ONTEX RESOURCES LIMITED DIAMOND DRILL HOLE SUMMARY HOLE NUMBER: FY-03-01 COMPANY PROPERTY CLAIM ZONE FIELD GRID LOCATION SURVEY LOCATION AZIMUTH DIP ACID TEST CASING CORE SIZE LENGTH OF HOLE DRILL CONTRACTOR DATE STARTED DATE COMPLETED LOGGED BY CORE STORAGE METHOD OF COMPLETION Ontex Resources Limited Faymar ^^^^^^^^^^ HR1170 (l43.0 meters) Coincident IP-Mag hi drilling under blast pit (shear-quartz vn) L8400E, 4200' North 81 0 15.356'; 48 0 24.703' ISO0 -43 0 No tests! Runner said he forgot to take both tests (and this was the same morning when he was told to take tests at 143.00m and at 71.00m) ??? 6.0 m (pulled) NQ 143.0m Norex Drilling Ltd. July 23, 2003 July 25, 2003 Armen Chilian Old Faymar Mme, Deloro Twp. Standard core barrel; short shell. SULPHIDE MINERALIZATION METRE INTERVAL From To STRATIGRAPHIC and STRUCTURAL INTERVALS From (metres) To (metres) 0.00 6.00 6.00 64.25 64.25 93.50 93.50 112.29 112.29 117.15 117.15 128.82 128.82 143.00 Page 1 of 1 DESCRIPTION f\ •r-S DESCRIPTION CASING. ANDESITIC (MAFIC INTERMEDIATE) FLOW GABBRO ANDESITE FLOW (MAFIC INTERMEDIATE) TONAL1TIC INTRUSIVE w/n 'ANDESITE' (MAFIC INTE 'ANDESITE' (MAFIC INTERMEDIATE). MAFIC VOL (CHLORITE, EPIDOTEiCARBONATE). 42A06NE2034 2.27226 DELORO 010
49
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ONTEX RESOURCES LIMITED DIAMOND DRILL HOLE SUMMARY … · ontex resources limited diamond drill hole summary hole number: fy-03-02 company property claims zone field grid location
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Dark green-gray, non-magnetic, fine-grained, weakly fractured with epidote-carbonateveins and blotches downsection. Scattered fine-grained pyrite. Minor calciumcarbonate veining. Thin (3cm) pillow selvages most apparent from 23.00m-29.00m,
marked by light green-gray centres, mantled by dark gray to black outer areas.
Low angle ^10") sheared section, weak sericitic, moderate carbonate with carbonateveins hosting local accumulations of fine-to medium-grained pyrite. Most veins ^cmthick. Weakly fractured throughout. Semi-abrupt contact areas. NOTE: 53.00m-
56.00m contains five feet of ground up core as noted by drillers block.
SPOTTED MAFIC INTERMEDIATE 'ANDESITE' FLOW?Altered version of typical volcanic, in this area being weakly silicified with gray-buff-
green epidotetfeldspathic spots (^1cm-3cm diameter) hosting red hematitic stain incentral area. Section fractured throughout. Locally broken core. Last three metresare foliated with increasing intensity downsection. Section as a whole has scatteredfine-grained pyrite but check samples when accumulations with carbonate occur.
FINE-GRAINED CARBONATE-RICH INTRUSIVE (GABBRO?).
Dark green, non-magnetic, homogeneous, fine-grained having rapid and steady
effervescence with 10"7o HCL. Contacts are sharp yet foliation (in volcanic) bounded.
Dark gray-green, non-magnetic, fine-grained with minor carbonate veining especially
upsection area (foliated). Minor broken/fractured core throughout.
Moderately foliated, with bleached appearance due to feldspathic-epidote (minorsericite possible) and interstitial calcium carbonate veinlets parallel to foliation. Veryweak fine-grained pyrite mineralization mainly associated with (and found within)calcium carbonate veinlets. (Check samples only).
