 (5

510

515{51015 10{510151010203010

55

105

{555

10555

{5{5{5

55

105

{55

{5

B-3 Sepps ppa

80 {0.540 {0.5 40 {0.530 {0.520 {0.530 {0.580 {0.510 {0.520 {0.520 {0.5 50 {0.520 {0.540 {0.540 {0.520 {0.520 {0.560 {0.540 {0.560 {0.590 {0.530 {0.520 {0.550 {0.540 {0.530 {0.540 {0.570 {0.520 {0.520 {0.520 {0.530 {0.530 {0.530 {0.530 {0.510 {0.520 {0.530 {0.520 {0.520 {0.530 {0.5

Bi ppi

ri{2 {2{2{2{2{2{2{2{2 {2{2{2aa{2{2{2{2{2{2{2{2{2{2{2{2{2

T

{2{2{2{2{2{2{2{2{2{2{2

Ca2

0.200.20 0.310.200.130.210.730.190.260.49 0.120.120.290.540.210.120.240.220.420.210.140.150.140.070.190.140.810.200.240.510.150.190.190.190.150.480.550.120.120.15

Cd ppi

{0.5{0.5 {0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5 {0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5{0.5

Co pps

216 6469

281

1119 12

49

1111

5212013

947

113186

1667

15945668

10344

Crppa

4630 27212732

1031430543618425137205036423124233577393169232840382426282633421922Mti

Cu pps

6817 2513402337112262 63224241in4***

1430

306432411273988471161

661

157622

27112775{124

4

Fe•f fm

5.422.04 1.391.332.003.407.430.822.165.432.961.322.743.133.492.945.47

15.692.753.501.781.802.529.161.702.523.021.411.703.402.521.311.391.442.131.842.461.391.541.75

CERT. * INVOICE DATEP.O. t

Ga K ppa 2

{10 0.03{10 0.02ao 0.02•ao o.oiao o.oi

10 0.01ao o.o3{10 {0.01ao {o.oi

10 0.01ao o.oi{10 0.01{10 0.02

10 0.01{10 0.02{10 0.01{10 0.02{10 0.03{10 0.02{10 0.02ao o.oi{10 0.01{10 0.02

10 0.02{10 0.01{10 0.01

10 0.02{10 0.01{10 0.01{10 0.01ao o.oi{10 0.01{10 0.02ao 0.02ao o.oiao o.oiao o.o3{10 0.01ao o.oiao o.oi

La PPi

1010 1010101010101010 10101010101010101010101010

ao10105010101010101010101020101010

A36133 126133 29-3EPNONE

Mg Hn 2 ppi

0.97 14290.24 112 0.27 1910.19 840.29 1360.40 2590.94 26400.15 900.24 1230.59 1393 0.34 1730.16 870.42 2700.66 5000.42 3010.18 3150.47 22840.41 24390.42 4460.30 3610.25 1030.23 1820.30 5701.14 9280.43 1550.24 1470.45 3530.28 1470.26 1390.41 10660.34 3890.20 1320.23 1500.29 1570.25 1290.38 2620.39 3000.14 620.16 670.17 159

— ^ o m Aj -j* -36

Ho Na pps l

{1 {0.01a {o.oi a {o.oi{1 {0.01a {o.oia {o.oia {o.oia {o.oia {o.oia {o.oi a {o.oia {o.oi{1 {0.01{1 {0.01{1 {0.01a {o.oia {o.oi{1 {0.01{1 {0.01{1 {0.01{1 {0.01a {o.oia {o.oi{1 {0.01a {o.oi{1 {0.01{1 {0.01{1 {0.01a {o.oia {o.oi{1 {0.01a {o.oi{1 {0.01{1 {0.01a {o.oi{1 {0.01{1 {0.01{1 {0.01{1 {0.01a {o.oi

val Ga , onl

tjez, r e p o r La, Mg. '

y be cons

ted for K, Na, i d e r e d

AlSr.as

. st.Tl,

semi

r Ba, T i, U

-quant

Be, Ca, Cr .and V can

i t a t i v e .

