PIFHER RESOURCES INC. 42E13SW2010 2.22558 TYROL LAKE 010 DIAMOND DRILL HOLE SUMMARY HOLE NUMBER: FC-01-01 :OMPANY PROPERTY FIELD GRID LOCATION SURVEY LOCATION AZIMUTH DIP SPERRY SUN TESTS CASING ___ CORESIZE^ LENGTH^OFJIOLE DRILL CONTRACTOR DATE STARTED DATE COMPLETED LOGGED ^ CORE STORAGE 'ifher Resources Inc. "orge Creek North East TB 1Z37683 _ _ VLF EMtargetat471 North L 31+25E L31+25E 5+43N METHOD OF COMPLETION ISO 0 -45 0 @ 75m -47 0 on tube/38-5 0 (corrected) @ 150m -48 0 on tube/39.0 0 (corrected) @ 177m -48 0 on tube/39.00 (corrected) 4.1 metres (pulled) 1 77.0 metres Major Dominik Drilling August 18, 2001 August 20, 2001 Armen Chilian Tyrol Lake Camp Standard core barrel and short shell. SULPHIDE MINERALIZATION METREINTERVAL From To STRATIGRAPHIC and STRUCTURAL INTERVALS From (metres) 0.00 ^ _ 4JO ___ 75.54^ 149.48 173.68 To (metres)^ 4.10__ ^ ^5.54__ 149.48 173.68^ 177.00 Page l of l DESCRIPTION DESCRIPTION Casing TuffjX:hloritk) ^ Porphyry (Feldspar) Porphyry (Amphibole) Lapilli Tuff RECHVE& GEOSCIiWGi ASSiSSMEN _____OFFICf__
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DIAMOND DRILL HOLE SUMMARY FC-01-01 - Ontario · 2017. 1. 17. · Standard core barrel and short shell SULPHIDE MINERALIZATION METRE INTERVAL From To No check samples taken STRATIGRAPHIC
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PIFHER RESOURCES INC.42E13SW2010 2.22558 TYROL LAKE 010
DIAMOND DRILL HOLE SUMMARY
HOLE NUMBER: FC-01-01:OMPANY
PROPERTY
FIELD GRID LOCATION SURVEY LOCATIONAZIMUTHDIPSPERRY SUN TESTS
PIFHER RESOURCES INC. Project Name: Forge Creek North East Hole Number:
Date: August 19-20, 200 W X?/7/". Location:Logger: Armen Chilian /V^* ~^5^-^-
Primary FROM TO0.00
4.10
75.54
4.10
75.54
149.48
Secondary From To
0.00
6.80
19.25
28.60
6.8019.25
28.60
75.54
LITHOLOGY Detailed Description
CASING.
TUFF (CHLORITIC).Volcaniclastic varieties and mixtures with compositional and/or fragmental clast sizesdifferent throughout. Sections of similar textures and compositions are no more thanten metres in length.Prominently broken core.
Patchy fine-grained scattered pyrite mineralization within amphibole 70*, feldspar30* speckled pyroclastic (tuff). Core has a speckled appearance due to mmeuhedral feldspar crystals (white) standing out in contrast to darker matrix. Faintpink-orange hue due to minor postassium-feldspar. Patchy brick red hematite mostlyin proximity to very thin 11 mm crosscutting calcite veining.Overall consistent gray matrix with black-green amphibole and white to faint grayfeldspar crystals (mm) flattened (pressed) in an interwoven style of ash tuff throughout.Minor coarser grained sections (up to 0.6m) where matrix contains orange-pinkpotassic patches allowing black 1 -3mm angular shards to stand out (shards of thissize are patchy).Similar texture as last section with matrix becoming finer grained having overall darkgray appearance. Patches of black chloritized angular shards up to 1 2mm in length(rare). Bands of black amphibole and quartz-potassium-feldspar (up to 1 5cm wide)gradational to semi-abruptiy occuring in vicinity of very fine-grained areas (mostnotable 34.50m-54.35m). Patchy 5-20cm bands hosting medium-grained 1-2cmelongate black amphibole crystals, most in vicinity of orange iron stained calciteveined areas. Semi-abrupt yet slight gradual (50cm transitional area) into nextsection.