Point data (fol, bed, cont.) Type Angle Metres
CA FOFOFO
FOFO
104559
55
62
59
59.72
82.23
84.40
85.31
89.11
89.95
Hole Number:
Location:
Dip:
Interval data (struct, alt, sulf, oxid) Type Angle "/o From To
Spotted light gray, medium-grained 'quartzofeldspathic' lithology with 20-30"7o dark
green chloritized mafics. Quartz is fine-grained and intermixed with feldspathic matrix.(No apparent quartz eyes as 'stand alones'). Vuggy carbonate lenses especially in
first few metres of section. Fine-to medium-grained pyrite locally concentrated to 1 "/o.'Xenolithic fragments' appear as angular blocky 1-2cm x 1-5cm very dark overprints
of intrusive (occur from 105.00m-1 1 1 .00m) and may be a mafic solution phenomenon.
Contact area between volcanic and intrusive having slightly elevated medium-grained
pyrite mineralization (although no alteration). Amphiboles 0.5mm x 8mm (easilyvisible). Minor muscovite-chlorite sheen on isolated planes although no foliation inthis area. (Check samples only). No pyrite in volcanic at or near contact.
AMYGDALOIDAL MAFIC VOLCANIC.
Mixed contact area (no distinct contact angle) leads into dark green, non-magnetic,fine-grained volcanic with 2-3mm diameter light green-gray zoned epidotetcarbonate
amygdules. Pyrite very scarce. Minor crosscutting white carbonate veins. Quartz-feldspar-chloritized mafic amphibole dyke (quartz-diorite) with sharp uppercontact and quartz and vuggy carbonate-epidote blebby lower contact area.Scattered fine-grained pyrite crystals.
DIORITE.
Dark gray (tint blue) homogeneous, fine-to medium-grained. Plagioclase-rich (65"7o)with chloritized mafics (amphibole) making up bulk of remaining composition. Non
magnetic. Scattered fine-grained pyrite (Q.25%).Light gray (tint faint green), fine-grained equivalent of surrounding intrusive with very
little ^0"7o mafics. Possible weak chloritic overprint. Appears to be a 'pulse' in the
intrusives' history. Sharp upper contact and banded with quartzlfeldspar vein.Dark green chloritized fine-grained mafic volcanic with patches of diorite within. Sharpcontacts banded with quartz and feldspar within vein.
Foliated mix of diorite and mafic volcanic having mainly scattered medium-grainedeuhedral pyrite (check sample only)Dark gray, non-magnetic, fine-grained chloritized mafic volcanic with sharp contacts.Void of pyrite.
Project Name:
Date: Logger:
Faymar
July 29, 2003Armen Chilian
Point data (fol, bed, cont.)
Type Angle Metres
CA
CA
CA
CAFOCACA
35
28
35 3532
3542
152.32
158.34
159.94160.65
161.12161.63162.47
Hole Number:
Location: Dip:
Interval data (struct, alt, sulf, oxid)
Type Angle "/o From To
Py
Cb vn
Cbvn
Cbvn
Cbvn
Py
39
46
51
57
1
0.2
97.50
133.43
153.58154.71155.93
161.00
98.50
161.60
FY-03-03
Sample #
5510
1852
Hole Size: NQ
Az:
Type
C/S/B
C
C
From
97.50
161.00
Page:
Assay To Au g/t
98.50
161.60
0.02
Nil
2 of 4
Check Reassay
Au g/t Au g/t
Contact Angle: CASchistosity: SC Foliation: FO Mafic Flattening: MF Kink Band: KBBedding: BO Lamination: LAM Fracture: F Crossfoliation: XFO
Alteration: Sericitization Ser; Silicification Sil Core: C Intensity: Weak Wk; Moderate Mod: Strong Str Standard : S Sulphide: Chalcopyrite Cpy; Pyrrhotite Po; Pyrite Py Blank: B Oxides: Hematite Hem: Magnetite Mag; Specularite Spec
ONTEX RESOURCES LIMITED Project Name: Faymar
Date: August 3, 2003
Primary
FROM TO
167.05
171.24
176.85
177.83
189.77
171.24
176.85
177.83
189.77
198.33
Secondary
From To
164.00 164.50
LITHOLOGY
Detailed Description
Light pink, very weak potassium-feldspar alteration in diorite locally with scattered fine
grained pyrite (check sample only).
PILLOWED MAFIC VOLCANIC.