COMMENTS : m mNi

ppi

3717 1412141244

41630 3111252217

7202328231012224524154411182415111116141819

711

7

Pppi

410320 110190170100370

5050

300 170

6016016012013034052019017011090

290360100150360

7070

170170210150

8011012024010080

120

Pbppa

36 iif

4OM

210

244 223644

1066244244242244282

{242424

Sb PPi

{5{5{5{5{5{5{5{5{5{5 {5{5{5{5{5{5{5{5{5{5{5{5{5{5{5,{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5

^Sr T:

ppa l

7 0 .198 0.11 9 0.108 0.097 0.117 0.259 0.066 0.086 0.104 0.13 6 0.126 0.08

10 0.109 0.165 0.166 0.076 0.095 0.02

10 0.109 0.097 0.106 0.097 0.093 0.037 0.118 0.12

12 0.1011 0.118 0.109 0.098 0.118 0.09

10 0.1210 0.116 0.097 0.10

14 0.106 0.095 0.097 0.09

Tl ppi

{10ao{10{10{10ao{10aoaoao ao{10{10ao{10aoaoao{10ao{10ao{10{10{10ao{10{10{10{10{10ao{10{10ao{10{10aoaoao

Uppi

ao{10 {10{10{10ao{10{10{10{10 {10ao{10aoaoao{10{10aoao{10aoao{10{10ao{10ao{10{10{10{10{10ao{10ao{10ao{10ao

•^

yppi

10533 23244088

1211843

101 532543707545

101715139423447

13733464930315554253929453645312844

^y

ppi

{5{5{5{5{5{5{5{5{5{5 {5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5{5

Znops

63 - -16 - ~13 - -14 - ~20 ~ -32 ~ -70 - ~

3 - -14 - -46 ~ ~ 23 ~ ~i* M _36 - -88 - -32 - -30 ~ ~60 - -

160 — - '43 — —22 ™ ~18 - -26 - ~54 - -78 ~ -26 - -40 ~ -CQ - —— jo —72

no - --76 ~ ~3*J

ft ~~

lo "~~ ~~

32 - ~162 - -38 - -24 - -26 - -12 - ~10 - - '22 - -

LOS

Saaple description

VS-081VS-082VS-033V3-OS4VS-085VS-036VS-087VS-038V'S-089VS-090ys-09iVS-092ys-093VS-094VS-095VS-096VS-097VS-098ys-099ys-iooyS-101VS-102ys-iosVS-104ys-iosVS-106ys-io?VS-108ys-109VS-110ys-iiiVS-112VS-113VS-114VS-115vs-116vs-117VS-118V'S-119VS-120

IK'0

AlT

1.001.211.031.031.461.271.311.472.220.570.901.052.400.651.321.840.621.502.800.680.771.661.202.261.790.381.401.951.211.101.241.431.331.381.481.711.121.651.351.34

'-J 1 T J.

Ag ppi

0.20.20.20.20.20.2A ** Vi*

0.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.2

n JL\ o. *-

As pps

5(510(510

510

555

1010(5(55

105

(510

55

10101010

5555555

(55

1055

1510

S

t

B.3ppa

20302020403040202010202020102040204040103030302050203040302020202020304040502030

Se ppi

(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0,5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5

Bi ppi

(2(2(2(2(2ti\ w(2(2/t\u

/l••bif

(2(2(2(2(2

"tM

(2(2(2(2(2(2(2(2(2

2(2(2(2(2(2(2(2(2(2(22

(2(2(2

C.3Vjt

0.360.110.140.200.140.220.140.150.170.030.410.100.130.100.100.150.350.120.360.150.110.120.110.320.140.230.120.120.160.110.110.100.120.110.150.160.140.200.140.13

Cd ppi

(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5

Coppi

3456

11777

17173

1125

1148

315265

199555633846775

1076

Crppi

2923292762233732

10314372062163139152871242037344438262934312423272933433527462854

Cuppi

22(1

4IS87

141362

1to

349(1102685

8319(120143619112

(12

(11935101625(1

11031

FeIV

f*

1.511.722.021.393.421.472.462.814.751.311.561.96

12.040.761.663.011.331.686.941.011.602.842.636.492.181.211.502.411.541.862.251 ontt m *i*M

1.392.782.641.811.342.791.591.85

l 1 "J

Gappi

(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10

1^^^^^^

K*ts.

0.01(0.010.010.010.020.020.020.010.010.010.020.010.010.010.020.030.010.010.030.020.010.020.020.010.020.030.020.030.030.020.010.010.020.010.010.030.020.020.020.02

^^^MMV

LaPps

10(1010101010101010

(102010

(10101010

(10101010

(101010

(1010101010101010101010101010101010

^^MilM

10.230.150.210.240.490.250.300.300.320.070.280.150.390.140.220.430.130.200.910.230.110.280.260.650.320.210.200.190.240.140.160.170.200.270.350.210.200.370.280.24

iîîî^H

"rtn ppa

2115632

120573118118164290

53250

59526

7436

132112

811548

8474

12611596412810684819866697586

170166

8975

203113

71

••••^^^^^H

Ho Ha ppa 2

(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01(1 (0.01

COMMENTS :

Ni ppi

151011162217171334

317

515

413235

1539116

1413232013151516

96

161112131912201220

Certlf

P ppi

130150170160230110180100200140240130280

7013020012016029010090

22019045019012015029025015013010015025026026017033030

150

led

Pb ppi

42423244i44422266442444242244222*i

M

4224

(24

by .