PORPHYRY (FELDSPAR).Faint pink tint within massive gray biotite-amphibole-quartz-feldspar matrix. Mm whiteeuhedral to subhedral feldspar phenocrysts throughout. In local patches it appearsmore like an ash tuff with stringy, wavey weakly chloritized amphibole crystalsalthough ii1mm thick are 1-2. 5cm lengths. Weakly to nonfoliated. Non-magneticexcept isolated pyrrhotite near biotite seams (especially 87.90m-88.1 1 m). Verygradual coarsening of feldspar phenocrysts to 1 1 0.50m- 1 1 6.40m where feldspar
spotted against a light gray feldspar (tquartz) matrix. Very minor thin ^ mmcrosscutting white carbonate veinlets. Trace pyrite and pyrrhotite in vicinity of localquartzicarbonate veins/veinlets.Quartz-carbonate vein with pyrrhotite spots and trace chalcopyrite (check sample).
FELDSPAR PORPHYRY.Dark biotite-rich mafic (with feldspar (and quartz?)) matrix with phenocryst *:1-3mmeuhedral to subhedral feldspar. Short section with very sharp, well defined contacts.
AMPHIBOLE-RICH GABBRO.Small interval equivalent to that observed earlier.
SILICIFIED TUFF.Glassy to vitreous gray with jagged spindly lenses throughout of various gray tonesindicating different chloritic tweak sericite alteration of tuff particulate beforesilicification. Silicification so intense that individual quartz crystals not discernableand ghosts of white feldspar crystals are barely recognizable.
AMPHIBOLE-RICH GABBRO.Dark gray spotted stubby mosaics of mm-sized chloritized amphiboles within gabbrosimilar to that observed earlier. Very sharp contacts.
ASH TUFF.Light gray, weakly foliated with 1 -3mm long fragments of quartz, feldspar and darkgreen chloritized material having discontinuous and overstacking mini-ribbonedappearance throughout. Weakly silicified. Non-mineralized. Very sharp contacts.
AMPHIBOLE-RICH GABBRO.)ark gray with black to gray mm mosaic chloritized amphibole interlocked crystalshroughout. Massive, non-magnetic; with minor white mm carbonate veinlets.
Scattered fine-grained specks of pyrrhotite and pyrite (trace). A gradual yet verydistinct decrease in mm-size to somewhat aphanitic to very fine-grained.
MAINLY FINE-GRAINED MAFIC VOLCANIC.Medium gray, locally foliated, fine-grained to aphanitic, non-magnetic mafic unit.
Within the first two metres, dark green bands with carbonate dots (mm) appear assmall pillow selvages. There are three distinct such structures, mafic unit is simplyine-grained with carbonate veinlets. By 49.00m mafic unit develops a massiveappearance as if to be a (very) fine-grained gabbro. From 60.00m area to end ofsection weakly foliated amphibole-rich no longer do amphiboles have spottedmosaic appearance but are more stubby and trend slightly along foliation.
ASH TUFF.Light gray, weakly foliated with 1 -2mm white to green-black, flattened to subangulartephra slightly 'mini'-ribboned adjacent to one another. Flattening of tephra 3-6: 1 .
QUARTZ VEIN (PYRRHOTITE, CHALCOPYRITE).White to glassy, weakly fractured quartz vein at the contact between tuff and gabbro.In contact with tuff, nonmineralized. A few splashes of pyrrhotite with tiny mmchalcopyrite specks (within pyrrhotite) in central area of vein. In contact with gabbro3mm-wide mineralized zone hosting pyrite, pyrrhotite and chalcopyrite.
FINE-GRAINED GABBRO.
Medium to dark gray relatively massive mostly fine-grained amphibole-rich gabbro,with local quartz veining. Trace of fine-grained pyrite.Small 1-3cm quartz veins hosting pyrite and pyrrhotite.
