drill hole record hole no pml-06 - ontario€¦ · *** dip tests *** depth azi. dip 41 205 -48 71...
TRANSCRIPT
UJ.U
PENTLAND FIRTH VENTURES LTD. rage: 1 of 12Property: MARCHAUD PROPERTY: GARRISON CREEK JV.EASTING: 9620 ENORTHING: 3160 NElevation: 2130Grid: PFVL GRID 1997Collar Azi.: 200Collar Dip: -47Local Ref: \Ref1Hole Length: 461.0 metresPrint Date: 11 May, 1999
DRILL HOLE RECORD
*** Dip Tests ***Depth Azi. Dip
41 205 -4871 201 -48
101 197 -49131 205 -49161 200 -49191 199 -49221 195 -49250 200 -49281 199 -49311 203 -49341 206 -50401 205 -49431 213 -46
Drill Hole: PML-06Township: MichaudClaim #: (Patented) L-45153Date Started: Nov 6, 1997Completed: Nov 14, 1997Logged by: K. D. TyleeDate(s) Logged: Dec 3-9, 1997Drilled by: NOREX DRILLING LTD.Core Size: NQCompany: PFVL
lj
ll/ O Av-" 1}
Purpose: To test a VLF feature w/in a lithological contact environment, south of the Ludgate Zone "Hole Condition: 36m NW casing left in hole, not cemented .
Comments: Core cross-piled at the Norex Drilling office, Hwy 101 E, Porcupine
From(m)
.0
35.9
41.5
To(m)
35.9
41.5
42.7
RockType
'h^t
'b* i
4-4-44-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-44-4-4- 4-4-4
'VVV,V W' VV\
Geology
OVERBURDEN
ALTERED FELDSPAR PORPHYRY
RECEIVEDMA" ! 4 "~1
GEOSCIENCF ASSESSMENTOfhCE
'
A variably altered coarse pegmatitic felsic intrusive adjacent to a dyke.
Colour varys from mauve to flesh-pink to pinkish-grey.Unit hosts approximately 25X predominantlyfeldspar laths sitting w/in a siliceous matrix- laths are commonly up to 4X1cm in size
euhedral, white to grey coloured,- groundmass.
. These tend two be alligned in twopredominant orientations at 0-20 and 50-60 degrees to the core axis.Variably carbonatized.
Local siliceous stringers and veinlets with adjacent flooding. Nil sulphides.Minor coarse rubble at random intervals.
ALTERED MASSIVE MAFIC VOLCANIC FLOW
Sample From(m)
To(m)
Lngt(m)
SULm
AUg/t
AUREg/t
AUREJg/t
AUAVg/t
Page 1 of 12 Hole No: PML-06
PML-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-06 Page: 2 of 12
From (m)
42.7
48.4
51.1
To (m)
48.4
51.1
64.4
Rock Type
vv\vvvvv\ vvv'VV\
vvvvv\ vvvvv\ vvvvvvvvv'VV\
vvv'VV\
vvvVS'^'
v^yV^yV^xV^x,V^x'
V^xi
Vi^x.
y^x"^/
yV^x'
4-4-4 4-4-4- 4-4-4 4-4-4- 4-4-44-4-4- 4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
"^ "t" t'VV\
vvv'VV\
vvv
Geology
A dark green, fine grained, magnetic, chloritic and carbonatized mafic rock unit.Scatched by a blade. Sheen of fine black sheet silicates noted. Biotite ?.
Moderately to strongly developed chloritic alteration adjacent to theemplacement of a diabase immediately downhole.
Foliated at 35 degrees to the core axis at 42.5 meters.
DIABASE
A hard dark grey - black, fine grained, magnetic, weakly porphyritic mafic dyke.A typical Abitibi diabase.
Numerous fine, white, wispy calcite stringers and fracture filling.Unit hosts approximately 2-35C anhedral greenish epidote-quartz blebs -phenocrysts, average 2-3mm diameter.
Upper contact at 20 degrees to the core axis.Irregular lower contact, possible at 50 degrees to the core axis.
ALTERED FELDSPAR PORPHYRY
A multiphase felsic porphyry intrusive. Salmon-pink, hard, texture varies fromequigranular - intrusive up to, locally, coarse porphyritic.
Several pale grey coloured, extremely siliceous, zones occur at:.at 48.4-49.1 meters, adjacent to the contact. Start seeing the partially
digested coarse lath porphyry at 48.8 meters. O.S-1% disseminated cubic pyrite.- at 49.5-50.4 meters, several minor pulses/floods, Q.5% pyrite.- at 50.5-51.1 meters, almost cherty. Trace to D.5% fine disseminated pyrite.Minor green chlorite and fine pyrite fracture filling.
ALTERED MASSIVE MAFIC VOLCANIC FLOW
Sample
73955
73956 73957 73958
73959
From (m)
47.9
48.4 49.1 50.5
51.1
To (m)
48.4
49.1 50.5 51.1
52.0
Lngt (m)
.5
.7 1.4 .6
.9
SULm
.0
.2
.5
.5
.2
AUg/t
.01
.04
.01
.02
.01
AUREg/t
.01
AUREJg/t
AUAVg/t
.01
.04
.01
.02
.01
Page 2 of 12 Hole No: PML-06
PML-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-06 Page: 3 of 12
From (m)
64.4
To (m)
85.4
Rock Type
vvvvvvvv\ vvvvvvvvv vvvvvvvvvvvv vvvvvvvvv vvvvvvvvvvvv vvvvvvvvvvvv vvvvvvvvvvvvvvvvvvvvv'VVV
vvv4-4-4
4-4-4-4-4-4
4-4-44-4-4-4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-
Geology
As intersected above the diabase, this unit is green coloured, fine grained,chloritic and carbonatized.Massive flow material VS. Fine grained quickly cooled mafic intrusive ?.
Unit is non magnetic.Local zones of fine grained biotitized material easily identified. Individualflakes up to V2mm dia.
At 51.1-54 meters, numerous white wispy calcite stringers - bands.one grey coloured, extremely siliceous zone at 52.0-52.55 meters.
Approximately 40cm TW, 40 degrees to the core axis.at 52.9 meters, one 12cm TU band at 60 degrees to the core axis. Pale pinkish
grey.- warping/buckling of the calcite stringers readily noted at 51.8 meters. Entireinterval, including the silicification hosts only trace sulphides.
At 64.4 meters, lower contact at 70 degrees to the core axis.
FELDSPAR PORPHYRY
a coarse feldspar porphyry, or pegmatite, as described uphole at 35.9-42.7meters.
Abundant (20-307, vol) coarse off-white to grey coloured, euhedral feldsparlaths, occasionally up to 4x1cm in size, sit w/in a pink to predominantly bridkred matrix - groundmass.Local areas with elevated py content, to a maximum of D.7-1%.Local fine chlorite fracture filling.
68.8 70.0 1-27. fine pyrite fracture filling and minor disseminated cubes.
At 70.8-71.4 meters, one dark green mafic dyke or possible xenolith. Chloritic,as described above the intrusive contact.Contacts at 50 degrees to the core axis.
At 80 meters, the coarse laths in the vicinity tend to be mauve coloured andavg. 1-2cm in length.At 83.4 meters, laths show a preferred orientation of 70 degrees to the core axis
Attitude of the lower contact difficult to determine, due to minor zone ofblocky core.
Sample
73960739617396273963739647396573966
739677396873969
From (m)
52.052.653.054.055.056.357.2
68.068.870.0
To (m)
52.653.054.055.056.357.257.7
68.870.070.6
Lngt (mj
.6
.41.01.01.3.9.5
.81.2.6
SUL (70
.2
.2
.0
.0
.0
.0
.0
.02.0.2
AUg/t
.03
.04
.06
.01
.01
.00
.00
.11
.06
.13
AUREg/t
.14
AUREJg/t
AUAVg/t
.03
.04
.06
.01
.01
.00
.00
.11
.06
.13
Page 3 of 12 Hole No: PML-06
PML-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record Page:
Hole No: PML-06 4 of 12
From (m)
85.4
To (m)
354.4
Rock Type
-t- 1- -1-
-t- 4- -i
vss/sxN/S/
/OXN
O"Ns\sN/N
ON/N//N/N/NXy/
x^/N/N/N
/N/V/N
ONX/N/N
CXxx/S/N
S/N/N/N/N
xS/N/
/N/
X)ONXL/N/N
C/Nx/N/N
ONx/N/N
N/N
)S?
Geology
ULTRAMAFIC VOLCANIC FLOW
Very dark green-grey coloured, fine grained, soft, magnetic and predominantlycarbonatized UM flows which have been intruded by many coarse felsic porphyrydykelets and larger dykes.
Readily scratched with a blade to produce a fine pale green talcose powder.
Numerous thin white calcite stringers, possible sutures.Averages nil to trace sulphides.
Occasional very dark green to black 1cm strongly chloritic - biotite bands.selvage ? trace to r/, adjacent disseminated pyrite.
At 90.9 meters unit is moderately carbonatized below this loc'n.
At 108.4 meters, 10cm dykelet. Resembles grannodiorite !. 2/i pyrite, 30 degreesto the core axis.
Numerous Pinkish grey, siliceous, lath porphyry to megapegmatitic. Whiteeuhedral laths reach 2-3cm in length. These are centred on.- at 114.1 meters, 23cm TW, 50 degrees to the core axis, 2'/, pyrite.- at 115.15 meters, 20cm TW, 30 degrees to the core axis, Z'/, pyrite.- at 115.9-117.0 meters, contacts oriented at 30 degrees to the core axis, D.5%disseminated cubic pyrite. Pinches It swells.- at 119.85 meters, 4cm TW, 30 degrees to the core axis.
120.2 121.8 Overprinting of pale pink calcite, leaving V2cm dia. Blackporphyryoblasts of chlorite - biotite. Numerous very fine whitecalcite seams oriented at 20 degrees to the core axis. Nil sulphides.
At 121.8-122.7 meters, pink - grey vuggy feldspar dyke at 25 degrees to the coreaxis. Abundant chlorite - calcite fracture filling. Trace pyrite.
Weak to moderate developed hematite zones, 20cm in corelength at 122.8 meters.at 123.7 meters.
From 128.8-129.48, flesh coloured, equigranular feldspar porphyry. Trace pyrite,siliceous, subhedral feldspar laths.- upper contact at 20 degrees to the core axis, lower contact at 70 degrees tothe core axis.
Sample
73970737717377273773737747377573776737777277872779739807398173982739837398473985739867398773988739897399073991739927399373994739957399673997739987399974000754017540275403754047540575406754077540875409754107541175412
From (m)
113.0113.9114.3114.8115.3115.9117.0118.5119.7120.2121.8122.7123.9183.8184.4184.9185.8186.2203.3204.4205.3206.0206.6207.9208.8230.0230.5231.0232.5234.0235.5236.6237.5238.5239.2240.3241.6308.0308.8310.0311.5328.8329.4
To (m)
113.9114.3114.8115.3115.9117.0118.5119.7120.2121.8122.7123.9124.5184.3184.9185.8186.2186.7204.4205.3206.0206.6207.9208.8209.8230.5231.0232.5234.0235.5236.6237.5238.5239.2240.3241.6242.7308.8310.0311.5312.0329.4330.3
Lngt (m)'
.9
.4
.5
.5
.61.11.51.2
.51.6.9
1.2.6.5.5.9.4.5
1.1.9.7.6
1.3.9
1.0.5.5
1.51.51.51.1.9
1.0.7
1.11.31.1.8
1.21.5
.5
.6
.9
SUL (30
.02.0
.22.0
.2
.5
.0
.2
.2
.0
.0
.2
.0
.01.0
.0
.2
.0
.0
.51.04.0
.5
.5
.0
.0
.2
.0
.0
.0
.01.0.0.0
1.01.0.0.0.2.2.0.0
1.5
AUg/t
.00
.03
.00
.17
.01
.10
.00
.00
.00
.03
.69
.021.01
.02
.30
.01
.00
.01
.00
.24
.21
.09
.47
.13
.00
.00
.01
.00
.04
.00
.00
.07
.02
.01
.09
.00
.01
.13
.16
.06
.01
.00
.03
AUREg/t
.67
.08
.02
.00
AURE Jg/t
AUAVg/t
.00
.03
.00
.17
.01
.10
.00
.00
.00
.03
.68
.021.01
.02
.30
.01
.00
.01
.00
.24
.21
.09
.47
.13
.00
.00
.01
.00
.03
.00
.00
.07
.02
.00
.09
.00
.01
.13
.16
.06
.01
.00
.03
Page 4 of 12 Hole No: PML-06
PML-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-06 Page: 5 of 12
From (m)
To (m)
Rock Type
(Xs\sXyX)/\/XJ)vSvS\x\
vS(Xx5X)y\
/\-/X)VS
sX/o^o\)\"jC
OcXyX)VSN/X
ON)Ox)\\y
X)y\
8?