3b ppi

(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5

•vN^

Sr PP"

5667

11977

476455*?

6565566437973676767939

' 77

li

0.090.090.110.090.090.100.120.120.200.070.070.080.050.060.100.120.150.090.200.070.080.110.120.120.120.080.090.120.100.100.120.100.110.110.120.110.090.130.090.11

\v a

li ppi

(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10

^

upps

(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10(10

Sbz^

yppi"29^

30402974274555

100392744

1222335533327

12621445746

10741242744293445373653523226503534

.* " -

H ppi

1(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5(5

————————— 1

Znppi

13 - -18 - -22 - -22 - -52 - ~16 - -IS ~ -20 - -52 - ~18 - -22 — —18 - ~70 -- ~10 - -14 - -30 - -28 - - 116 - -76 - -12 - -36 ~ -34 - -20 - ~54 -- -T) ~—**4*

12 ~ ™16 - -16 - -14 - -12 - -20 - -18 - -18 - -28 - -32 - ~16 -- ~16 - —40 -- -24 - -24 -- ~

V03rev 11,85

——————————————————————————— CERTIFICATE

TO : DOCHEETY. BRIAN

563 RIDGE RD. RIDGEUAY. ONTARIO LOS 1NO

Saiple AI Ag As Ba Be Bi Ca Cd description 1 ppa ppi ppi ppa ppi ~ ppi

' OF ANALYSIS ——————————————————————————

AA CSRT. # : AS613373-004-A INVOICE * : 13613372 DATE : 29-SEP-SG P.O. t : NONE

Co Cr Cu Fe Ga K La Mg Hn Ho Nappa ppi ppa * ppa I ppa I ppi ppa Z

Nitr ic-Aqua-Regia digestion of 0.5 g m ofmaterial followed by ICP analysis. Since thisdigestion is incomplete for many minerals, values reported for Al, Sb, Ba, Be, Ca. Cr . Ga, La, Mg. K ^ a , Sr, Tl, Ti f R and V can only be consio^Fed as semi-qualitative.

COMMENTS :

Hi P Pb Sb Sr li 11 U V M Zn ppi ppa ppa ppa ppa 1 ppa ppa ppa ppa pea

ys-i2iVS-122 VS-123 VS-124 VS-125 VS-126 VS-127 VS-128 VS-129 VS-130 VS-131 VS-132 VS-133 VS-134 VS-135 VS-136 VS-137VS-138 VS-139 VS-140 VS-I41 VS-142 VS-143 VS-144 WS-001 US-002 MS-003ys-oo4US-005 MS-006 MS-007 US-008 MS-009 MS-010ys-oiiMS-012 MS-013

0.971.781.211.231.150.820.911.161.151.371.291.681.681.351.611.121.311.091.260.731.121.201.500.931.061.030.711.121.421.571.941.312.051.831.251.230.55

0.20.20.20.20.20.20.20.20.20.20.20.26.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.2

510510105

(55

10555

10555555(510(5515-5 —

(5510tf(5105555(55

30803020302010402010303040303030302030202030201020202030203030304040304020

^. 5(0.5(0.5a. 5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5(0.5

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SAMPLE LOCATI DIM-SO ILS- WALTERS TOWNSHIP-CLAIM NO.845985

LINE NO. 0+00 1+00 E. 2+00 E. 3+00 E.

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0+50

0+75

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1+25

1+50

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WS-58

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WS--69

WS-68

WS-67

WS-66

MS-65 WS-62

WS-63

WS-62

WS-61

WS-60

WB-59

SAMPLE LOGATION-SOILS~ WALTERS TOWNSHIP-CLAIM NO. 845991

LINE

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WS-23 WS--15

WS-22 WS-16 WS--10

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WS-5

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C C-

42E12NEei87 2.9546 VINCENT 900

January 23, 1987 Your File: 263Our File: 2.9546

Mining RecorderMinistry of Northern Development and Mines435 James Street SouthP.O. Box 5000Thunder Bay, OntarioP7C 5G6

Dear Madam:

RE: Notice of Intent dated December 19, 1986 Geophysical (Electromagnetic, Magnetometer) Geological and Geochemical Surveys on Mining Claims TB 845986. et al, 1n Vincent Township

The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.