Dark gray-green, non-magnetic, fine-grained to aphanitic with chloritized mafics spotted(1-4mm) throughout. 2cm thick pillow selvages clearly visible. Pyrite barren except for
minor carbonate with isolated fine-grained crystals.
'GRANITOID1 ALTERED DIORITE.
Faint pink-orange congealed (altered) spots against a quartzofeldspathic (fine-grained)matrix with approximately 25"7o amphibole and other (?) mafic phenocrysts (amphibole75"Xo, O.Smm x 6mm) other (2mm x 4mm spots, 25"Xo). Check sample of section
with elevated pyrite. Section is very hard (weakly silicified throughout). Consistentpatterns of fracture throughout, almost a weak foliation, best viewed 1 72. OOm-1 73.00m.
AMYGDALOIDAL MAFIC VOLCANIC.
Medium green-gray, aphanitic to fine-grained, non-magnetic with dusty beige calcite
amygdules inundated throughout. Relatively barren of pyrite except for minor cross
cutting carbonate veinlets. First 25cm is broken/fractured core.
ASSIMILATION AREA: ALTERED DIORITE and AMYGDALOIDAL MAFIC VOLCANIC.Patches of both epidotized diorite and amygdaloidal mafic volcanic throughout in an area
of mix and assimilation. Minor pink-red hematite staining in cross veining ±beige felds pathic material. Sharp contact of end of section.
DIORITE (LOCALIZED SILICIFIED), EPIDOTE.
Light to medium gray-green, weakly epidotized, locally weakly silicified; mm creamfeldspar and 1 mm x 5mm (largest) amphibole phenocrysts. Local orange-brownpotassium-feldspar alteration (196.08m-198.33m). Minor xenolithic fragments (2cm x
3cm) especially 192.00m-1 93.00m. Last 20cm of section foliated with abrupt terminationat quartz-carbonate veining.
Dark gray spotted translucent matrix with fine-to medium-grained quartz+feldsparcrystals. Dark green chloritized mafics mainly amphibole crystals 25-30"Xo are up to1 mm x 6mm in size. Weakly fractured with rusty fracture planes or as spots on core.
Minor (^"/o) xenoliths (mafic volcanic). Fine-grained disseminated pyrite (1.507o)
somewhat consistent throughout. Foliated contact at end of section.
28.15m-30.74m: broken/fractured core.31 .10m-31 .34m: dark green chloritized mafic volcanic with blebby quartz contacts.Likely caught as wallrock and left a xenolithic chunk.34.12m-37.13m: broken/fractured (ground core locally).37.32rn-38.31rn: possible transition zone. Upper contact foliated. Weak foliation of
crystals (coarse-grained) throughout blebby section. Very sharp lower contact.
FINE-GRAINED DIORITE.Speckled dark green homogeneous with 4507o chloritized mafics (predominantly
amphiboles) against gray plagioclase-rich matrix. Non-magnetic. Scarce pyrite
(trace). Lower contact obscure (rusty).
QUARTZ DIORITE.
Dark gray spotted fine-to medium-grained having 3007o chloritized mafics. Unlike
24.28m-38.31m, only local fine-grained pyrite along select low angle (all ^0" to core
axis) hair thin fractures (and only accumulating up to 1 0Xo in one area 49.77m-50.33m).Check sample. Dark green fine-grained non-magnetic xenoliths of chloritized mafic
volcanic (up to 2cm x 3cm) scattered throughout (O.2507o). One main set of cm thickquartz and/or carbonate veins throughout - every 1 0-20cm, all of which contain no
pyrite mineralization.Light gray-green 'bleached' hues of feldspathic alteration at borders of lower angle^45") quartz±carbonate veinlets. Hues mantle these low angle (veins cm or less inthickness) for several cm beyond the vein. Slight elevation in pyrite mineralization in
this area. One quartz vein in particular 84.86m-84.95m hosts coarse-grained pyritemeshed crystals (pyrite is classic pale brass - not golden).