Geology
At 129.6-132 meters, numerous diffuse zones of strongly carbonatized and weaklyhematitic material. Trace pyrite.- adjacent to 133.9 are black well developed selvages, buff coloured amygdulesalligned at 90 degrees to the core axis.
Coarse lath porphyry - megapegmatitic readily noted at 134-139.6 meters.
Upper contact oriented at 30 degrees to the core axis. Increasing lath sizebelow 134.9m. Trace pyrite.Lower contact at 40.
At 149.3 meters, well developed polysuture texture, calcite infilling.
Several mottled mauve - pink - grey coloured felsic dykes occur AT:.- at 153.73 meters, 18cm TW, 25 degrees to the core axis.- at 156.6-156.9 meters, adjacent hematite for 50cm.- at 157.3-157.7 meters, 30cm TW, 45 degrees to the core axis.- at 159.7-160 meters, pink to buff, chlorite fracture filling, adjacentsi licif ication.
Minor DIABASE dyke at 160.0-161.4 meters. Fine grained, hard, black to very darkmauve/wine coloured, and strongly magnetic.- with 2-3/6 pale green, olivine eyes, each 2-3mm in dia.- upper contact at 50 degrees to the core axis, lower oriented at 30 degrees tothe core axis.- core is blocky, reduced to a rubble at 160-160.3 meters.
At 161.4-162.2 meters, buff coloured, ankeritic halo adjacent to the maficintrusive. Nil sulphides, minor barren calcite stringers.
Salmon-pink coarse lath porphyritic at 164.7-165.6 meters. Predominantly 1cmsized euhedral white to grey coloured feldspar laths.
siliceous, trace pyrite. Irregular blocky contacts with adjacent calcitefracture filling, stringers.
At 176.25-183.8 meters, megapegmatitic intrusive. White to pale grey laths up to3X2cm in a carbonatized, salmon-pink matrix.Upper contact at 25 degrees to the core axis, lower contact oriented at 50degrees to the core axis.
Minor pale pink grey coloured siliceous felsic intrusives occur at:.
Sample
75413754147541575416754177541875419
From (m)
330.3349.0349.5350.5351.2352.7353.8
To (m)
330.8349.5350.5351.2352.7353.8354.4
Lngt (m)
.5
.51.0.7
1.51.1.6
SULm
.0
.01.0.2.2.0.2
AUg/t
.01
.04
.00
.04
.01
.01
.01
AUREg/t
.04
.01
AURE Jg/t
AUAVg/t
.01
.04
.00
.04
.01
.01
.01
Page 5 of 12 Hole No: PML-06
PML-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-06 Page: 6 of 12
From (m)
To (m)
Rock Type
\Xs\sVj)xNsySy\yScS0\/OV/X
0\/"x
X/ON/S/y/yX.
s\^X
cYCxCx/N/NONX/XyvNONXT/*xS\y\/\yN/NOK/\vx/ONX)/*
x/\x*/N
/Nx
CX
Geology
- at 184.35-184.9 meters, irregular contacts, undulates about the CA, 155 finedisseminated cubic pyrite.
at 186 meters, 12cm TW, oriented at 45 degrees to the core axis, tracesulphides.- at 195.4-200.7 meters, pink coloured, siliceous felsic porphyry. Averagestrace pyrite, 155 adjacent to 200m. One spur or off-shoot, similar to a vein runsdown the CA between 195. 4-196. 1m.This is perfectly boudinaged, individual knots/boudins average 2X1cm in size.Volcanic xenolith at 198.3-198.85 meters. Chloritic, well developed biotitizedcontacts. At 200.7 meters, lower intrusive contact at 70 degrees to the core axis
at 202.7-203.3 meters, pale green-grey, siliceous, equigranular, nil to tracepyrite. Contacts at 30 degrees to the core axis.- at 204.35-208.8 meters, a larger, salmon pink coloured siliceous unit.Multi-phase, predominantly fine grained with local lath intervals.Numerous dark green xenoliths at: 204.4 (5cm), 205.3 (15cm) and 207. 9-208. 15m.Unit averages O.S-1% disseminated cubic pyrite.A maximum of 3-555 vol. Occurs between 206-206. 6m as disseminated cubes, blebsand fracture filling. Stringer adjacent silicification, flooding.Both contacts oriented at 40 degrees to the core axis.
Numerous minor pale pink grey coloured siliceous felsic intrusives continue tooccur at.
at 213.1-213.35 meters, 40 degrees to the core axis, with adjacent(down-hole), weak silicification and very weak hematite.
at 218.3-219.8 meters, numerous minor irregular intrusives w/in stronglycarbonatized and very weakly hematitic volcanics.- at 221.4 meters, 20cm TW, at 40 degrees to the core axis.- at 223.6-224.2 meters, 20 degrees to the core axis.- at 225.3 meters, 18cm TW, 75 degrees to the core axis.
at 230.5-230.95 meters, extremely siliceous, flooding, dirty white in colour.Occasional pyrite cube only.- at 232.85-233.15 meters, 75 degrees to the core axis.- at 236.6-237.45 meters, equigranular feldspar porphyry at 25 degrees to thecore axis. 155 disseminated pyrite cubes, very siliceous, buff - pink coloured.- at 239.2-241.6 meters, pale pink to flesh coloured, coarse, equigranularfeldspar porphyry.Abundant euhedral laths average 1cm in size. 155 fracture filling pyrite.Contacts at 40-45 degrees to the core axis.- at 244.7-248.8 meters, buff - grey, abundant euhedral laths, trace pyrite, 40degrees to the core axis.- at 251.15 meters, 15cm TW.- at 254.05-254.4 meters, calcite replacement of fine matrix. Grey, 40 degreesto the core axis.- at 255.95 meters 15cm TW, 45 degrees to the core axis.
Sample From (m)
To (m)
Lngt (m)
SULm
AUg/t
AUREg/t
AUREJg/t
AUAVg/t
Page 6 of 12 Hole No: PML-06
PML-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-06 Page: 7 of 12
From (m)
To (m)
Rock Type
^x/x5x/vSS/N
S/N
OsvSvS?VX)X)'xN/\y'xxSS/N
ON
A/
OsX/Os/\yN/N
ON0\vS/S/
y\yxS
8
Geology
Intrusive textured medium grained interval at 213.35-220 meters, possibly due tothe calcite replacement of the groundmass. Local epidote.
Predominantly blocky core at 213.6-216.5 meters, and at 256-261 meters, finepale green soapy gouge.
At 263.85-266.8 meters, megapegmati tic intrusive. Pink, abundant (30-405Svol.)feldspar laths av 1-2cm in length. Trace - Q.5% pyrite.Fine grained adjacent to both contacts, grading into coarse porphyry after20-30cm. Minor pyrite at lower contact.
At 271.6-272.4 meters one or more 5-10cm dykelets undulate about the CA.At 276 meters, medium grained biotite in the immediate vicinity.
At 279-287 meters, numerous 2-10cm fine grained felsic dykes cut this interval.Nil to trace pyrite. 0-30 degrees to the core axis.
Numerous moderate sized felsic porphyritic - syenite dykes intrude the DMbetween 291 -300. 5m.
these average 20cm TW, are carbonatized, pale grey in colour and arepredominantly oriented at 40 degrees to the core axis.
At 303.3-31.55 meters, pinkish siliceous megapegmati tic. Feldspars reach 3X1cm.Dark green chloritic xenolith at 304.95-305.5 meters.
both contacts oriented at 25 degrees to the core axis. Unit becomes increasingsiliceous towards the lower contact, below 308.8m.
At 317.3 meters, 2mm black biotite - chlorite fragments, porhyryoblasts w/in apale green fine matrix.
At 319 meters, one 4cm pinkish-grey siliceous felsic dykelet weaves about the CAfor V2m, centred on this loc'n. Trace pyrite.At 322.8-324 meters, the adjacent fine grained volcanics tend to be slightlyharder, greener. Possible an intercalated mafic flow interval, but lacksdiatinct boundaries.
From 329. 1-330. 3m: one dirty-grey coloured strongly siliceous feldspar porphyrydyke. T-2% fine pyrite fracture filling, minor white calcite fracture filling.Oriented at 40 degrees to the core axis. 18cm chloritic xenolith centred on329.8m.
At 331.4 meters one strongly biotitized zone, 20cm in TW. No adjacent intrusive
Sample From (m)
To (m)
Lngt (m)
SUL C 0/.)
AU 9/t
AUREg/t
AUREJg/t
AUAVg/t
Page 7 of 12 Hole No: PML-06
PML-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-06 Page: 8 of 12
From (m)
To (m)
Rock Type
\A
^X)O/\yxS'S/
CX
vSN/S
v\y\^o
\s\s\X")xS0\x/vRvRvSs\//x/V)YyX)''/X
x/XxN/S/\/x/"yX.0\x)
s
Geology
or veining.
At 339.0 meters fine vugs lined with calcite and chlorite.
From 339.5 to 340.1m: increasing chlorite - biotite content towards the contactat 340.1 meters.Dark to very dark green coloured, near-complete groundmass replacement by whitecalcite.Nil sulphides, very minor calcite stringers - sutures.
At 340.1-343.2 meters, fine grained mafic dyke. Dull reddish-grey in colour,hard, pervasive calcite.- 35i fine (2mm dia.) black chlorite chips or wisps, as well as T-2% pinkfeldspar blebs scattered throughout the matrix.These chlorite wisps show an allignment, foliation at 20-30 degrees to the coreax i s .- hand samples resemble a clastic sediment, however the sharp contacts andadjacent alteration suggest intrusive emplacement.- nil sulphides and significant veining.Upper contact oriented at 25 degrees to the core axis, lower at 0-10-20 degreesto the core axis.
From 343.2 to 344.7m, contact alteration, as above the dyke. Again white.barren, calcite replaces the groundmass.
At 345.2-347.8 meters, coarse lath porphyry intrusive, Almost megapegmatitic.40K Euhedral, white to grey laths sitting w/in a salmon pink fine grained weaklyhematitic matrix.Numerous dark green chloritic xenoliths.Irregular, non-parallel intrusive contacts.
At 349.5-352.7 meters, strongly siliceous lath porphyry with 3-4 10-20cm zones,floods ? of silicification.- T-2% fine disseminated pyrite adjacent to the upper contact, but the intrusiveaverages trace, at best, pyrite.
interval also hosts 2 partially digested, wispy chloritic xenoliths. Numerousthin white, barren ankerite-quartz stringer.- moderately developed hematitic matrix, brick red in colour, at 351.2-352.7meters. No appreciable increase in pyrite content.- upper contact oriented at 25, lower contact at 40 degrees to the core axis.
