42A01NE0197 OP91-236 GRENFELL VALUER EXPLORATION - DIAMOND DRILLING 1991 010 During the summer and early fall of 1991, we, Vallier Exploration, drilled 781 feet of EX (7/8 inch) core on our Kapakita Creek claims in northeast Grenfell Township. The core came from six holes as follows: HOLE NO. VE91-1 VE91-2 VE91-3 VE91-4 VE91-5 VE91-6 FOOTAGE 2|7 feet 115 feet 76 feet 100 feet 105 feet 168 feet AZIMUTH DIP 45 0 500 45" 90" 45 0 45 0 3400 1800 O0 vert. 180" O0 CLAIM NO. 1112059 1112059 1169149 1169149 1169149 1169149 Hole VE91-1 was drilled to test a major east-west striking VLF anomaly (designated 'O') which had some associated magnetic activity in the region of the drill hole. This hole remained in cherty and/or graphitic sediments throughout its length. Disseminated sulphides were observed throughout the core with pyrite to 109fc in some sections and concentrated pyrrhotite bands of 6 inches at two locations. Assays on representative samples at five different locations in this core gave Zn highs of 1100 ppm and Cu highs of 200 ppm. Hole VE91-2 was drilled southward from the same set-up as hole VE91-1 in an attempt to define the southern edge of the sedimentary sequence. The hole was discontinued at 115 feet still in fine grained sediment. Suphide bands were detected over a six foot section (pyrite with some pyrrhotite) but most of the core was relatively free of mineralization. Hole VE91-3 was drilled to test a strong VLF signal on the south westward continuation of anomaly 'O' in claim 1169149. This region also had a strong parallel magetic anomaly and was subsequently shown by Maxi-probe EM analysis to have a strong associated conductor at depth. This hole was terminated at 76 feet due to repeated core blocking. Highly siliceous felsic volcanics made up the material in this hole. The hole terminated in fragmented felsic volcanics that contained pyrrhotite and some pyrite in the cementing interstitial chert-feldspar matrix. Hole VE91-4 was drilled vertically from the same setup as VE91-3 in an effort to determine dip of the structures in this region. The VLF data which we had were difficult to interpret. Subsequent Maxi-probe data suggest a near vertical dip for the conductive structures, in agreement with the results from this drill hole. Hole VE91-5 was drilled south from the same setup as 3 and 4 in an effort to determine the structure of the parallel magnetic anomalies in this region. This hole, mostly in poorly mineralized felsic volcanics, traversed a feldspar porphyry section (possibly a trachytic dike or sill) and within a few feet from this a micaeous dark phaneritic material (probably a lamprophyre dike).
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VALLIER EXPL DIAMOND DRILLING 1991 · VALUER EXPLORATION - DIAMOND DRILLING 1991 010 During the summer and early fall of 1991, we, Vallier Exploration, drilled 781 feet of EX (7/8
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42A01NE0197 OP91-236 GRENFELL
VALUER EXPLORATION - DIAMOND DRILLING 1991010
During the summer and early fall of 1991, we, Vallier Exploration, drilled 781 feet of EX (7/8 inch) core on our Kapakita Creek claims in northeast Grenfell Township. The core came from six holes as follows:
Hole VE91-1 was drilled to test a major east-west striking VLF anomaly (designated 'O') which had some associated magnetic activity in the region of the drill hole. This hole remained in cherty and/or graphitic sediments throughout its length. Disseminated sulphides were observed throughout the core with pyrite to 109fc in some sections and concentrated pyrrhotite bands of 6 inches at two locations. Assays on representative samples at five different locations in this core gave Zn highs of 1100 ppm and Cu highs of 200 ppm.
Hole VE91-2 was drilled southward from the same set-up as hole VE91-1 in an attempt to define the southern edge of the sedimentary sequence. The hole was discontinued at 115 feet still in fine grained sediment. Suphide bands were detected over a six foot section (pyrite with some pyrrhotite) but most of the core was relatively free of mineralization.