Alteration: Sericitization Ser; Silicification Sil Core: C Intensity: Weak Wk; Moderate Mod: Strong Sir Standard : S Sulphide: Chalcopyrite Cpy; Pyrrhotite Po; Pyrite Py Blank: B Oxides: Hematite Hem: Magnetite Mag: Specularite Spec
ONTEX
Primary
FROM TO
99.07
102.80
113.00
102.08
113.00
113.00
RESOURCES
Secondary
From To95.61 99.07
LIMITED
LITHOLOGYDetailed Description
Minor 'bleached 1 hues, grainy to blotchy textures decrease in quartz-feldspar contentand increased mafics and areas of very fine-to fine-grained pyrite mineralization with
a trace of chalcopyrite. No apparent mineralization trend, most in area of silica
Rounded blobs (to 50cm) to cm angular fragments of dark green chloritized fine
grained, nonmineralized mafic volcanic intermixed with very dark green medium-
grained amphibole - feldspar dioritic rock.
•DIORITIC 1 (with MAFIC VOLCANIC ASSIMILATION).
Variable grain size, from coarse-grained 'salt and pepper1 with xenoliths of maficvolcanic to dark green, medium-grained for smaller ^Ocm patches. Cm to decimetresized xenoliths (largest in last metre of section). Weak fizz with HCL on matrix and
minor vuggy cm-sized carbonate veinlets. No quartz apparent in chloritized amphiboleand feldspar matrix. Entire section pyrite poor except for rare isolated incidentalvery fine-grained specks.
Alteration: Sericitization Ser; Silicification Sil Core: C Intensity: Weak Wk; Moderate Mod; Strong Str Standard : S Sulphide: Chalcopyrite Cpy; Pyntiotite Po; Pyrite Py Blank: B Oxides: Hematite Hem: Magnetite Mag: Specularite Spec
ONTEX RESOURCES LIMITED Project Name: Faymar
Date: August 8, 2003Logger: Armen Chilian
Primary
FROM TO
68.54
71.04
78.60
86.71
71.04
78.60
86.71
90.71
Secondary
From To
LITHOLOGY
Detailed Descriptionto core axis. Mainly swiried pyrite mineralization with carbonate but mainly associated
with hair thin fractures and carbonate veinlets. Most accumulation in siliceous brecciazone (64.85m-65.25m). Messy contact (weak flow brecciation) into next section.Note: 1899 is a check sample on mineralized contact - no mineralization above or
below.
QUARTZ DIORITE.Medium gray, fine-to medium-grained with 35-407a chloritized mafics, approximately
45"Xo plagioclase, approximately 70Xo interstitial quartz mixed with plagioclase andminor carbonate. Dark green fine-grained mafic volcanic xenoliths occur throughoutand get larger downsection. (Note: quartz most easily distinguished at end of
section (translucent gray-blue dots up to 4mm diameter)).
AMYGDALOIDAL 'ANDESITE1 MAFIC INTERMEDIATE.
Dark to medium green, non-magnetic, aphanitic with dark green to black chloritic spots(1-3mm) throughout. Individual pyrite crystals 1-2mm surrounded by carbonate halos
(amygdules) in central part of section. Patches of quartz diorite at beginning and endof section. One splash of chalcopyrite occurs at a cm-thick carbonate vein junction that
crosscuts quartz diorite near beginning of section. Outside of amygdules, section isfairly unfractured, therefore no chrysotile veinlets and stringers, therefore no swirled
pyrite mineralization.
QUARTZ DIORITE.
Gray with dark green chlorite spots (1-3mm) 35-40"Xo and scattered dark green
aphanitic mafic volcanic xenoliths. Very minor fracture-fill white carbonate veinlets(all angles to core axis) which do not contain pyrite and in an isolated incident containsa mm speck of chalcopyrite (82.80m). Blebby lower contact. (Xenolith at 83.32m-
Dark green, non-magnetic, aphanitic with calcite rimmed vesicules to calcite-filledamygdules dotted throughout. Weakly fractured with white carbonate hair thin veinletsS-7% throughout. Pyrite crystals associated with amygdules only.
Speckled dark green-black chloritized mafics (25"Xo) against a lime green sauseritizedplagioclase-rich, (and interstitial quartz) matrix. Plagioclase crystals easilydistinguishable. Very minor fractures yet very distinct cm-thick quartz-carbonate
veinlets (the only outstanding feature of this unit other than the lime green colour).Up to /"/o quartz, somewhat stripped appearance. Minor (O.50;4) very fine-to fine grained pyrite crystals. Isolated chalcopyrite occurring as mm specks in one quartz-carbonate vein (96.87m-96.88m). Vein is offset dextrally by 0.9cm. Cm-sized mafic
volcanic xenoliths.