QUARTZ VEIN.White to vitreous weakly fractured quartz vein with discontinuous trains and veins ofmedium-to coarse-grained pyrite, splashes of pyrrhotite and specks of chalcopyrite.
Project Name: Forge Creek
Date: August 26-27, 2001Logger: Armen Chilian
Point data (fol, bed, cont.) Type Angle Metres
CA/FO
FO
CACA
CACA
45
42
2721
2124
43.40
68.97
69.2569.50
81.7586.68
Hole Number:
Location: Dip:
Interval data (struct, alt, surf, oxid) Type Angle "X. From To
Alteration: Sericitization Ser Silicification Sil Core: C Intensity Weak Wk, Moderate Mod: Strong Str Standard Sulphide Chalcopyrite Cpy; Pyrrhotite Po: Pyrite Py Blank: B Oxides Hematite Hem: Magnetite Mag: Specularite Spec
PIFHER RESOURCES INC. Project Name: Forge CreekDate: August 27, 2001
Logger: Armen Chilian
Primary FROM TO86.68 173.78
Secondary From To
130.80
132.12
149.69
152.39
131.67
132.26
152.39
153.11
LITHOLOGY Detailed Description
MAFIC VOLCANIC (CHLORITIC; AMPHIBOLE).)ark gray to black, weakly foliated fine-to very fine-grained mafic volcanic. Foliation
has obliterated most of the textures. Chloritization moderate. Local sections of highamphibole content, crystal size is consistently fine-grained. Splashes and specksof pyrrhotite and chalcopyrite occur throughout unit especially where quartz±carbonateveins and veinlets occur, (many check samples).
Very small lens of silicified and pyrrhotite mineralized ash tuff.
brecciated FAULT ZONE with carbonate/gouge mixture between angular fragmentsup to 3cm diameter. Trace pyrite.
Silicified porphyry with discontinuous 1-3cm ("dmm thick) lenses of pyrite andpyrrhotite mineralization throughout. Strongly foliated.
Amphibole-rich, medium-grained, weakly foliated gabbro with gradational fining ofgrain size (away from porphyry) into fine-grained foliated volcanic.
Alteration: Sericitization Ser Silicification Sil Core C Intensity: Weak Wk; Moderate Mod; Strong Str Standard Sulphide: Chalcopyrite Cpy; Pyrrhotite Po. Pyrite Py Blank: B Oxides: Hematite Hem. Magnetite Mag. Specularite Spec
PIFHER
Primary FROM TO
173.78
179.09
179.09
296.44
t RESOURCES
Secondary From To
160.08
167.92
179.09210.49
230.80
246.11
269.27270.00
160.70
168.22
219.00212.25
231.50
260.58
270.00273.00
INC.
LITHOLOGYDetailed Description
Black feldspar porphyry segment with white 1 -2mm feldspar phenocrysts. Thin mmgreen chloritic (1 cm-wide and ^mm thick) discontinuous seams throughout. Tracepyrite (fine-grained).Quartz vein with massive webbed pyrrhotite and minor specks of chalcopyrite.
WEAKLY SILICIFIED PORPHYRY.Black with white feldspar phenocryst up to 2mm, weakly foliated so as to slightlysmear phenocryst. Very weakly silicified. Trace pyrite and pyrrhotite.
RECRYSTALLIZED PILLOW VOLCANICS.Very sharp contact into light to medium gray, medium-to fine-grained ^1mm) chloriticvolcanic with minor seams of biotite. Very peculiar round bands (up to 2cm thick)appear as pillow selvages, some as from 185.00m-1 86.00m have white carbonatedots 1 mm haloed on both sides being amygdaloidal. Trace pyrrhotite and up to G.5%pyrite locally (particularly in gabbroic textured areas).Medium-grained recrystallized to gabbroic texture.Quartz vein, barren of mineralization with trailing 65cm quartz-feldspar porphyry.
White carbonate veining with pyrrhotite splashes and trace chalcopyrite and pyrite.