At 353.8-354.4 meters, dark grey fine grained, hard, contact altered halo.Strongly magnetic, nil sulphides.
Sample From (m)
To (m)
Lngt (m)
SUL C/0
AUg/t
AUREg/t
AUREJg/t
AUAVg/t
Page 8 of 12 Hole No: PML-06
PML-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record Page:
Hole No: PML-06 9 of 12
From (m)
354.4
To (m)
444.0
Rock Type
i
Geology
At 354.4 meters lower unit contact oriented at 45 degrees to the core axis.
MODERATELY ALTERED FELDSPAR PORPHYRY
A visually distinct, altered porphyry phase. Possibly a marker unit.
This altered coarse lath porphyritic intrusive unit varies from grey to pink tooccasionally mauve and green in colour.Unit hosts up to 40/6 predominantly euhedral feldspar laths, reaching 2-3cm inlength.These sit w/in an altered matrix, which has been strongly carbonatized andvariably replaced by:.- dark green fine chlorite (of the original pyroxenes ? - rectangular in formand 2-3mm in length).- black shiny FeOxides - magnetite ?.- fine grained pyrite.- and minor black fine grained biotite.
Unit is locally magnetic.
2 Preferred orientations to the allignment of the feldspars may be observed, atapproximately 70 and 30 degrees to the core axis.
354.4 355.3 1/6 fine disseminated cubic pyrite at 354.4-356.3 meters.
At 359.5-362.1 meters numerous quartz-calcite veinlets, average 1cm TW, with2-3/6 adjacent fine pyrite along the walls,.- this veining cuts the intrusive predominantly at 40 degrees to the core axis.
361.8 362.2 2/6 fine grained pyrite adjacent to a 3cm TW veinlet centred on 362m.
368.8 369.3 2/6 fine pyrite lines the walls of a 2cm siliceous veinlet at 40degrees to the core axis.
At 369.8-370.0 meters, local pale grey coloured, silica flooding. Totallyreplaces the matrix. 2-356 fine disseminated pyrite.
371.1 371.7 Local accumulations of 2/6 fine pyrite adjacent to minor sweats.371.7 372.2 2/6 disseminated and fine fracture filling pyrite.
At 378.1-378.45 meters pale grey coloured, strongly siliceous interval. Veiningor flooding.- numerous fine fractures, with calcite and minor pyrite fracture filling.
Sample
75420 75421754227542375424754257542675427754287542975430754317543275433754347543575436754377543875439754407544175442754437544475445754467544775448754497545075001750027500375004750057500675007750087500975010
From (m)
354.4 355.3356.3359.0359.5360.5361.8362.2368.0368.8369.3369.7370.1371.1371.7372.2377.1378.1378.5378.8379.2380.0381.5382.7383.4384.6385.2389.0389.9391.0392.0393.1393.9394.7400.7401.4402.8404.0405.2405.8407.0
To (m)
355.3 356.3357.0359.5360.5361.8362.2362.7368.8369.3369.7370.1371.0371.7372.2372.7378.1378.5378.8379.2380.0381.5382.7383.4384.6385.2386.0389.9391.0392.0393.1393.9394.7395.8401.4402.8404.0405.2405.8407.0408.2
Lngt (m)
.9 1.0.7.5
1.01.3.4.5.8.5.4.4.9.6.5.5
1.0.4.3.4.8
1.51.2.7
1.2.6.8.9
1.11.01.1.8.8
1.1.7
1.41.21.2.6
1.21.2
SUL (36)
.5
.5
.0
.0
.2
.22.0.0.0
1.0.0
2.0.0
2.02.0.0.0.5.5
2.0.0.0.0.0.0.5.0.0
1.5.0.0
1.01.0.0.0
1.02.01.03.02.0.2
AUg/t
.08
.07
.02
.01
.02
.02
.01
.00
.01
.12
.01
.12
.03
.03
.09
.05
.02
.14
.07
.07
.02
.01
.02
.02
.00
.02
.02
.01
.16
.00
.01
.16
.16
.04
.18
.00
.08
.01
.10
.02
.03
AUREg/t
.02
.08
.00
.01
.25
.07
AUREJg/t
AUAVg/t
.08
.07
.02
.01
.02
.02
.01
.00
.01
.12
.01
.12
.03
.03
.09
.05
.02
.14
.07
.07
.02
.01
.02
.02
.00
.02
.02
.01
.16
.00
.01
.16
.16
.04
.22
.00
.08
.01
.10
.02
.03
Page 9 of 12 Hole No: PML-06
PHL-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record Page:
Hole No: PML-06 10 of 12
From (m)
To (m)
Rock Type
Geology
At 379.0 meters, one 40cm, pink, calcite-quartz vein oriented at 35 degrees tothe core axis. Pyrite fracture filling and 1 band, 3-5mm TU.
At 384.6-385.2 meters, siliceous - hematite zone. Pale grey silicification withnumerous brick red bands and wisps of hematitic material.Numerous fractures with fine calcite, chlorite and minor pyrite fracture filling.
At 389.3 meters local FeHags have been replaced by a very fine grained, black.shiny FeOxide - magnetite.
From 387. 9-391. Om, buff coloured sericite - siliceous. Numerous quartz-calcitestringers and the occasional veinlet.
interval averages T-2% very fine disseminated pyrite. Veining is predominantlybarren.
Blocky core, with local gritty rubble at 393.1-397.7 meters. Brecciated lathscommon.- fine red hematite and pyrite fracture filling.
At 400.0-400.5 meters, megapegmatitic portion/phase of the intrusive.
At 405.8-404 meters, buff coloured sericite emanates-bleeds outwards fromquartz-calcite fracture filling into the dark reddish grey host.These are oriented at 0-30 degrees to the core axis. Interval averages 2/idisseminated fine grained pyrite.
401.4 402.8 T-2% disseminated pyrite at 402 meters.404.0 405.2 Buff coloured sericite adjacent to local fractures which run along
the CA, and locally split the core.405.2 405.8 Fine grained semi-massive pyrite adjacent to one irregular white,
barren QUARTZ VEIN at 30 degrees to the core axis, centred at 405.6meters.
405.8 407.0 Minor pyrite adjacent to one quartz-calcite stringer at 406.2 meters.
6 Pale grey siliceous stringers and one 17cm TW QUARTZ VEIN cut the intrusivepredominantly at 55 degrees to the core axis between 408. 8-409. 2m.- adjacent replacement of the original retangular laths (or FeHags ?) by veryfine grained pyrite. Veining is barren.
408.8 409.3 S-5% pyrite emanates outwards, (perpendicular to the vein walls),from a 17cm vein centred at 409.1 meters, oriented at 55 degrees to
Sample
750117501275013750147501575016750177501875019750207503375034750217502275023750247502575026750277502875029750307503175032
From (m)
408.2408.8409.3410.5411.6413.0414.3421.7422.2423.0426.2427.0428.0428.8430.0431.5433.0434.5436.0437.5438.5439.2440.0441.0
To (m)
408.8409.3410.5411.6413.0414.3415.3422.2423.0423.5427.0428.0428.8430.0431.5433.0434.5436.0437.5438.5439.2440.0441.0442.0
Lngt (m)
.6
.51.21.11.41.31.0.5.8.5.8
1.0.8
1.21.51.51.51.51.51.0.7.8
1.01.0
SUL("/o)
5.04.0.2
2.0.2
3.0.2.0
3.0.0.0
1.0.2
4.03.02.01.51.01.01.01.0.2.2.0
AUg/t
.05
.02
.00
.12
.00
.01
.00
.00
.04
.02
.02
.07
.01
.01
.01
.00
.14
.14
.35
.16
.55
.12
.04
.03
AUREg/t
.04
.53
AUREJg/t
AUAVg/t
.05
.02
.00
.12
.00
.01
.00
.00
.04
.02
.02
.07
.01
.01
.01
.00
.14
.14
.35
.16
.54
.12
.04
.03
Page 10 of 12 Hole No: PHL-06
PML-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-06 Page: 11 of 12
From (m)
444.0
To (m)
452.2
Rock Type
4-44 -t- + 4
4-4-4
+W4- 4- 4
44-4
+Wt t- 4
444+Y+*- 1 1 4!
- 4- t- 4
4-4-4
Geology
the core axis.410.5 411.6 2-3/6 pyrite growth adjacent to 3-4 minor white, barren
quartz-calcite stringers at 50 degrees to the core axis.
At 413.3-414.3 meters, interval averages 3/6 disseminated pyrite, as partialreplacement of the dark green chloritic FeMags.
422.2 423.0 Fine pyrite fracture filling and haloes adjacent to fractures whichundulate aout the CA.
427.0 428. 0 Several pale grey siliceous bands or floods oriented at 45 degreesto the core axis. 1-2/6 associated fine grained disseminated pyrite.
From 428.8 to 439.1m, a distinct, interval which averages 256 pyrite. Thissulphide predominantly occurs as fracture filling and a network/matrix of finedisseminations w/in the porphyrys groundmass.
428.8 430.0 Zone Maximum of 3-5/6 pyrite.
At 439.2-444.05 meters, a crowded lath porphyry phase of the intr. 40/6 whiteeuhedral feldspar average 1cm in length sit in a pinkish grey fine matrix. Tracepyrite only.
440.0 441.0 Moderately developed red hematite w/in the matrix at 440.3-440.6meters. Trace pyrite.
FELSIC INTRUSIVE
A hard, predominantly fine grained, dirty-buff to mauve coloured, weaklyporphyritic unit.A possible seperate, cross-cutting phase of the larger, coarser porphyry oneither side.
Minor phenocrysts of anhedral feldspar and blebs of green chlorite observed.- Individual pieces of the equigranular material resemble syenite.
Pervasive strong calcite. Weakly hematitic, gives the unit its mauve colour.Predominantly blocky core. Occasional trace sulphides on the chloritic fractures.
At 440.05 meters, irregular upper contact. Lower contact at approximately 30degrees to the core axis.
Sample From (m)
To (m)
Lngt (m)
SUL (36)
AUg/t
AUREg/t
AUREJg/t
AUAVg/t
Page 11 of 12 Hole No: PML-06
PML-06 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-06 Page: 12 of 12
From (m)
452.2
To (m)
461.0
Rock Type
+VV4-'. 4; 4
4-' ^-. 4-'
4-' J-. V
4-' *. 4-'
4-' J-. 4-'
4-' 4-. 4-'4-'. t 4
4-' *. 4-'4-'. 4; 4
4-'-t 44-' J-.4-'4-'.4- 4
r j-.V4-' J-. f4-'.4; 4
t-' t. f4-'-4; 4
f J-.V
*A*
Geology
MODERATELY ALTERED SYENITE
A continuation of the altered (chlorite-pyroxene/carbonate/hematite/magnetite)porphyry uphole above 440.05m.
Interval lacks the appreciable veining or pyrite content seen uphole.
Unit is variably carbonatized and magnetic.
At 457.5 meters, almost total replacement of the matrix by fine white calcite.
At 461 meters End of the Hole.
130 Samples submitted to Swastika Labs Ltd. For Au analysis.
Sample From (m)
To (m)
Lngt (m)
SULm
AUg/t
AUREg/t
AUREJg/t
AUAVg/t
Page 12 of 12 Hole No: PML-06
-----}-----f ——— ——— -I---949286
-f950225 ' 950226 ,
806029
LDT 10
l 950217 l
463,000 -t g 5.91 g/t Au 88,000 oz, gold falconbridge United, 1988
PENTLANDGARRISON CREEK
PML-p T l (QSR) JV l L40914 i t L40918 l L 40920^ — i — \-40922_
I'T^sT'rSi * ii i/ ' '\ i il \ A L45153 !