•ANDESITE' MAFIC INTERMEDIATE (AMYGDULES) with QUARTZ DIORITE BLEBS.
Dark green-gray, non-magnetic, aphanitic amygdaloidal flow with patches of intrudingsauseritized quartz-diorite. Hair thin fracture-fill carbonate veinlets truncate both
lithologies. Within volcanic flow minor (up to 2"7o within 10cm interval) accumulations
of pyrite mineralization.
ACTINOLITIC GABBRO.
Green actinolite needles up to 4cm long (40"Xo of lithology is actinolite); no fracture,
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
ONTEX RESOURCES LIMITED Project Name:
Date: August 21, 2003
Primary
FROM TO
67.97
85.90
85.90
111.85
Secondary From To
49.80
55.43
65.92
72.30
72.63
92.00
111.45
55.43
59.00
67.97
72.63
85.90
110.37
111.85
LITHOLOGY
Detailed Description
Mostly broken core consisting of black fine-grained serpentinite separated by intervals
of spotted serpentinized pyroxenite.Blebs of a gray-beige, soft (scratched easily with knife) tremolitic gabbro phase with
easily distinguishable boundaries against the black fine-grained serpentinite. Non magnetic, weak fractured appearance, (this interval is less broken than surrounding
serpentinite). No pyrite.Dark green-black serpentinized pyroxenite. Tremolite (gray) along fractures. Trace
fine-grained pyrite, non-magnetic.
SERPENTINITE (SERPENTINIZED PERIDOTITE).
Black-green, coarse-grained with fibrous habit along fresh breaks. Crosscutting white75"yo and green 257o chrysotile veinlets (-^lO"/)) (locally symmetrical) and tiny grayseams tremolite (up to 100Xo) giving core a gray webbed overprint due to its abundance.
Very consolidated. Non-magnetic becoming magnetic downsection. Trace pyrite aswispy fine-grained specks, (no chalcopyrite or pyrrhotite). Local white calciumcarbonate veining. Blue-green variety of chrysotile apparent in magnetic section.Low angle (14") tension gash with minor calcium carbonate. Separates non-magnetic
(upsection) from magnetic section.Very fine-to medium-grained magnetite specks (approximately 3 0Xo) yet magneticoccurs as more prominent mm-thick bands of concentrated mineralization which is a
progression from scattered crystals to consolidated accumulations (into crude mm-thick bands) downsection. (Enough of section sampled for a thorough "check").
CUMULATE TEXTURED SERPENTINIZED PERIDOTITE.Less green and more black than last section progressing into well defined pervasive
white to beige seams (0. 5mm) of chrysotile replacing cumulative olivine. Lessconsolidated downsection with local broken core. Approximately 67e very fine-grained
magnetite. Trace fine-grained pyrite.Area of strongest and most prominent cumulate texture of chrysotile with a sky blue-
green variety.103.70m-105.20m: broken core.Transition area marked by FAULT GOUGE between serpentinized peridotite with
cumulate texture and fractured serpentinized peridotite.
Logger: Armen Chilian
Point data (fol, bed, coni.)
Type Angle Metres
FB 61 87.20
Hole Number
Location:
Dip
Interval data (struct, alt, sulf, oxid)
Type Angle "/o From To
FG
PyChr vnlt
TGChr vnltCbvn
Mt
FG
30
59
14
31 38
30
Ir
3.5
56.34
67.97
72.90
72.30
75.62
81.29
72.63
110.37
56.35
74.00
72.63
85.90
110.45
FY-003-06 Hole Size:
Az:
Type
Sample* C/S/B From To
1919
1920
1921
1922
1923
1924
1925
1926
1927
1928
1929
1930
1931
1932
1933
1934
1935
1936
65.00
66.00
67.00
68.00
69.00
70.00
71.00
72.00
73.00
74.00
75.00
76.00
77.00
78.00
79.00
86.00
89.00
92.00
66.00
67.00
68.00
69.00
70.00
71.00
72.00
73.00
74.00
75.00
76.00
77.00
78.00
79.00
80.00
87.00
90.00
93.00
Page:
Assay Aug/t
Nil
0.01
Nil
Nil
Nil
Nil
Nil
Nil
0.01
Nil
Nil
Nil
Nil
Nil
Nil
Nil
0.01
0.01
2 of 3
Pt Pdg/t g/t
0.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
0.01
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
O.005
0.005
^.005
O.005
0.005
Contact Angle :CASchistosity: SC Foliation: FO Mafic Flattening: MF Kink Band: KBBedding: BO Lamination: LAM Fracture: F Crossfoliation: XFO
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
ONTEX RESOURCES LIMITED Project Name.