Please Inform the recorded holder of these mining claims and so indicate on your records.

Yours sincarely,

J.C. Smith, A/ManagerMining Lands SectionMineral Development and Lands BranchMines and Minerals Division

Whitney Block, Room 6610 Queen's Park Toronto, Ontario M7A 1W3

Telephone: (416) 965-4888

SH/mccc: Brian Oocherty

563 Ridge RoadRidgeway, OntarioLOS 1NO

Resident Geologist Thunder Bay, Ontario

Encl.

Mr. G.H. FergusonMining i Lands CommissionerToronto, Ontario

y o ^

t, o K o

Ministry ofNorthern developmentand Mines

Ontario

Technical Assessment Work C redits

File

2.9546Date Mining Recorder'! Report o*

Work No.December 19,1986 , 263

Recorded Holder

BRIAN DOCHERTYTownsn;Q or Area

VINCENT TOWNSHIPType of survey and number of

Assessment clays credit per claimGeophysical

Electromagnet,c _-

Magnetometer ———

40

20

Radiometric __________,

Inauced polarization ______

Other _______________

.days

. days

. days

-days

.days

Section 77 (19) See "Mining Claims Assessed" column

Geological __.__..___________.___days

15Gi;oc:v;mical _,

Man days

. days

Airborne j_,

Ground \Xl

C:"'C!its nnvo ::een niduccd because of corrections :o .vork datos and fiyures of applicant.

Mining Claims Assessed

TB 845986 to 990 inclusive

Special credits under section 77 (16) for the following mining claims

Mo ornciits ,iave been uilowecl for the foilowinq mimno ninims

nsuif ; c:ent technical data filed

iMn'-",: •v i roKl''i '".u ri'diKV 'tis 1 jbovr criHiitr, M M"ci;',s.n\ ' mil,'i ".-.M t he total number of approved assessment days recorneo on each cl.iim iioes not eu t'''' r" -ixi m LI,T . ; o'.MM l .is M Hou s: G i 1 o pin suvii - /O, '^ -j o,H i c.;: - --0. o coe he rtit cal - 40; Section 77(19) - 60.

828 (85/12)

Ontario

Ministry ofNorthern Developmentand Mines

Geophyslcal-Geological-Geochemical Technical Data Statement

File—

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

lW

Type of Survey(s). Township or Area. Claim Holder(s).!

lo

G. A

Survey Company

Author of

Address of Author . K

Covering Dates of Survey \ o\L

Total Miles of Line r.ut(linecutting to office)

g. o

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical —Electromagnetic —— z

DAYS per claim

—Radiometric-Other ^—Geological.Geochemical. •2.0

AIRBORNE CREDITS (Special proviiion credits do not apply to airborne surveys)

Magnetometer Electromagnetic Radiometric(enter dayi per claim)

nfa SIGNATURE..Author of ReporWor Agent

Res. Geol.. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

-rg (number)

re.t~s ryxj? t* * * * •T*•••••••••••••••••••••••••••••r*r**********

TOTAL CLAIMS.

837 /85/12)

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

Number of Stations Station interval ——Profile sralp l CM ^ fo Ol

25 x/l fa-rfcTR.5

.Number of Readings

.Line sparing 11? O

Contour interval.

C

Instrument. G f? o

Accuracy — Scale constant. Diurnal correction method.

A /M d/*-

6Asg

Base Station check-in interval (hnnrs) Base Station location and value A/ooflrts D

ECTROMAGNETIC Oijl configuration

CV*j] separation

Acnirary i X /*

Method: 0 Fixed transmitter Q Shoot back d In lineFrermenrv ^A Cvr L-trii //liO'^f g*/- P *"?;. .... ... ....

D Parallel line

Parameters measured.(specify V.L.F. station)

J,,

O

Instrument.Scale constant.Corrections made.

Base station value and location.

Elevation accuracy.

9M

O)

InstrumentMethod D Time Domain

— On time ———.- Off time ——.

Delay time.

Power.Electrode array — Electrode spacing . Type of electrode

Q Frequency Domain _ Frequency .^.—-—— — Range_______

SELF POTENTIALInstrument_______________________________________ Range.Survey Method •—-—-———————^—-—-—————————-—.^^-—.———-^.......-—

Corrections made.