IB Bl 521421
CDN. lil
CDN. IIl
L45159 j 38505M B B BBL — —— —— -
Pen-Hond 1997 Drill Hole (Filed for Assessment)
Previous Drilling
47192
PENTLAND FIRTH VENTURES LTD.Tinrans ONTARIO
Garrison Creek (QSR) JV
Drill Hole Locations: PML—O6
Marchaud Property - Michaud Twp. Larder Lake Mining Division
0.25 0.5 0.75 IKM
MAY 10/99 PLM6C
LDTl 8
L40914
L45152
EDH 461n
#PML-06 -47* Dip 200\Azn, PENTLAND
\
GARRISON (QS\?)
L45153m m mmmmL-521416
LDT 7
L40920 CDN. Ill
CDN, II
CREEK JV
L45154
L-521421
18*
SCALE: 1/5000100 800M
PENTLAND FIRTH VENTURES LTD.Tinnins ONTARIO
MARCHAUD PROPERTY
Garrison Creek (QSR) J.V.1997 DRILLING
Michaud TownshipDRAWN DATE' NTS'
A.H.R. MAY 10/99DWG. No.
PML06B
EDM 461n
96B5E
VLF FEATURE PML-06
9620 E 3160 N
800' Azn
LEGEND GeologyMAJOR RDCK DIVISIONS
9XF, 9YF l 1 WeoMy Altered, Moderately Altered (Henotrtlredl Syenl-te ' ——— 1 */- Silicified. pyrrtir*d, corbonotized
9F | | Unaltered Syenite
2 | | Mafic Volcanic Flows
1 | | Ultranofic Flows (Konatstic)
sz/rz's 'w/x, Shear Zone/Fault Zone
VG Visible Gold
Significant Assays Reported in g/t Au
PENTLAND FIRTH VENTURES LTD.Tlrmins QNTARID
Garrison Creek (QSR) JV
SECTION 9625E(Looking Towards 890')
MICHAUD TDWNSH1P
Au Hlstogran ] en = 5 g/t
SCALER 1^40050 150
Moy 10/99
2.19499Property: MARCHAUD PROPERTY, GARRISON CREEK J.VEASTING: 8475 ENORTHING: 3265 NElevation: 2130Grid: PFVL GRID 1997Collar Azi.: 180Collar Dip: -45Local Ref: \Ref1Hole Length: 401.0 metresPrint Date: 11 May, 1999
Purpose: Test the potential of a geophysically
PENTLAND FIRTH VENTURES LTD. Page: 1 of 10
DRILL HOLE RECORD Drill Hole: PML-10
*** Dip Tests ***Depth Azi. Dip
80 185 -44110 189 -42170 191 -43200 193 -42230 194 -41260 195 -39290 197 -38320 197 -38 360 200 -35401 200 -33
Township: MichaudClaim #: (Patented) Claim L-40911Date Started: NOV. 20, 1997Completed: NOV. 29, 1997Logged by: D. B. CRICKDate(s) Logged: NOV.26-DEC.5, 1997Drilled by: NOREX DRILLING LTD.Core Size: NQ /[Company: PFVL l
1 l\L(O^rv
anomalous zone (low VLF-MAG values) on the western side of the Property) Cj-. -, -Hole Condition: 63.0 m NW casing left in hole, not cemented. ~* ** " 'Comments: CORE is cross-piled at the Norex Drilling facilities, HWY. 101 E, Porcupine
From(m)
.0
63.0
To(m)
63.0
227.0
RockType
ictgi
'b^t'."l!.1^ 4 44-' J-. 4-'
4-'. t 4
f i-, f
r t. -rV.4; 4r j-.V4-'. 4; 4
4-' t. f4-'-t 4
4-' J-. 4-'
4-'. 4; 4
4-'. 4; 4
f i-, fV.4; 4
4-' 4-. 4-'
4-' J-. -T
4-'. 4; 4f *. f 4-'. 4; 4
4-' J-. 4-'
f"* .4
4-'.4- 44-' t.'-f
Geology
OVERBURDEN
MODERATELY ALTERED SYENITE
Lath porphyry.
RECEIVEDMAY i 4 1339
GEOSCIENCE ASSESSMENTOfFlCE '
LITHOLOGY : coarse grained syenitic lath porphyry, and megapegmatitic lathporphyry, red locally and mottled white and light grey feldspar laths, upto 1x4cm, locally zoned cores or rims, feldspar laths crowded to porphyritic, locallypseudo trachytic textured, moderately to strongly hematitized, fracture fillingsand staining, oxidized with limonite staining between 63 to 82 metres, veryblocky, highly fractured core very poor ROD, rubbly intervals, occur narrowintensely hematitic granulated zones, with brick red hematitization, moderatelyto strongly silicified, increased sulphides, variable ferromagnesian mineralcontent.
ALTERATION: moderately to strongly hematitic fracture filling and stainingconcentrated in matrix to lath porphyry, hairline hematitic red fracturefillings transecting feldspar laths.
Sample
79118791197912079121791227912379124791257912679127791287912979130791317913279133791347913579136
From(m)
74.075.577.078.580.081.282.383.184.184.8105.3106.8108.3108.7109.1109.4109.9111.4112.1
To(m)
75.577.078.580.081.282.383.184.184.886.0106.8108.3108.7109.1109.4109.9111.4112.1113.0
Lngt(m)
1.51.51.51.51.21.1.8
1.0.7
1.21.51.5.4.4.3.5
1.5.7.9
SUL(50
.3
.3
.2
.3
.2
.2
.2
.33.0.2.5.5
5.05.07.05.0.5.3.3
AUg/t
.02
.13
.03
.15
.21
.06
.03
.23
.25
.03
.11
.201.10.61
1.681.03.13.01.00
AUREg/t
.04
1.06
1.61
AUREJg/t
AUAVg/t
.02
.13
.03
.15
.21
.06
.04
.23
.25
.03
.11
.201.08.61
1.641.03.13.01.00
fi ,"\s\\ 1
Page 1 of 10 Hole No: PML-10
42A08NE2007 2.19499 MICHAUD 020
PML-10 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record Page:
Hole No: PML-10 2 of 10
From (m)
To (m)
Rock Type
4-'. -t 44-' i-. 4'
4-'. 4; 4
4-'.4;44-' 4-. 4'
4-'. t 4 f t. f
4-' J-. f 4-'-4; 4
4-' J-. fV.-t 4
4-' J-. 4'
4-'. H; 44-' J-. -f
4-'. 4; 44-' J-. f
'•r *. 4--4-'. 4; 4
4' d-. 4-"4-'. 4; 4
4-' J-.V
4-'. 4; 4 4-' ;K 4-'4-'.4; 4f J-. 4-'
4.- J-.V-4-'.4;4
4-'. 4; 44-' J-.V
f j-.V4-'.4;4f *. 4-'
4-'. 4; 44-' J-. 4-'
4-' 4-.V4-'. 4; 4
4" J-.V4-'. 4; 4f J-. 4-'4-'-t 4
4-' J-. f4-'.4;4
4-' i-. 4-'
V.4; 44-' J-. f
4-'. 4; 4 4' J-.V4-'. 4; 4
4-' i-, f
r j-.V4-'. 4; 4
4-' j-. *
V j- V; V.H: 44-' J-.+-
Geology
SULPHIDES: D.2-0.3% finely disseminated pyrite in mafic equigranular syeniticphase, coarse grained crowded megapegmatitic feldspar porphyritic, T-3% mediumgrained disseminated and clotty pyrite.
STRUCTURE: strongly fractured at 45-60 degrees to the core axis, blocky, highlyfractured core, oxidized over first 82 metres, occur undulating slip at 15-25degrees to the core axis, very poor RQD.
From 63.0 to 82.0 very blocky, highly fractured core, oxidized, rubbly core,groundwater percolation.From 74.0 to 85.0 subtle increased hematitic alteration, strongly hematitized.partially obscured by water percolation.From 84.1 to 84.8 granulated intensely hematitized zone, feldspar grainsdestroyed, fine grained brick red, silicified, with 10 cm light brownish greychert band at 75 degrees to the core axis between 84.5 to 84.6 metres, with redangular syenite fragments, S-5% disseminated pyrite, irregular black chloriticfracture fillings mm-size, contacts at 65-75 degrees to the core axis,gradational alteration contacts possible healed over FAULT ZONE, or mylonite.From 87.5 to 95.5 intensely hematitized feldspar laths, dark brownish red, lathtexture preserved.From 95.5 to 105.0 intermixed mafic lath porphyry, mafic matrix, andmegapegmatitic crowded lath porphyry, coarse grained white feldspar laths withweak hematitic red transecting fracture fillings, increased ferromagnesianmineral content in mafic matrix lath porphyry, stubby chloritized, epidotizedand biotitic dark grey to black matrix.From 105.0 to 118.5 subtle increased hematitic staining, centered around narrowgranulated, mylonite pyritized carbonatized zones.From 108.3 to 108.7 narrow granulated zone, intensely hematitic red staining,moderately to strongly carbonatized fracture fillings at 60-70 degrees to thecore axis, S-7% stringery pyritized fracture fillings, contacts at 60-70 degreesto the core axis.From 108.7 to 109.1 between granulated zones carbonatized matrix lath porphyrywith pseudotrachytic texture and S-10% pyritized laminae parallel topseudotrachytic texture at 60 degrees to the core axis.From 109.2 to 109.5 narrow granulated zone, intensely red hematitic staining,dark brownish grey anostamising pyritized fracture filling mm-size, vaguecontact at 75 degrees to the core axis.From 109.5 to 109.9 carbonatized matrix lath porphyry, S-5% disseminated pyriteconcentrated in interstitial carbonatized matrix.From 109.9 to 123.3 coarse grained megapegmatitic lath porphyry, crowded whitefeldspar phenocrysts, weak to moderate hematitic fracture filling transectingfeldspar grains.From 123.3 137.8 predominantly light pink lath porphyry with 7-15K chloritized
Sample
79137791387913979140791417914279143791447914579146791477914879149791507915179152791537915479155791567915779158791597916079161791627916379164791657916679167791687916979170704347043570436704377043870439704407044170442704437044470445
From (m)
113.0113.8114.7115.4116.2117.4136.0136.4137.7138.6139.4140.0141.1152.6154.1155.2156.7158.2159.7161.2162.7179.5181.0182.0193.5194.0199.5200.1200.4201.2202.7203.2204.5205.5206.5208.6209.3210.4211.4212.6213.6215.0216.5218.0220.0220.5
To (m)
113.8114.7115.4116.2117.4118.5136.4137.7138.6139.4140.0141.1142.6154.1155.2156.7158.2159.7161.2162.7164.2181.0182.0183.0194.0195.5200.1200.4201.2202.7203.2204.5205.5206.5208.6209.3210.4211.4212.6213.6215.0216.5218.0220.0220.5221.7
Lngt (m)
.8
.9
.7
.81.21.1.4
1.3.9.8.6
1.11.51.51.11.51.51.51.51.51.51.51.01.0.5
1.5.6.3.8
1.5.5
1.31.01.02.1.7
1.11.01.21.01.41.51.52.0.5
1.2
SULm
.31.0.5
1.02.0.3.7.3
1.01.01.51.5.3.5
5.0.3.3.3.5.5.5.5
1.0.3
1.01.01.02.01.01.02.0.5
2.01.0.5
2.0.2.2.3
1.0.1.1.1.1.3.1
AUg/t
.02
.48
.05
.07
.46
.02
.04
.00
.015.01.12.00.01.00.02.00.00.00.00.03.01.08.04.02.04.08.12.06.07.10.13.04.15.10.08.11.03.06.07.07.02.01.05.02.04.04
AUREg/t
.45
4.80
.01
.04
.04
.03
.05
AUREJg/t
1.45
AUAVg/t
.02
.48
.05
.07
.45
.02
.04
.00
.013.18.12.00.01.00.01.00.00.00.00.03.01.08.04.02.04.08.12.06.07.10.13.04.15.10.08.11.03.06.07.07.02.01.05.02.04.05
4rt X -^"y . ' O
O'^"~\
Page 2 of 10 Hole No: PML-10
PML-10 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-10 Page: 3 of 10