Well developed pillow selvages with accompanying white mm-sized carbonate-filledamygdules.Silicified porphyry with specks of pyrrhotite and/cr potassuim-feldspar altered.Local silicification and accompanying veining ^carbonate that carries high ratios ofchalcopyrrte:pyrrhotite (1:10). Highest proportionate amounts of chalcopyrite observedin drill hole so far. Veining does not follow foliation and is observed at several differentangles.
Project Name: Date:
Logger:
Forge CreekAugust 27-28, 2001Armen Chilian
Point data (fol, bed, cont.) Type Angle MetresCACA
FO
CACA/FO
FO
FO
FOFO
6151
43
42
45
50
6958
160.08160.70
168.08
179.09
193.70
233.00
269.69272.43
Hole Number: Location:
Dip:
Interval data (struct, alt, sulf, oxid) Type Angle "it From To
Structure: Fault Gouge: FG; Fault Zone: FZ Alteration: Sericitization Ser; Silicification Sil Core: C Contact Angle: CA Fracture Fill: FF; Fault Breccia: F bx Intensity Weak Wk, Moderate Mod; Strong Str Standard : S Schistosity SC Foliation: FO Mafic Flattening: MF Kink Band: KB Shear Zone SZ; Alteration Vein AVN Sulphide: Chalcopyrite Cpy; Pyrrhotite Po; Pyrite Py Blank: B Bedding BD Lamination LAM Fracture: F Crossfoliation XFO Vein VN, Vemlet vlt Oxides Hematite Hem; Magnetite Mag, Specularite Spec
PIFHER
Primary FROM TO
296.44
345.99
400.00
345.99
400.00
400.00
RESOURCES
Secondary From To
276.00
290.10
356.00379.91
388.47
390.17
284.67
296.44
357.00381.50
388.71
393.54
INC.
UTHOLOGYDetailed Description
Scattered quartz veining containing specks of pyrrhotite.276.30m-277.00m altered and strongly silicified volcanic.278.82m-279.50m silicified quartz-feldspar porphyry relatively barren of mineralization283.00m-284.00m local accumulation of pyrrhotite specks.Transition 'clastic' zone appears either fragmented or injected with carbonate. Weaklyoliated.292.00m-292.50m small contact zone between an apophyses sill of porphyry thatras clearly pierced and intruded into the volcanic. Minor pyrrhotite specks in clearsilicification contact vein.
FELDSPAR PORPHYRY (SIL).Massive black to dark gray feldspar porphyry with 0.5-3mm feldspar phenocryststhroughout (25"*), the darker silicified matrix of amphibole-biotite-quartz and feldspar.Silicification locally intensifies. Crystals of quartz grains not visible due to glassycrossline nature of matrix. Isolated pyrrhotite specks.
FINE-GRAINED GABBRO.Dark green-gray massive non-magnetic fine-grained amphibole-rich gabbro. Matrixmainly of plagioclase and amphibole equigranular mixture. Throughout the sequence[2-4cm) white subhedral feldspar phenocrysts have developed (indicating the intrusivenature). Isolated pyrrhotite and pyrite specks.White quartz veining with cm-sized specks and splashes of pyrrhotite.Silicified (porphyry?) with accompanying quartz veins and minor slip planes whichhave not developed breccia or gouge.Feldspar porphyry sill with fused yet sharp contacts with gabbro. (Porphyry clearlyhas intruded into gabbro, coarse-grained size in centre and slightly smallerphenocrysts in contact with gabbro).Altered/silicffied porphyry (ghost like in appearance after alteration with remnants ofthe protolith) becomes relatively unaltered (sharp contact) with somewhat equal grainsize (phenocrysts) down section, ends at very sharp contact with gabbro.
End of Hole.
Project Name: Forge CreekDate: August 28-29, 2001
Logger: Armen Chilian
Point data (fol, bed, cont.) Type Angle MetresFOFOFO
CAFO
CA
736361
2663
72
276.20279.15283.55
345.99355.95
356.50
Hole Number: Location:
Dip:
Interval data (struct, alt, sulf, oxid) Type Angle * From To
AMPHIBOLE-RICH GABBRO.Medium gray massive with mm-sized intercrystalline mosaic amphiboled (black spots)throughout matirx of feldspar-amphiboletbiotrte. Trace pyrrhotite. Minor white cross cutting carbonate and quartz-carbonate veins and veinlets.