Date: August 22-23, 2003
Logger: Armen Chilian
Primary
FROM TO
111.85
117.48 l
130.00
-- — - -
——————
117.48
130.00
—— . . .
———— —
— - —
Secondary
From To
111.85
113.00
114.85
117.04
121.81
124.73
126.37
-- - -
- ———— -
--
113.00
114.85
117.04
117.48
123.10
125.74
126.34
-- ———
—— —
- ————
LITHOLOGYDetailed Description
VARIOUS LITHOLIGICAL INTERVALS AMIDST FINE-GRAINED and BROKEN CORE.
Low angle (0-10" to core axis) white fracture-fill veinlets of chrysotile within black to
black-green fine-to medium-grained moderately magnetic serpentinized peridotite.
Mostly broken core consisting mainly of serpentinized peridotite with chrysotilefracture-fill veinlets and clusters of muddy GOUGE which give a light fizz with HCL.
Where definable, GOUGE appears to cut across lithology at 9".
Black moderately magnetic, weakly fractured serpentinized peridotite.
Apple green and black mix of serpentine after olivine and antigorite, moderately
magnetic.
SERPENTINIZED PYROXENITE.
Black, moderately magnetic, fine-to medium-grained with 1 -2 mm-sized black spots
of antigorite that have possibly replaced pyroxene crystals. Blue-green shimmer of chrysotile on all sides of core when broken, therefore groundmass likely consists ofa mix of antigorite and chrysotile although texture is one of black congealed spots.Fine-grained magnetite 307o throughtout (note: white carbonate-rich vein fizzed with
HCL only when scratched).Green waxy serpentine-chrysotilelantigorite fractured mixture with 2-3mm crosscutting
chrysotile (asbestos) veins.Area of crosscutting green waxy serpentinetchrysotile veins.
FELDSPAR PORPHYRY.White euhedral 2-4mm plagioclase phenocrysts within a dark gray siliceous feldspathicgroundmass. Feldspar phenocrysts are zoned having a central 'dirty' beige-green coreand porcelain white exterior. Massive overall. Local fine-grained euhehedral pyrite(check samples). Non-magnetic.Phaze of gray soft (easily powders with knife) feldspathic material having mm black
mafics 3"Xo (some of which containing very tiny magnetite specks). Unit contains veryfine-grained scattered pyrite and chalcopyrite (trace). Check samples.Phenocrysts of feldspar much smaller than previous (mm) against a very dark graygroundmass. Siliceous contact into next section.
INTERMEDIATE INTRUSIVE.Gray overall with black anhedral 1-2mm mafic spots (2007o) in a soft (easily scratchedwith knife) feldspathic groundmass of medium-grained size. No quartz. (Mostcharacteristics display anintrusive in nature!). No fizz with HCL. A weak but pervasivetype of veining or seam is evident throughout, consisting of dark gray interior havingcrosscutting core axis between 25-35" (BND). Sharp contact into next section.
Non-magnetic.
FINE-GRAINED MAFIC PHAZE.Dark gray very fine-grained and relatively featureless. Homogeneous throughout
lacking magnetism. Appears black (chloritic on end of freshly broken core). Some what hard groundmass (quartz-feldspar±mafic). Veined contact.
WEAKLY SERPENTINIZED PYROXENE-PLAGIOCLASE GABBRO.