From (m)
To (m)
Rock Type
4-'.4; 44' ir. 4-'
4-'. 4; 4 4' . 4'
4;.4; 1
4' *.V 4-'.4; 1
C*.*4-'-4; 4
4' 4-. f
4- *!V4-'.4; 4
4* ^. 4'
4-'. 4 44-' J-.V
4-'. 4 4 4-' J-.V
r j-.Vf S-. 4*
4-'. 4; 44' t.'f
4-'. 4; 1 4' 4-.V
4' 4-. 4-
4-^.4-
4' J-.V
4' 4-.V4-'. 4 4
4-'4-.4-
4-'. 4; 44-' J-. 4-'4-'-4;4
4-' 4-. 4-'4: .4- 4
4' 4-.V
4^4; 4
4-'.4; 44' 4-. 4P
4-' 4-.V4-'.4; 4r j-. 4-'l-'-t 4
i 4-'.4; 4 4' J-. 4"4-'.4;4r j-. 4"
r 4-.V: 4-'. 4; 44-' i-.V
•f J-.4--
4-' 4-. V
Geology
and epidotized ferromagnesian minerals, mafic lath porphyry, occur maficvolcanic xenolith or dike, fine grained, dark green chloritic, biotitic, andcarbonatized, minor calcite fracture fillings, broken contacts.At 136.0 meters 40 cm brecciated red hematitized granulated syenite, brokencontacts, carbonatized, with calcite fracture fillings, Q.5% finely disseminatedpyrite.From 137.8 to 141.0 recrystallized mylonite zone, fine grained, very hard, lightwatery grey to dark charcoal grey, with red hematitized banding and streakslocally, variable banding at 15-45 degrees to the core axis, silicified andcarbonatized, irregular calcite fracture fillings, variable fracturing at 15-45degrees to the core axis, chlorite infilling, irregular jagged contacts, 1-256quartz-calcite stringer mM-SIZE, various degrees to the core axis, chert LIKE,0.5-1. OX finely disseminated and streaked pyrite.From 154.1 to 155.2 granulated hematitized zone, FAULT ZONE at 154.8 withcarbonaceous fault gouge at 50 degrees to the core axis, dark purplish red.moderately to strongly carbonatized, 2-3/6 calcite fracture fillings, contacts at50-55 degrees to the core axis, black chloritic fracture fillings at 50-55degrees to the core axis, sheared contacts, 2-4/6 disseminated and streaked pyriteFrom 155.2 to 169.0 intermixed coarse grained crowded lath porphyry with mediumgrained equigranular syenite, moderately hematitized fracture filling andstaining, weak granulation, Q.5% finely disseminated pyrite.From 169.0 to 174.7 medium grained equigranular mafic syenite, pink feldsparphenocryst, dark purplish grey weakly hematitized mafic matrix.From 174.7 to 177.4 very coarse grained megapegmatitic lath porphyry, contactsat 5-15 degrees to the core axis.From 177.4 to 192.7 crowded lath porphyry, moderately hematitized fracturefilling and staining, locally moderately siderite and granulated zone.hematitization concentrated in matrix.From 181.0 to 182.0 moderately silicified granulated zone, very hard, lightclear buff coloured, feldspar grains destroyed, narrow pyritized red hematiticcm-size band at 60 degrees to the core axis, diffuse alteration contacts.From 192.7 to 202.8 coarse grained megapegmatitic lath porphyry, crowded whitefeldspar laths, moderately hematitized fracture fillings and associated staining.From 200.2 to 200.5 yellowish green carbonatized zone at 50 degrees to the coreaxis, intensely carbonatized, weak acid reaction ankerite, sheared at 50 degreesto the core axis.From 202.8 to 203.2 intensely brick red hematitic envelop aroundquartz-carbonate vein at 50-60 degrees to the core axis, at 203 metres,moderately granulated syenite, 2-3/6 disseminated and clotty pyrite.At 193.6 meters oxidized slip limonite staining over 5 cm.From 193.6 to 195.3 moderately hematitized megapegmatitic lath porphyry,moderately granulated, 5X quartz-calcite stringer at 30 -45 degrees to the coreaxis, possible FAULT ZONE at 195.1 metres, chloritic band at 65 degrees to thecore axis, cm-size, red angular syenite fragments.
Sample
7044670447704487044970450
From (m)
221.7222.9224.1224.8225.9
To (m)
222.9224.1224.8225.9227.0
Lngt (mX
1.21.2.7
1.11.1
SULm
.1
.2
.3
.2
.2
AU 9/t
.02
.03
.09
.01
.01
AUREg/t
AUREJg/t
AUAVg/t
.02
.03
.09
.01
.01
Page 3 of 10 Hole No: PML-10
PML-10 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-10 Page: 4 of 10
From (m)
To (m)
Rock Type
*'"t 44' J-.+-
4-'. t 4 4' J-.4-
V.+ 4+-J-.+-
V.4; 4 4-' J-. 4'*'-t 4
4-' J-. 4-
4-".4; 44-J-.+-
4-'.4; 44-' J-.4-
4-'. 4; 44-' J-.4--
4-'. 4; 4 4' J-.+-
4-'. 4; 44" J-. 4'
4-'. 4; 4r t.'-r4-'.4; 4r j-.'-r
4-'. 4; 4 4' J-. f•r. t 4
4' *. 4'
4-'. 4; 44' *. 4'
4-'.4; 441 J-. 4'
4-'. 4; 14-' J-. 4"
4-'. 4; 4 4' t. 4'
4-'. 4; 14-' 4-. 4'
4-'. 4; 1 4-' 4.V
4-'. 4; 4f J-.4-
V.4; 4 4" J-. 4'4-'.4; 1
4-' J-.+-
4-'-4; 44-' J-.+-
; *'-t *4- J-. 4'
4-'.4; 4+1 J-.4-
4-'. 4; 4 4' 4-. 4"
; *-'-t 1r *. 4'
4-'. 4; 4 4-' J-. H-'
: *'-t 44' J-. 4"
4-'. \ 4 4'*.4-
4.-.4;44- *. 4"
; 4"-"1; ^
Geology
74.0 75.5 Intensely brecciated red syenite, oxidized with limonite staining.very blocky, highly fractured core rubbly material, Q.1-0.3%disseminated pyrite.
75.5 77.0 Same as above.77.0 78.5 Q.2% finely disseminated pyrite.78.5 80.0 Moderately oxidized with limonite staining, competent core, moderately
to strongly hematitic staining, D.3% disseminated pyrite.80.0 81.2 Weak to moderate oxidized with limonite staining, competent core.
strong red hematitic staining, ghosty feldspar laths, Q.2-0.4%disseminated pyrite.
81.2 82.3 Same as above.82.3 83.1 Stubby grains of hematite mm-size, weakly carbonatized, decreased
oxidation, Q.2% disseminated pyrite.83.1 84.1 Carbonatized matrix to lath porphyry, D.2-0.4% disseminated pyrite.84.1 84.8 Red hematitic granulated zone, tight brownish grey chert band, S-5%
disseminated pyrite.84.8 86.0 Bracket sample.105.3 106.8 Pale hematitic red altered syenite, Q.5% disseminated pyrite.106.8 108.3 D.5% pyritized and hematitic fracture fillings at 60 degrees to the
core axis.108.3 108.7 Red hematitized granulated zone, moderately to strongly carbonatized
and pyritized fracture fillings, S-7% pyrite fracture fillings.108.7 109.1 Carbonatized matrix lath porphyry, S-7% pyrite laminae parallel to
feldspar lath alignment.109.1 109.4 Mottled brownish grey and red hematitized granulated zone.
anastomizing pyritized fracture fillings, 5 -77, pyritized fracturef i 1 1 i ngs .
109.4 109.9 Carbonatized matrix lath porphyry, S-5% disseminated pyrite incarbonatized matrix.
109.9 111.4 Q.5% disseminated pyrite.111.4 112.1 D.1-0.3% finely disseminated pyrite.112.1 113.0 Intermixed dark green mafic volcanic xenolith ?, with red brecciated
syenitic dikelets, Q.3% finely disseminated pyrite.113.0 113.8 Same as above.113.8 114.7 T.0% disseminated pyrite.114.7 115.4 Q.5% disseminated pyrite.115.4 116.2 Yellowish green bleached silicified zone, D.7-1.0% finely
disseminated pyrite.116.2 117.4 Red hematitic matrix lath porphyry, 2-4X medium grained disseminated
pyrite concentrated in matrix.117.4 118.5 Bracket sample.136.0 136.4 O.S-0.7% finely disseminated pyrite.136.4 137.7 Bracket sample.137.7 138.6 Brecciated hematitic banded mylonite, 1-2X finely disseminated pyrite138.6 139.4 Hematitic stained and streaked, purplish brownish grey chert like
recrystallized mylonite?, T.0% finely disseminated pyrite.
Sample From (m)
To (m)
Lngt (m)
SULa-) AUg/t
AUREg/t
AUREJg/t
AUAVg/t
Page 4 of 10 Hole No: PML-10
PML-10 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-10 Page: 5 of 10
From (m)
To (m)
Rock Type
V+M4-' t.'f
4-'. ± 44.- j-.'-r
4-". 4; 4r *. 4-'4-'.4; 4
4.- j-. V4-'.4; 4+1 *. 4-'
4-'. 4; 44-- i-, f4-'.4; 4
4-' *. f 4-'. t 4
4-' J-. H-'4-'- 4; 4
4' i-. 4-'4-'. 4; 4f t'-f
•f t.'f4-'. 4; 4
4-' *. +14-'.4; 4
f i-, r4-'. 4; 4+1 J-. 4-'
4-'. 4; 4f t. 4-'
V.4; 44-' *. f
4-' J-.V4-'.4;4
4-' J-.+-
4-'. t 44-' *. H-'
4-'- 4; 4r *.'*4-' J-. 4-'
f . 4'4-'.4; 4f J-. 4-'
V.+; 44-' *. f
^ t 1
: 4-'--t t4-' J-. 4-'
4-". 4; 44--J-.+-
r 4-. f4-'. 4; 4
4-' t.'-f: *-''t *4-' :K 4-'
4-' J..V
4-' J-. +1
V.+; 4
Geology
139.4 140.0 Mottled white and red silicified recrystallized mylonite, withchloritic fracture fillings with 1-2/6 associated disseminated pyrite.
140.0 141.1 Same as above.141.1 142.6 Bracket sample.152.6 154.1 Bracket sample.154.1 155.2 Carbonatized and hematitized granulated zone, sheared contacts,
FAULT ZONE at 154.8 metres, 5/6 disseminated and pyritized chloriticfracture fi 1 1 ings.
155.2 156.7 0.3-0. 5/6 finely disseminated pyrite.156.7 158.2 0.3-0.5/6 finely disseminated pyrite.158.2 159.7 Same as above.159.7 161.2 20 cm, granulated zone, at 65 degrees to the core axis, black
chloritic fracture coating, 0.5/6 disseminated pyrite.161.2 162.7 0.3-0.536 disseminated pyrite.162.7 164.2 Moderately altered megapegmatitic syenite, 0.556 disseminated pyrite.179.5 181.0 Bracket sample, 0.556 disseminated pyrite.181.0 182.0 Bleached granulated silicified zone, 1-256 disseminated and pyritized
hematitic band.182.0 183.0 Bracket sample.193.5 194.0 Oxidized and brecciated slip, limonite staining, 1.0-2.056
disseminated pyrite, scrappy quartz-carbonate veining.194.0 195.5 Narrow FAULT ZONE breccia, carbonaceous and chloritic with angular
red syenite fragments, 536 quartz-calcite stringer at 30-45 degreesto the core axis, mm-to cm-size, moderately hematitized staining.