Hole VE91-3 was drilled to test a strong VLF signal on the south westward continuation of anomaly 'O' in claim 1169149. This region also had a strong parallel magetic anomaly and was subsequently shown by Maxi-probe EM analysis to have a strong associated conductor at depth. This hole was terminated at 76 feet due to repeated core blocking. Highly siliceous felsic volcanics made up the material in this hole. The hole terminated in fragmented felsic volcanics that contained pyrrhotite and some pyrite in the cementing interstitial chert-feldspar matrix.
Hole VE91-4 was drilled vertically from the same setup as VE91-3 in an effort to determine dip of the structures in this region. The VLF data which we had were difficult to interpret. Subsequent Maxi-probe data suggest a near vertical dip for the conductive structures, in agreement with the results from this drill hole.
Hole VE91-5 was drilled south from the same setup as 3 and 4 in an effort to determine the structure of the parallel magnetic anomalies in this region. This hole, mostly in poorly mineralized felsic volcanics, traversed a feldspar porphyry section (possibly a trachytic dike or sill) and within a few feet from this a micaeous dark phaneritic material (probably a lamprophyre dike).
Hole VE91-6 was drilled to extend the northward exploration of hole VE91-3 into the conductive region defined by VLF and by Maxi-probe. Disseminated sulphides are found in the felsic volcanics along the length of the hole. The major variation is the degree of fracturing of the fine grained felsic material which varies from massive, through fractured with minor displacement, to brecciated. Higher concentrations of sulphides, mainly pyrrhotite, occur at a number of locations within the core and one stretch of over 30 feet contains M09fc with a one foot section of over 509fc pyrrhotite. This region of sulphides corresponds roughly to the position of the VLF signal but well above (vertically) and south of the region of highest conductivity. The best assays in the submitted samples for this hole were Cu at 200 ppm, Ni at 150 ppm and Zn at 400 ppm.
VALLIER EXPLORATION KAPAKITA CREEK PROPERTY
1991
CLAIM NUMBERS AND LOCATIONS
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Nota : Dans cette formule, lorsqu'il designe des personnes, le masculin est utilise au sens neutre.
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Nota : Dans cette formule, lorsqu'il designe des personnes, le masculin est utilise au sens neutre.
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Nota : Dans cette formule, lorsqu'il designe des personnes, le masculin est utilise au sens neutre.
Ministry ofNorthern Developmentand Mines
Ontario
DiamondDrillingLog Complete this form and Fill in on
related sketch in duplicate. every pageHole No. Page No.
Drilling Company
Date Hole StartedC c -\. 2. H \
Date Completed
Exploration Co., Owner or Optionee
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® Mini tryo' , Ministere du Diamond Journal de Complete this form and
and Meirnes OPm S^SST Drilling forage au related sketch in duplicate. FilMn on every page
Qntario L oa diamant Remplir en deux exemplaires la Remplir ces cases a O9 presente formule et le croquis annexe chaque page
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f-9/-^Z-} l -t,6-}J-(,•7-5)- 1
Hole No. Page No. k Forage n" Page n 0
^ V^9;-6 o)Map Reference No. Claim No. N 0 de reference sur la carte N 0 de concession miniere
l ) f Q 1 *1 *3
Location (Twp. Lot, Con. or Lat. and Long.) Emplacement (canton, lot, concession, ou latitude et longitude)
Property Name Norn de la propriete
Sample Footage/Niveau de pre- levement de I'echantillon fen oieds)
From/De
^ Q
^3'83'
94^.'/o/ '; ffil '
/^S 9
/^2
To/A
5-0'
t*'
W*
94,So3'
MtQ'^/23
Sample Length Longueur de I'ecnantillon
Assays t/Analyses mineralurgiques
/y-v
H^/^ —
C- A
^
0204(03/91) *F0r features such as foliation, bedding, schistosity, measured from the long axis of the core. t Additional credit available. See Assessment Work Regulation.
*Exemples de caracteristiques : foliation, schistosity stratification. L'angle est mesure par rapport a I'axe longitudinal de la carotte. t Des credits supplementaires sont offerts. Consulter les reglements relatifs aux travaux devaluation. Nota : Dans cette formule, lorsqu'il designe des personnes, le masculin est utilise au sens neutre.