Medium green-gray, non-magnetic, fine-grained with relatively indistinguishable crystal
boundaries (which are interlocked or fused together in groundmass). Soft (easilyscratched with knife) matrix. White fracture-fill veins, some of which are calciumcarbonate, and chrysotile crosscutting at all angles to core. Trace very fine-grainedpyrite (check samples).Area of blebby seemingly antigoritic veins 3cm thick, fractured and crosscut by secon dary veinlets.
Alteration: Sericitization Ser; Silicification Sil Core: C Intensity: Weak Wk; Moderate Mod: Strong Sir Standard : S Sulphide: Chalcopyrite Cpy; Pyrrhotite Po; Pyrite Py Blank: B Oxides: Hematite Hem; Magnetite Mag; Specularite Spec
ONTEX
Primary FROM TO
27.10
33.80
42.59
33.80
42.59
56.22
. RESOURCES
Secondary From To
25.50
32.60
33.80
44.03 44.0647.98
53.57
54.52
25.80
33.80
35.66
44.06 46.5353.57
54.52
56.22
LIMITED
LITHOLOGYDetailed Description
Completely serpentinized (green waxy) section with spots of chalcopyrite. Local very
faint foliation throughout.
FINE-GRAINED MAFIC.
Dark gray, homogeneous, aphanitic and non-magnetic with gray-green, weaklyserpentinized groundmass. Nonmineralized. Broken core of serpentinized gabbro?
leads into the section (similar in featureless character as is 16.35m-20.24m).
(Both sections oddball and conspicuous). White quartz vein with chalcopyrite specks
at one location.Ground core.
SERPENTINIZED PYROXENITE.
Green-black, locally weakly magnetic ^0.5"7o very fine-grained magnetite) with green-gray chrysotile±tremolite inundating (250Xo) matrix. Very fine-grained pyriteO.50/!). Black pyroxene crystals appear partially altered to tremolite. (Check samples).
Foliation defined by chrysotile stringers.Non-magnetic.
SERPENTINITE.
Green-black fine-to medium-grained with green-blue chrysotile stringers throughout -
locally defining a foliation. Change from locally magnetic to consistently magnetic.
Chrysotile veinlets become thicker and fibrous character very apparent.Area of minor slippage (weak faulting) with three parallel quartz veins.
Coarse-grained serpentinite alteration.Consistently magnetic downsection (4-5"Xo very fine-grained magnetite), thicker
chrysotile stringers and veinlets and white wispy chrysotile±tremolite spots (mm-size)
gradually increase.Coarse-grained with peripheral gray tremolite and green chrysotile stringers. Fairly hard (scratches faintly with knife). Overall coarse-grained tremolitelchrysotile-pyroxene-plagioclase gabbroic rock that has undergone a moderate degree of serpentinization.
Serpentinite with 4-5"7o very fine-grained magnetite.
Project Name:
Date:
Logger:
Faymar
Aug. 25, 2003Armen Chilian
Point data (fol, bed, cont.)
Type Angle MetresFO
FO
45
45
25.55
34.43
Hole Number
Location:
Dip:
Interval data (struct, alt, sulf, oxid) Type Angle "/o From To
SERPENTINIZED PRYOXENITE.Black spotted mosaics of pyroxenes interwebbed by gray tremolite with green-blue
chrysotile stringers. Coarse-grained and weakly magnetic throughout entire section.Crosscutting veinlets ^mm to veins up to 3cm thick of green-blue chrysotileltremolite.1 .S-2% very fine-grained magnetite. Pyrite? Check samples only. A very subtle
crossalignment locally equals foliation.
Blue-gray chrysotile±tremolite fuzzy veins (no fizz with HCL) crosscutting at all anglesto core axis.
WEAKLY CARBONACEOUS SERPENTINIZED SECTION.Gradational contact into abundant (25Va) blue-gray chrysotilettremolitic wispyveinlets. Groundmass is predominantly light gray having green (40"7o) serpentine afterolivine and black (1507o) pyroxene crystals. Non-magnetic.
Broken and ground core.Soft (easily scratched with knife).
FELDSPAR PORPHYRY.Sharp contact into feldspar porphyry consisting of white anhedral to euhedral 2-4mmzoned plagioclase phenocryst^ and minor (5"Xo) black mafic specks ("d mm) against asmoky gray quartz-feldspathic groundmass (can't scratch with knife). Contact areaand section overall is nonmineralized. Rare pyrite.