199.5 200.1 Bracket sample.200.1 200.4 Yellowish green carbonatized zone, sheared at 50 degrees to the core
axis, 2-356 finely disseminated pyrite.200.4 201.2 Hematitized and moderately silicified lath porphyry, 1-256 clotty
pyrite.201.2 202.7 1-236 clotty pyrite.202.7 203.2 5 cm quartz-carbonate vein at 60 degrees to the core axis, brown-red
syenitic streaks, intensely hematitized wallrock envelopes 1-356finely disseminated pyrite.
203.2 204.5 Bracket sample.204.5 205.5 Locally, bleached and silicified lath porphyry, 2-356 finely
disseminated pyrite.205.5 206.5 Locally carbonatized and moderately silicified narrow zones, 1-256
disseminated and pyritized fracture fillings.
206.5-208.6 : moderately hematitized, intermittently finer grained, trace to 27,pyrite disseminated and in fractures.
208.6-209.3 : moderately hematitized, carbonatized, silicified, finer grained.Occasional quartz veinlets up to 1cm at 55-65 degrees to the core axis. Trace to57, pyrite disseminated and fracture filling.
Sample From (m)
To (m)
Lngt (m j
SUL (56)
AUg/t
AUREg/t
AUREJg/t
AUAVg/t
Page 5 of 10 Hole No: PML-10
PML-10 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-10 Page: 6 of 10
From (m)
227.0
To (m)
242.0
Rock Type
-t- *-. 4-
4-'.4; 4
4-' i-.-f4-'. 4; 4 +1 4-. 4-'
4-'. 4; 4-K *. 4-'
-K 4-.V4-'-4; 4
'-K t.'-f
4-' J-. V
4-'. 4; 4 f 4-. 4-'
: 4--H: 44' i-. 4'
-K J-.4--
4-' 4-. 4-'4-'. t 4
f t. f 4-'. 4; 4
-K 4-. -K4-'.4; 4
•V J-.4--4-'. 4; 4
V.4; 4 K 4-. -K
f t. f4-'.4; 4
4-'. 4; 44-' 4-. 4-'4-'.4; 4+1 J-. f
4-'. 4; 44--J-.4--
V-t 4-K 4-. -P4-'-4; 4
-K J-.'-K: *'-t 4r 4-. 4--4-'-4; 4
-K 4-. 4-'
4-4-44-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4- -4-4-44-4-4-
Geology
209.3-210.4 : lath porphyry, coarse grained, weakly hematitized. Occasionalhematitized fractures at 60-65 degrees to the core axis. Trace to Q.5%disseminated pyrite.
210.4-213.6 : Finer grained, moderately to strongly hematitized, carbonatized,silicified. Local hematitized fractures at 55-65 degrees to the core axis. Traceto 3X pyrite disseminated and fracture filling.
213.6-221.7 : coarse grained lath porphyry, locally weakly hematite, trace toQ.5% disseminated pyrite.
- at 220.3 meters, strongly silicified over 20cm, light redish grey, 1 2cmQUARTZ VEIN at 55 degrees to the core axis trace to Q.5% pyrite.
221.7-224.8 : Redish grey to brick red, fine grained, moderately to stronglyhematitized, silicified, carbonatized. Local weak fabric at 45-55 degrees to thecore axis. Local hematitized fractures at 45-55 degrees to the core axis. Traceto 1/S pyrite disseminated and fracture filling.
at 224.25 meters, brecciated and strongly hematitized and carbonatized. Q.2%disseminated pyrite. Upper and lower contacts at 55 degrees to the core axis.- at 224.6 meters, redish grey, intensely sheared, mylonitic over 25cm. Stronglysilicified and carbonatized, weakly hematitized. Minor chlorite. Trace to y/.disseminated pyrite. Shearing at 55 degrees to the core axis. Sharp upper andlower contacts at 55 degrees to the core axis.
,
224.8-227.0 : Crowded lath porphyry. Weakly to moderately hematitized. Localhematitized fractures at 45-60 degrees to the core axis. D.2% disseminated pyrite
ALTERED SYENITE
Medium grained syenite.
Medium grey to salmon pink to brick red, medium grained, with up to 50'/, of whiteto pink subhedral feldspars (up to 4mm), up to 15/S of chloritized ferromagnesianminerals, in a finer grained groundmass. Locally weakly to strongly hematitized,silicified, and carbonatized. Weak fabric at 45-55 degrees to the core axis.
227.0-235.5 : weakly hematitized locally, trace to 1X pyrite.
Sample
70468704697047070471704727047370474704757047670477
From (m)
227.0228.5230.0231.5233.0234.5235.5236.6237.6238.6
To (m)
228.5230.0231.5233.0234.5235.5236.6237.6238.6239.6
Lngt (m)
1.51.51.51.51.51.01.11.01.01.0
SULm
.1
.1
.1
.0
.1
.12.01.51.0.2
AUg/t
.00
.02
.04
.03
.07
.20
.27
.21
.10
.05
AUREg/t
.27
AUREJg/t
AUAVg/t
.00
.02
.04
.03
.07
.24
.27
.21
.10
.05
Page 6 of 10 Hole No: PML-10
PML-10 (continued) Pentland Firth Ventures ltd. Diamond Drill Record Page:
Hole Mo: PML-10 7 of 10
From (m)
242.0
250.4
To (m)
250.4
299.0
Rock Type
4-4-4-
4-4-44-4-4-4-4-4
4-4-44-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-44-44-4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-'. 4- 44-' t-.'f
4-'. 4- 4 4-' 4-.V
4-'. 4; 44-' f-.'f
•V 4-.V4-'-4; 4
4-' J-.4-*
4-'. 4; 4
-K *. V
4-' t; 4-'
4-' J-.4-'
4-4-44-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4- 4-4-44-4-4-
Geology
- at 229.0 meters, 40cm of blocky core.
- at 233.5 meters, 40cm lath porphyry.
235.5-236.6 : 25/6 of silicified, carbonatized, and weakly hematitized bands (upto 5cm) at 70-80 degrees to the core axis. Trace to 556 pyrite.
236.6-238.6 : dark redish grey to brick red, moderately to strongly hematitized.silicified and carbonatized. Local hematitized fractures and streaks at 55-65degrees to the core axis. Trace to 356 pyrite disseminated and in fractures.
238.6-242.0 : weakly to moderately hematitized. Trace to 356 pyrite.
- at 240.8 meters, 30cm fine grained syenitic dike at 60 degrees to the core axis
MODERATELY ALTERED SYENITE
Lath porphyry.
Salmon pink to brick red, coarse grained, with feldspar phenocrysts up to 1.5cm,moderately to strongly hematitized, silicified, carbonatized. Local hematitizedfractures and streaks at 0-25 degrees to the core axis. Trace to 156 disseminatedpyrite. Sheared upper contact at 60 degrees to the core axis.
ALTERED SYENITE
Crowded lath porphyry.
Pinkish grey to salmon pink, coarse grained, with white to grey feldsparphenocrysts (up to 1x3cm). Weakly hematitized locally. Occasional hematitizedfractures and streaks at 60-70 degrees to the core axis. Trace pyrite.
250.4-250.7 : Mafic syenite dike at 50 degrees to the core axis. Sheared uppercontact at 50 degrees to the core axis.
250.7-251.2 : fine grained, moderately hematitized and silicified locally, tracepyrite.
Sample
7047870479
704807048170482704837048470485
704867048770488704897049070491704927049370494704957049670497
From (m)
239.6240.6
242.0243.5245.0246.5248.0249.2
250.4251.2252.0279.8280.7282.3284.0285.5287.0288.4289.7291.0
To (m)
240.6242.0
243.5245.0246.5248.0249.2250.4
251.2252.0253.0280.7282.3284.0285.5287.0288.4289.7291.0292.0
Lngt (m)
1.01.4
1.51.51.51.51.21.2
.8
.81.0.9
1.61.71.51.51.41.31.31.0
SULm
1.5.2
.1
.2
.1
.1
.1
.1
.1
.1
.0
.0
.3
.2
.1
.2
.2
.2
.2
.1
AUg/t
.01
.07
.06
.11
.04
.02
.01
.08
.01
.00
.00
.06
.05
.04
.00
.04
.00
.00
.00
.01
AUREg/t
.01
AUREJg/t
AUAVg/t
.01
.07
.06
.11
.04
.02
.01
.08
.01
.00
.00
.06
.05
.04
.00
.04
.00
.00
.00
.01
Page 7 of 10 Hole No: PML-10
PHL-10 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PHL-10 Page: 8 of 10
From (m)
299.0
To (m)
342.1
Rock Type
-t- -t- -i-444444444444 444
444444444444 444444 444
444444
444 4444444444444444444444+4 444444444 4 + 4 444 444
444 4+44444 + 4444 4 + 4444444444 444
444 4 + 44444 + 4
4 + 44444 + 4 4444 + 44444 + 44444 + 44 + 44 + 4 + + 44444 + 4 4 + 4t 4 44444444 + 4
Geology
251.2-263.3 : Crowded megapegmatitic lath porphyry.
263.3-273.4 : Finer grained with few feldspar phenocrysts, weakly to moderatelyhematitized with abundant narrow silicified bands (up to 5cm). Trace pyrite.
273.4-279.8 : Crowded lath porphyry. Weakly to moderately hematitized locally.trace pyrite.
- at 274.6 meters : fracture at 50 degrees to the core axis with specularhematite fracture filling.
279.8-280.7 : dark grey, fine grained, mafic syenitic dike. Trace pyrite. Upperand lower contacts at 15 and 55 degrees to the core axis respectively.
280.7-291.0 : Intermixed lath porphyry and fine to medium grained syenite.
280.7-284.0 : Salmon pink to brick red, fine to coarse grained, weakly tomoderately hematitized and silicified, trace to 2/6 disseminated pyrite locally.
287.0-291.0 : dark redish grey to brick red, fine to coarse grained, weakly tomoderately hematitized, silicified, and carbonatized. Local hematitizedfractures and streaks at 45-55 degrees to the core axis. Trace to 2/6disseminated pyrite locally.
- at 290.8 meters, 20cm of blocky core.
291.0-299.0 : lath porphyry.
SYENITE
Intermixed Crowded lath porphyry and megapegmatitic lath porphyry.
Light to medium grey, locally pinkish grey, coarse grained, with up to 807. ofwhite to light grey subhedral to euhedral feldspar phenocrysts (up to 1x4cm),locally zoned, in a fine grained matrix. Matrix is weakly hematitized locally.Local fracturing at 15 to 65 degrees to the core axis with hematite fracturefilling. Weak fabric at 55 degrees to the core axis. Trace to D.5% pyrite locally
- at 309.9 meters, 60cm fine grained syenitic dike, weakly hematitized. Lowercontact at 30 degrees to the core axis.
Sample From (m)
To (m)
Lngt (m)
SULr/.)