RADIOMETRICInstrument.Values measured.Energy windows (levels) ————-———..-—-——^—^——.—.——-.——.————.-.——.—-Height of instrument___________________________Background Count, Size of detector—————^——————.^—.^————-.—^^^^^..————.——..————Overburden —^—^—-——..^^^^^————.^——-....—-^^———————^—.——

(type, depth — include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.) Type of survey.—————.^^——^—.—-———————^— Instrument ————————————————————————— Accuracy——————————————————————————Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYS Type of survey(s) ———— Instrument(s) —————

(specify for each type of lurvey) Accuracy^—————————————-

(specify for each type of survey) Aircraft used—^-^———————-..————-—-^——^^—.——.—

Sensor altitude.Navigation and flight path recovery method.

Aircraft altitude_______________________________Line Sparing Miles flown over total area________________________Over claims only.

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.

Total Number of Samples.t~i

Type of Sample.(Nature of Material)

Average Sample Weight—J±L-5nl Method of Collection, •SV---^-^—q~t

S -Soil Horizon Sampled. Horizon Development, 7)oofi ~ Sample Depth. Terrain dues

*.~,

Drainage Development—Estimated Range of Overburden Thickness.

ANALYTICAL METHODSValues expressed in:

Others———————

per cent p. p. m. p. p. b.

Field Analysis (.Extraction Method. Analytical Method. Reagents Used——

Field Laboratory AnalysisNo. ————-^^—-.

SAMPLE PREPARATION(Includes drying, icreening, cruihing, athing)

Mesh size of fraction used for analysis____

Extraction Method. Analytical Method - Reagents Used __

Commercial Laboratory (. Name of Laboratory Extraction Method Analytical Method, Reagents Used __

9/D

©(circle)

.tests)

.tests)

.tests)

GeneraL General.

CO CO

toCL

(T UJ OD2OOo

WALTERS TWP G-I7I

614231 .145052

- - l- - - -,- J"T"; -. y -gr~~\ ^^933

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614495 1614496

BEARDMORE G-7

42E12NE8187 2.9546 VINCENT 200

TOWNSHIP

C Hf™ R, l ™W** r" l\! 8 KL*M H li B

M.N.R. ADMINISTRATIVE DISTRICT

MINING DIVISION ^ QeAAUtTo ri

THUNDER BAYLAND TITLES REGISTRY DIVISION

THUNDER BAY

SAND AND GRAVEL

\} G H AV E. L

(s) QUARRY PLhMIT

FILE i I3IO"5

THUNDER' BAYMIMINO D IVIVION

JAN -9 1987AM Pfcfl7|8|9|IO|11|12|1|2I3|4|5|C

LEGEND

PATLNTLD L.ANO

i-'ATtNii;o ron suHi'Aci: RK.HK; ONLYLKASL

LICCNSK Ol- OCCUPATION

CHOWN LAND bALEG

LOCATfDLAND

CANCELLED

MINING RIGHTS ONLY

;;unrAc;[: HIGHTG ONI Y HIGHWAY A nourr. NO.ROADS

THAILS

HAILWAYii

©l'

L,O.

C. S.

Loc.C,

M.n.o.5 H.O.

WAHfiH OR MU5KCG

MINUS

'uf.frd unly with L. u mm f: r rujjurt ij ur whyn : [-.IL-O i^ limited

SCALE: 1 INCH ^ 40 CHAINS

F f h T1000 ?000 4QOO 6000 aooo

—J

D 2DO METRES

1000M KM)

2 f J 00(2 K M

Ministryof LandNatural ManagementResources Branch

Ontario

DateFEBRUARY IGth, I9BI

Number

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WALTERS WfcST CLAIM 845985

VLF ProfilesCAYUGA SYNDICATE

SCALE

2.54cm. to 5o{nFIELD WORK PERFORMED, INTERPRETED AND PLOTTEI

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VERTtCAl SCACt lc TRANSMITTER NAA- 24 kHz

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VLF ProfilesCAYUGA SYNDICATE

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42E12NE0187 2.9546 VINCENT

OH-OO

3C7

MAGNETIC BASE = 60300 GAMMAS

VERTICAL SCALE 1 cm - 25 GAMMAS

3/V/& -

WALTERS WEST CLAIM 845985

Magnetic ProfilesCAYUGA SYNDICATE

SCALE; 2.54cm. to 50m.

FIELD WORK PERFORMED, INTERPRETED AND PLOTTEIBY: P. ... ..,~,

L 3W

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MAGNETIC BASE* 60300 G AMMAS

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WALTERS EAST CLAIM

Magnetic ProfilesCAYUGA SYNDICATE

SCALE.

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J.A.

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42E12NEai87 2.9546 VINCENT

250

L 23

VL

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LO

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Download - RECONNAISSANCE GEOPHYSICAL SURVEYS VINCENT TOWNSHIP … · 010 2.9546 reconnaissance geophysical surveys

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