ASH TUFF.Minor segment of light gray moderately foliated ash tuff with flattened -cmm thick times5mm gray to black chloritic and light gray to white feldspathic tephra.
AMPHIBOLE-RICH GABBRO.Similar to that seen earlier at 2.00m-1 5.30m.
QUARTZ VEIN.Mainly vitreous quartz vein with splashes of pyrrhotite observed throughout. Minorsmall specks of chalcopyrite.
ASH TUFF.Light gray moderately foliated with white feldspathic to dark gray chloritic tephrafragments •Jlmm times up to 15mm in width. Isolated specks pyrite.
AMPHIBOLE-RICH GABBRO.Medium gray-green with dark green-black weakly chloritized amphibole crystalsappearing as mosaic dots throughout. Scattered small specks of pyrrhotite (trace).
FELDSPAR PORPHYRY.Light gray feldspar±quartz and minor amphibole crystals of a matrix which is dotted by1 -2mm euhedral to subhedral feldspar phenocrysts. Moderately foliated. Isolatedpyrrhotite specks.
AMPHIBOLE-RICH GABBRO.Dark gray-green with black mm-sized amphibole crystals dotted throughout. Massiveand relatively featureless aside from a few white carbonate veinlets.
with gray slightly flattened carbonate specks (2-3mm) throughout. Minor thin gray towhite carbonate veinlets the thicker variety *2mm hosting thin seams of pyrrhotite.
FELDSPAR PORPHYRY (AMPHIBOLE).Black with white specks of -:1-2mm gray to white subhedral feldspar phenocrysts.'hroughout matrix dark green 1-2mm amphibole crystals (weakly chloritized) are
similarly visible.
WEAKLY MINERALIZED MAFIC VOLCANIC.)ark green-black fine-grained to aphanitic very weakly foliated mafic volcanic, similar
to 44.62m-51.47m but with notable increase of quartz veining hosting pyrrhotite splashes.Notable pyrrhotite, chalcopyrite and minor pyrite swirls, splashes and disseminationshroughout carbonate veining that crosscuts foliation.
MINERALIZED QUARTZ VEIN.Mostly vitreous, to white which has injected into volcanic in some areas (59.54m-59.87m)injections are several and penetrative which have mineralized the protolith. Quartz veinis weakly fractured. Contact angles not clearly defined yet when matched with vein inFC-01-06 from 81 .00m-86.00m the dip from surface is 55*. Pyrrhotite splashes alongwith accompanying chalcopyrite±pyrite is mostly concentrated along contacts or as areplacement near contacts of quartz vein and volcanic protolith.
MAFIC VOLCANIC.Black, very weakly foliated to massive non-magnetic mafic volcanic relatively barren ofmineralization. Minor carbonate streaks.
End of Hole.
Project Name: Forge Creek
Date: August 30, 2001Logger: Armen Chilian
Point data (fol, bed, cont.) Type Angle Metres
FO
FOFO
46
6364
44.57
54.2955.13
Hole Number: Location:
Dip:
Interval data (struct, alt, sulf, oxid) Type Angle 'ft From ToVNVN
We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.
At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.
If you have any question regarding this correspondence, please contact STEVEN BENETEAU by email at [email protected] or by phone at (705) 670-5855.
Yours Sincerely,
Ron GashinskiSupervisor, Geoscience Assessment Office
Cc: Resident Geologist
Metalore Resources Limited (Claim Holder)Pifher Resources Inc. (Assessment Office)
Assessment File Library
Pifher Resources Inc. (Claim Holder)
Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16731
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MINING LAND TENURE
MAP
Dale I Time of Issue JUD 12 2001
TOWNSHIP f AREA
TYROL LAKE AREA
14:58h Eastern
PLAN
0-0141
ADMINISTRATIVE DISTRICTS l DIVISIONSMining Division Thundir Buy
Land Titles'Rcgistry Division THUNDER BAY
Ministry of Natural Resources District NIPIGON
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