AU 9/t
AUREg/t
AUREJg/t
AUAVg/t
Page 8 of 10 Hole No: PML-10
PML-10 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record Page:
Hole No: PML-10 9 of 10
From (m)
342.1
371.5
To (m)
371.5
401.0
Rock Type
-t- 1- -r4-4-4
4-4-4-4-4-4
4-4-44-4-4-4-4-4
4-4-4- 4-4-44-4-4- 4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-44-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4- 4-4-44-4-4-4-4-4
4-4-4- 4-4-4
4-4-4--4-4-4 4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-44-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4- 4-4-4
4-4-4-4-4-4
4-4-4-4-4-4
Geology
311.0-312.4 : fine grained syenitic dike. Upper and lower contacts at 40 and 55degrees to the core axis respectively.
317.3-320.7 : dark grey, medium grained syenitic intrusive, with up to 50/4 ofchloritized ferromagnesian minerals. Upper and lower contacts at 45 degrees tothe core axis.
326.9-328.8 : dark grey, fine grained syenitic dike. Upper and lower contacts at30 degrees to the core axis. 2cm fault gouge at lower contact oriented at 30degrees to the core axis.
SYENITE
Medium grained syenite.
Dark greenish grey, medium grained, granular, with up to 3056 of chloritizedferromagnesian minerals. Occasional quartz veinlets at 40-55 degrees to the coreaxis. Weakly foliated at 55 degrees to the core axis. Trace pyrite. Uppercontact at 50 degrees to the core axis.
354.2-359.1 : megapegmatitic lath porphyry. Matrix is weakly hematitizedlocally. Local weakly hematitized fractures at 40-50 degrees to the core axis.Upper and lower contacts at 45 degrees to the core axis.
360.6-361.4 : dark grey, fine grained, mafic syenite dike. Upper and lowercontacts at 55 and 50 degrees to the core axis respectively.
ALTERED SYENITE
Crowded megapegmatitic lath porphyry.
Pinkish grey, coarse grained, with grey to white to pink euhedral feldsparphenocrysts, locally zoned, in a weakly hematitized matrix. Local weaklyhematitized fractures at 10-35 degrees to the core axis. Trace pyrite. Upper andlower contacts at 40 degrees to the core axis.
383.5-393.3 : strongly epidotized and chloritized lath porphyry. Foliated at10-35 degrees to the core axis.
Sample From (m)
To (m)
Lngt (m)
SULm
AUg/t
AUREg/t
AUREJg/t
AUAVg/t
Page 9 of 10 Hole No: PML-10
PML-10 (continued) Pentland Firth Ventures Ltd. Diamond Drill Record
Hole No: PML-10 Page: 10 of 10
From (m)
To (m)
Rock Type
Geology Sample From (m)
To (m)
Lngt (m)
SUL C/0
AUg/t
AUREg/t
AUREJg/t
AUAVg/t
At 401 meters EOH.
Page 10 of 10 Hole No: PML-10
806029 l
LOT 110
806028 950246
DT 9
1
950243 !
LDTJ8
1
950242^nsna l 949283 949286
LUDGATE ZONE: 463,000 t e 5.91 gX-t Au 88,000 oz. gold TalcontoridQfr Linited, 1988
^1 l l dna^o
PENTLAND,GARRISON CREEIf
(QSR) JV lL40918 l L40920 , _ L40^2^ i_ _ _ _ - l
y ' \ yl -L45M9- ^ J^5151B ___ . .\ .^———'1T^——
5158 l L45159 jm m ^™L* m ——~ m m J-
l --- ___----±----
Pentland 1997 Drill Hole (Filed for Assessment)
Previous Drilling
PENTLAND FIRTH VENTURES LTD.Tinnins ONTARIO
Garrison Creek (QSR) JV
Drill Hole Locations PML—1 O
Marchaud Properly - Michaud Twp. Larder Lake Mining Division
0.25 0.5 0.75
MAY 10/99 PML10C
LDT 10 LDT, 9
L40911 L40913
-252n-
HDLE #PML-10 -45* Dipleu
PENTLANDGARRISON CREEK
(OSR) JV
L45149
L46238
L45151
L/46239
M
ll l
lPENTLAND FIRTH VENTURES LTD.
Tinmns ONTARIO
MARCHAUD PROPERTY
Garrison Creek (QSR) J.V.1997 DRILLING
Michaud TownshipDRAWN: DATE' NTS'
A.H.R. MAY 10/99 PML10B
S)
8475C
Q
FS") FI ^s^i n^s^i a ^L — uesiLru o -^
|^— - 180* Azn
0
-400
-600 ^
SoottD^ini s
S401X10 n.
PML-10
9X
LEGEND
^-^^ L -45149
VLF VLF
Overburden
i S 1 9Y
\/ \
.s \
\ i i
9
CLAIM
1
—
-45*
S'
*^
^
MAJOR ROCK DIVISIONS9XF, 9YF l 1 Weakly Altered, Moderately Altered (Henatitizedi Syenite
1 ——— 1 */- Silicified, pyrrtized. c*rbo*wtlz*d
9F | | Unaltered Syenite
2 Mafic Volcanic Flows
1 | | Ultranafic Flows (Konotlitic)
sz/rz'i -v/v/v. Shear Zone/Fault Zone
VG Visible Gold
Significant Assays Reported in g/ 1 Au
L -40911
^PML-10 8475E
PML-10 8475 E
V.^ l,0571,6n |
3.18/O.Sn |
CLAI,
L -4OS
-eoo
M
Ul
-400
-600
PENTLAND FIRTH VENTURES LTD.Tlnnms ONTARIO
Garrison Creek (QSR) JV
SECTION 8475E(Looking West)
MICHAUD TOWNSHIP
Au Hlstogran 1 en - 5 Q/t
SCALE' 1:400
0 50 100 150 200M
May 10/99
Ontario MHWyofNorthwn D*v*topm*ntand MOM
42A08NE2007 2.19499 MICHAUD
Declaration of AssessmentWorkPerformed on Mining Land
2) and 66(3), R.S.O. 1990
900
Transaction Number (office use)
Assessment Files Research Imaging
authority of subsections 65(2) and 66(3) of the Mining Act. Under This information will be used to review the assesment work and
tion should be directed to a Provincial Mining Recorder, Ministry , Sudbury. Ontario, P3E 6BS.
Instructions: - For work performed on Crown Lands before recording a claim, use form 0240. - Please type or print in ink.
1. Recorded holder(s) (Attach a list if necessary)
Name Pentland Firth Ventures Ltd.Address
Box 1690, South Porcupine, Ontario, PON 1HO
Name
AddressHbUUHUtU
MAY 1 - jccq j w j j
Client Number 300694Telephone Number (705)235-2311
Fax Number (705)235-2433Client Number
Telephone Number
Fax Number
2. Type of work performed: Check (/') and report on only ONE of the following groups for this declaration.
D Geotechnical: prospecting, surveys, assays and work under section 18 (regs)
Physical: drilling stripping, trenching and associated assays D Rehabil i tat i on
Work Type
Diamond Dri 1 1 ing
Dates Work From 6 11 97 To 29 Performed Day | Month | Year Day
Global Positioning System Data Township/Area (if available)
Michaud/GuibordM or G-Plan Number M-372/G-3642
J11 97
| Month | Year
Office Use
Commodity
Total S Value of -30^ Work Claimed ^ 's **" '
NTS Reference
Mining Division . , 1 sLarder Lak-e^
PunupiiieResident Geologist , t t i District fu /"^/G'lOL ^OM.e^
Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212; fv- provide a map showing contiguous mining lands that are linked for assigninuA- include two copies of your technical report. ^"*
rk;
3. Person or companies who prepared the^ Q
technical report (Attach a list if necessary) t^ Q
Name Ken Tylee - Pentland Firth Ventures Ltd.Address Box 1690, South Porcupine, OntarioName
Address
NamerRECElVFDll I-lU-V-n ' - i
Address 1 k/i&Y \ A 133^ l
Telephone Number 705-235-2311Fax Number 705-235-2433Telephone Number
Fax Number
Telephone Number
Fax Number
4. Certification by Recorded Holder or Agtfct,
- ^-V\-T\ , do hereby certify that I have personal knowledge of the facts set forth inI,(Print Name)
this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.
Signature of Recorded Holder or Agent Date
13 ISAgentbs Address
Ro. Box f- 0,Telephone Number
"705-535-2-1Fax Number
O. 003/65. Work to be recorded and distributed. Work can only be assigned to claim that are contiguous (adjoining) to the mining land where work was performed, at the time work was performed. A map showing the contiguous link must accompany this form.
Mining Clan Nutter. Or if work was done on other eligible mining land, show in this column the location number indicated on the claim map.
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
iV^OOSSS L
Parcel 12096 SEC (1.45153)1fcooSBO) 4
Parcel'12095 SEC (L45152)/goor*86* 4
Parcel 12141 SEC (L40911)/6OOOSS& ^
Parcel 12086 SEC (L45149)
L 798803
L 798804
L798805
L 798806
L 798807
L798811
L798812
L798813
L798814
L798816
L798817
Column Totals
Nutter of data Units. For other mining land, list hectares .
16.23 ha
16.37 ha
16.19 ha
16.19 ha
1
1
1
1
1
1
1
1
1
1
1
Value of work performed on this claim or other mining land.
S17.555
S9.879
S1.696
S22.167
SO
SO
sososososososososo
S51.297
Value of work applied to this claim.
SO
SO
SO
SO
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S4.400
Value of work assigned to other mining claims.
SO
S8.633
SO
S22,167
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
530,800
Bank. Value of work to be distributed at a future date
817,555
S1.246
S1.696
SO
SO
so
so
so
so
so
so
so
so
so
so
S20.497 (CONTINUED . . .)
- o , do hereby certify that the above work credits are eligible underl (Print Full Note)
subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim
where the work was done.
Signature of Recorded Holder or Agent Authorized in Writing Oate
6. Instructions for cutting back credits that are not approved.
Some of the credits claimed in this declaration may be cut back. Please check (/) in the boxes below to show how you prioritize the deletion of credits:
B' 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.
Q 2. Credits are to be cut back starting with the claims listed last, working backwards; or
D 3. Credits are to be cut back equally over all claims listed in this declaration; or
E 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):
Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.
For Office Use Only—^^——^^——^^——^^^^—^^^———Received Stamp Deemed Approved Date
Date Approved
Date Notification Sent
Total Value of Credit Approved
Approved for Recording by Mining Recorder (Signature)
0241 (06/97)
Ontario MnMiyofNortum DtvttopnwnltndMnn
Schedule for Declaration of Assessment Work on Mining Land
Transaction Number (office use}
Mining Claim Number. Or if work was done on other eligible mining land, show in this column the location number indicated on the claim map.
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30
31
32
33
34
35
36
37
38
39
40
41
42
43
44
45
46
47
48
49
50
51
CONTINUED
L 798818
L 798820
1798821
L798822
L798823
L 798824
L 798825
L 798826
1798827
L802477
L802479
1802482
L 802483
L802484
L 802487
L802488
L802489
L 802490
1802491
L802492
L802493
L802496
L802497
L802498
L 802501
L802539
L802541
L 806020
L806021
L806022
L806023
L806024
L806025
L806026
L806027
L806028
Number of Claim Units. For other mining land, list hectares.
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
-1— 3 —— i ^ , ,
Value of work performed on this claim or other mining land.
851,297
SO
SO
SO
SO
SO
:sososososososososososo
' ^'Ptf "P? t9(T•Xo
1 I SO
1 f SO
1 f 90
1 | SO
1
1
1
1
l sosososo
, L _____ , jo
.rRECEWhlT M-^ —— FttTHr
1 GEOSC (ENl*AL--— ̂^"
1
1
ir-p^ SO
so.ShSSMENT ————j, — —— —— SO
soso
Value of work applied to this claim.
S4.400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
Value of work assigned to other mining claims.
S30.800
SO
SO
SO
SO
SO
SO
SO
SO
SO
sososososososososososososososososososososososososososo
Bank. Value of work to be distributed at a future date.