Subtle weak foliation with groundmass slightly green and phenocrysts only 1-2mm in
size (70"7o) versus ^mm (257a).
FINE-GRAINED MAFIC PHAZE.
Sharp contact into dark gray to gray-green, non-magnetic, nonfoliated homogeneous
unit with white calcium carbonate jagged veinlets (4 07o) occurring locally in areas ofweak fracturing.
Minor very fine-grained pyrite and possibly pyrrhotite. Trace magnetite.Area of increased fracturing and subsequent fracture-fill veinlets of white calciumcarbonate. Main veining 28"-35 0 to core axis.
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,
/f-Ron C. GashinskiSenior Manager, Mining Lands Section
Cc: Resident Geologist
Ontex Resources Limited (Claim Holder)
Assessment File Library
Ontex Resources Limited (Assessment Office)
Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:19171
ThoM wishing lo stake mining claims should consult with the Provincial Mining Recorders' Office of the Ministry of Northern Development and Mines for additional General Information and Limitations Information on the status of the lands shown hereon. This map Is not Intended for navigational, survey, or land title determination purposes as the Information Contact Information: shown on this map ia compiled from various sources. Completeness and accuracy are not guaranteed. Additional information may also be obtained through the Provincial Mining Recorders' Office local Land Titles or Registry Offloa, or the Ministry of Natural Resources.
This map may not show unregistered land tenure and interests inToll Free Map Datum: NAD 83 la "d Including certain patents, leases, easements, right of ways, Tel: 1 (888) 415-984.5 ext 57ffbjectiom UTM (8 degree) flooding rights, licences, or other forms of disposition of right* and
Willet Green Miller Centre 933 Ramsey Lake Road Fax: 1 (877) 670-1444 Topographic Data Source: Land Information Ontario Interest from the Crown. Also certain land tenure and land uses Sudbury ON P3E 6B5 Mining Land Tenure Source: Provincial Mining Recorders' Office that r*51** or prohlbk free entry to stake mining dalms may not be
The Information shown la derived from digital data available In the Provincial Mining Recordera' Office at the Urns of downloading from the Mlniatry of Northern Home Page: www jnndm.gov.on .ca/MNDM/MINES/LANDS/mlamnpga.htrn illustrated. Development and Minos web site.
Date; Time of Issue: Mon Mar 29 10:26:43 EST 2004
TOWNSHIP l AREA PLAN DELORO G-3993
ADMINISTRATIVE DISTRICTS l DIVISIONS
Mining DivisionLand Titles/Registry DivisionMinistry of Natural Resources District
PorcupineCOCHRANETIMMINS
TOPOGRAPHIC
i Administrative Boundaria
i Township
; Concession. Lot
j i Provincial Par*
g;! indian Reserve
: "": CIKf, PillPite
Land Tenure
Freehold Pntenl
e
4
Contour
Mlno Shafts
Mlno Haadfnmo
Railway
ROM
Trail
Natural Oat Pipeline
UMira
Tower
f Jil SurflBO And Minint RWtt
nil Surface RloWt Onlyi-Sj["^'j Mining Rlghte Only
leosenold Palsnl
f-Tl Surface And MWnoRlohttL. "j;' ̂ , ; Surface Rlgnts Only
Order In Council Withdrawal Types WOT Surface And MMnj HW* Withdrawn W"l Surface RlgTili Only Wlthdmwri W"m Mining RlBfiB Only WltHdmim
IMPORTANT NOTICES
cab 1:4111*
LAND TENURE WITHDRAWAL DESCRIPTIONSIdentifier Type Date Description
8995 Ws May 19, 1966 Mining Claims Shown within this area ore subject to the Rights and Pitgranted to Delnlts Mines Ltd. under an Easement order dated May 16.
P.APLA Warn Aug 12. 2003 Pending application under tha Public Acts, Surface Rights Only W-P-05-04 Wsm Fob 3, 2004 Sec. 38 Surface Rights Only Feb 3, 2004 MNR Filnt 196180 W-P-12/92 Ws Feb 24,1892 W-P-12/9S NR Feb. 24,1682 SRO (Application under the Public