S20.497
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
sososososososososososososososososososososososo
Colunn Totals l (continued ...) S18.800 830,800 S20.497
Ontario MnWryofNorthern DovctopmoniwdMnrn
Schedule for Declaration of Assessment Work on Mining Land
Transaction Niober (office use)
Mining Claim Number. Or if work was done on other eligible mining land, show in this column the location number indicated on the claim map.
52
53
54
55
56
57
58
59
60
61
62
63
64
65
66
67
68
69
70
71
72
73
74
75
76
77
78
79
80
81
82
83
84
85
86
87
CONTINUED
L806029
L806030
1606031
L806032
1806033
L950207
L950208
1950209
L950210
L950217
L950218
L950219
L 950220
L950221
L950222
L950223
L950224
L950225
L950226
L 950242
L950243
L 950244
L 950245
L950246
L 1206695
L 1206696
L 1206697
Number of Claim Units. For other mining land, list hectares.
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1 D1 * y ,•^iiiiiiii
Column Totals
Value of work performed on this claim or other mining land.
S51.297
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
sosososo
3 ————— -r ̂ Q -t7 Oso
——— *ysososososososo
REut.., . MAY- 4
——— QE03CIENCE OF
Value of work applied to this claim.
S18.800
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S400
S1.600
S400
:IVED'i - r-D
^COtdOMtN 1ICE
Value of work assigned to other mining claims.
S30.800
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
sososo
sosososososososososososososo
Bank. Value of work to be distributed at a future date.
S20.497
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
SO
so
so
soso
so
soso
so
so
sosososo
sososo
S5 1,297 S30.800 S30.800 *20,497
Ontario MnMiyofNorthwn DcvtlopnwnlandMnm
Statement of Costs for Assessment Credit
Transaction Number (office use)
LO rt c/ 20- C O
Personal information collected on this form is obtained under the authority of subsection 6 (1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Act, this information is a public record. This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.
Work Type
Pentland Wages
Data Compilation/Drafting
Contractor Costs
Assay Samples
Units of work Depending on the type of work, list the number of hours/days worked, metres of drilling, kilometres of grid line, number of samples, etc.
31.5 days
2.5 days
862 metres
230 samples
Associated Costs (e.g. supplies, mobilization and demobilization).
Saw Blades
Supplies
P•^ . JTransportation Costs -*. ,
Truck Lease
Gas S Truck Supplies
Food and Lodging Costs
Cost Per Unit of work
5233/day
5247/day
543.11/metre
511.75/sample
9 *9 9
Total Value of Assessment Work
Total Cost
57,340
S617
537,161
52,703
52,784
583
5289
5320
K 1,297
Calculations of Filing Discounts:
1. Work filed within two years of performance is claimed at 100X of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 50X of the Total
Value of Assessment Work. If this situation applies to your claims, use the calculation below:
TOTAL VALUE OF ASSESSMENT WORK x 0.50 = Total S value of worked claimed.
Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.
Certification verifying costs:
I,
Declaration of Work form as
, do hereby certify, that the amounts shown are as accurate as may reasonably
•red whi
,.A-(please print full name)
be determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying
Q eco
I am authorized to make this certification.____________________ (recorded holder, agent, or state company position with signing authority)
RECEIVEDMAY 1 4 1333
GEOSCIENCE ASSESSMENT OFFICE
OntarioMinistry of Ministers duNorthern Development Developpement du Nordand Mines et des Mines ___
Geoscience Assessment Office 933 Ramsey Lake Road
June8, 1999 6th FloorSudbury, Ontario
Kathryn Andrews Smith P3E 6B5PENTLAND FIRTH VENTURES LTD.BOX 1690 Telephone: (888) 415-9846HIGHWAY 101 EAST Fax: (877)670-1555SOUTH PORCUPINE, ONPON-1 HO Visit our website at:
www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm
Dear Sir or Madam: Submission Number: 2.19499
Status Subject: Transaction Number(s): W9980.00315 Deemed Approval
We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.
If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.
Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the . response date on the summary.
If you have any questions regarding this correspondence, please contact Steve Beneteau by e-mail at [email protected] or by telephone at (705) 670-5855.
Yours sincerely,
ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section
Correspondence ID: 13870
Copy for: Assessment Library
Work Report Assessment Results
Submission Number: 2.19499
Date Correspondence Sent: June 08, 1999
General Comment:
Assessor: Steve Beneteau
Transaction NumberW9980.00315
First Claim Number12096
Township(s) 1 Area(s)MICHAUD, GUIBORD
StatusDeemed Approval
Approval Date
June 08, 1999
Section:16 Drilling PDRILL
Correspondence to:Resident Geologist Kirkland Lake, ON
Assessment Files Library Sudbury, ON
Recorded Holder(s) and/or Agent(s):Kathryn Andrews SmithPENTLAND FIRTH VENTURES LTD.SOUTH PORCUPINE, ON
Page: 1Correspondence ID: 13870
o o
IoHE
4(xl 1"
10
76P677
763690
7836/S
7B3679
.783683
7B36B4
7836SO
lj ?' ' \ - 7 53661 l
7836S17S3682
"B1&307
4O
UQ4&6
^94999
l803^32 A-
804507
783685
7S3S65
j
7S3663
12
/Vt
361
'59378^;?!. 783664
i '734g 97 l 794994
l \
7S4996 l -!',794995 ;
rt'
,J V
80450S J 8045C3
804636- -l-
783567
40010
Mccool.
.'40 Q Tt
1228390
1227472 l
i i1227473
'X0012
TV)
283666
803S1B
,.-)A.-^lV XJ - Qi"*"^
S03916
8U3S06 ,'
i J "^ - "~ ~-
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•"x:\ .-^-4--
ti 03899 t VOUJi
! V804439 l 804494 [ E03B93y
-^ - l80449S\ ' 8C44S5If"\
S03393
303894,
803907
\
803909
80389
80390E
8038S4
803B90
••l——----
803BS5
304505,..S04504
i 80&033 l
10 ~- :-~JK~ ̂ i"" ~ ~ ~7 "i
-- - * ' i, 8060?? l ('!|OGQ;
BO
44245 J -
v
1
804497 t 804496
l
.. — --L.—— --~
•'30389.5
806031 1106029 ,-
97S908
979903
l579902 l
l
S7S9Q4
979^)1/'
80602?
44243
806020
S06021
5S6497
8G6028/
S03SSS 803886
8038.88
9502(7 950246'
— _ —'_ i ' _ _ _ _ _ —^ -^
950220 l 950219
,^T:::yT~ ^ ~ ~~" T "*
1 586496 l 536435
409C&r
3D3BC7
1 603904
— ——ir
1204455,X
'i*'
535961
O-ITAC
.f 03901
303883 .6038SO'A. lo-'
303900l
i
8496S7'' 649664 i
849666849665
803362 0^71,803331
950243
950245
40S10 40912^
l
950244]
979895)''' i 979896
979891 l l
'l'
402&6
40^51
079833
973345
979 E
5S6493 53'64S4 " I B
1586490
4514j
l
979897 j S79898 l
979B66 i 979867 l l
- t979894 979S6G
586486
97986S l 979841
^..|..---f
979816 l 979B17*
40313
vi.
'84389M . 843'eS'Sl,
v^- r-,^'' ft ^ ^•-843396 ^""^^
3.50242l
40916 /;ii
t
95C223
1206790 . 724903
1207486
' "^ .. . j- ^" t
CO
1227773
24904 ' 724909
•'724905 724908
\724S14i7249,10 l\ i
l i
——— - —————— ---.--f!— ———.-—— —^ -
24906 724907
8496S3849660
v
,J 343661.
843899\ 6439CO
i 49658
843901 843902
/r. ,--
950710
\
l "050226*1 950209
l 950224 ll
M9282
X
"^^ 40923 ,, r^Mtftoftds
|,'f it^ ^a*si) 4C929*
40014C
\4091 B :
— -(--Y- ——
45151 l /-45162 l , ^51 ^* i y ^
4.^233521412 H 521415 ^''5214 W
—
l
556484
521413, L
521414
521416
—-T 1
521419
y79844
97987S
521420
979870
9/9875
979846 979847 979848 979949l
979880 | 97987997987^'
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979654
• w-^j^-4-'i"T:;i"W'-r-z^i-"--ir l ^-- —^ -.
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i979BS1 979832
r M
979883
4D920
j LW i
45154 J
521427 G214P8I521421
l M- -_____i— — — — —^ —^ -i-
\521423IB
979371 | 979872
40930'
*'40928
451Sfi 451
7673477S7345
772746
1225544 1225545
1226791
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i l' Ltlilf '8-19656
7249 l 2 739293
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-*'. V.
949284 949?85
i 40931'40933
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39290
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i^z\
94607946068 V*-
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946067 M.-945066'
r i59'
l1Q47184 l 1047163
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"\———— l ——————
l, 1-023102 | 1029101''J"\ !,
H .j. — _ _ ̂ j 946064.
946065
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739304
t '' 95,02 *fc /' 960248 l j. l950247
r l
•t x9492^3
t- — ...— -
l 94)6291l
'" 949294
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3892S
.38493 l •' * l
i "l l ? ' lV l J . l - i ^
40932
45158 45159
1 521397 l 52139Bp. f mm i -
772976
1235312
1235309
1224)673''
12267B4od. 'lCO
772747
772975
772748
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Ontario
Ministry ofNaturalResources
Ministry ofNorthern Developmentarid Mines
INDEX TO LAND DISPOSITION
PUN
G-3682TOWNSHIP
MICHAUD
M.N^.ADMWIITRATIVf DISTRICT
KIRKLAND LAKEMINING DIVISION
LARDER LAKEUNO nTUIS/HIOISTHT DIVISION
COCHRANE
•CM)* 1:20 000
t Md 1HOM*w* r- r
i ODD a MHO TOM mo HW) ISAM
CentourlnHmnl 10 M*IFH
AREAS WITHDRAWN FROM DISPOSITIONMRO- Mining Flights OnlySRO- SurfacnPHgn(sOnlyM +S - Mining and Surface Righta
SYMBOLS Sec. 42OrMrNe DM*
R.S O. 60 SROFHf
1645S6
Boundary Township.!
Rami allowance, nurvsyad... stxxa-ine
Lot/Concaaalon - surveyed .unsurveyed
Parcel,
Rlghl-Qf-way; road . , railway utility..
Reservation . . . . . .
Cliff, PU. Pile . . . . . . . . - .
ComourIntarpalalAd
Depression
Control point (hprunntfll) .
Flooded land . . . . . . . . . . . . . . . . . . .
Mine nead (rarra . . . . . . . . . . . . . . . .
Pipe! i ne (above ground) . . -, .. .
Railway; *inflla track.doubl* truck . . . . . . . . . . . . . . .
.. A
...,. a
^t*—.... ^...——^..
Hoad highway, county, township
trail, buah . , . . . . . , , . . . . . . .
Shoreline (ordinal) . . , . . . . . . , . . .
Transmission Mire . . . . . . . . , , . . , .
DISPOSITION OF CROWN LANDSPntwit
Surface i Mining Rtghls Surface Rlghra Only . . . . . Mining Rights Only . . . . . .
Surface l Mlnlno RlQhtfiSurface Rights Only . . . . . Mining Rights Only . . . .
Licence of OCCL patton . . . .
Ordor-ir-Council
Cancelled , . . . . . . . . . . . . . .
Reservation . . . . . . . . . . . . . . ,
Sand ft Gravel- . . . . . .
. .63T
OC
Map base nnd Ipnrt dlBposriion drafting by Survaya and MappingBmncfi, M(nisiry of Matural
The dispasilion al land, location aflat fabric and parcnl boundaries on this Index was comp led lor administrative purposes anl/