DIAMOND DRILLING REPORT NUGGET CREEK GROUP. Victoria Mining Division. NTS 92B/l.3W qm Ti.s' by A. J. Davidson May 25,
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1 0 wner: DIAMOND DRILLING REPORT NUGGET CREEK GROUP Victoria Mining Division NTS 92B/l.3W qm Ti.s' C orporation Falconbridge C opper 0 perator: C orporatlon F alconbridge C oppcr by A. J. Davidson May 25, Claims Little Nugget C he m &us B elk Dunsmuir Seattle Copper King C opper (1 ueen Queen Bee Alliance Fr. Patricia Jane Fr. Peggy Fr. Beatrice Iforley Jane Fr. Bonnie I Bonnie I Bonnie IJI Bonnie IV Bonnie V Bonnie VI CK I CR I GEOLOGICAL BRANCH ASSESSMENT REPORT
2 TABLE OF CONTENTS PAGE D?TK 0 DU C TI0 I? / Location and Access... Property... History... W 0 K K DONE... TECHNIC AL DATA... C 0 I? C L u SIO I? s... STATEIIEMT 0 F COSTS... STATEMENT 0 F Q IJALIFIC ATIONS... 2 / 2 / 3, 4, 5 / f
3 JNTK 0 DU C TI0 N Location and Access The Postuk-Fultton Option is I.ocated 1.3 km north of Duncan, B. C. on the northwest dope of Big Sicker Mountain. Access is by 2 wheel. drive vehicle (Fig. I.). Property The property consists of the follnwing contiguous claims (Fig. 2): Name Record # 11 onth Litde Nugget 1.3 January C he m ainus 1.4 January B elle 1.5 January Dunsmuir 1.6 January S e atde 1.7 January Copper King 1.8 January Copper Queen 1.9 January CR El ay CR II 930 FI ay Queen Bee 22 January Alliance Fraction 1.20 September Patrica Jane Fr. 83 I1 ay Florley Jane Fr. 84 El ay Peggy Fraction September Beatrice I. 21. September Bonnie 1: 41.5 September Bonnie I 41.6 September Bonnie III 41.7 September Bonnie IV 41.8 September Bonnie V ctober Bonnie VI ctober f
4 MINERAL RESERV CLAIM HT- SICKER MAP PROPCRT~ I%D-.Liza?. a - PF QpnoA) - i-5 LEMOC~ &?,or&& I: SO,OOO ~-.-_-.?..,... ~ _ :.... > ~ ~..... _.- ~
5 History The property is part of the Elt. Sicker Camp which has had a history of sporadic mining activity since The Tyee mine adjacent to the Nugget Creek Group produced 305,787 tons of 3/31.% Cu, 7.51.% Zn, oz/ton Au and 2.75 oz/ton Ag from The Nugget Creek Group was part of the lit. Sicker property when!it. Sicker!lines Lttl. was formed in In Ducanex made a reconnaissance geolngicd. map of the area and drilled 866 feet in two diamond drill. holes on the Queen Bee and Seattle claims. The claims were staked by the present owners Dr. P. Postuk and Elr. S. B. Fdton of Duncan and were optioned in by S.E.R.E.N. Ltd. S.E.R.E.N. geo1nogicall.y mapped, sofl. sampled and ran VLF and some DEEPEN on the property. They drllled 4 holes totalling 591. metres testing geoptiydcd. responses. S.E.R.E.N. dropped the option in when they pdled out of the entire Eft. Sicker area. WORK DONE (].7(January)). One diamond drill. hole has been completed on tlie Seattle Claim The hole was clrilled a total. of metres and was of BQ size. TECHNICAL DATA The hole was drilled to test the western strike extent of sd.pllide mineralization found 200 metres east of tlie Iiola. The hole encountered 35.4 metres of mixed andesite-rhyolite and then metres of quartz diorite. The hole was stopped at metres. Core is stored at Hykawy Road, Duncan, B. C.
6 -3- C 0 N C LUSIO NS The 't1ol.e (Lid not extend the previously known mineralization and encountered a substantial. thickness of quartz diorite. Further drllling wi73. be necessary to better define the geology. I
7 Y F. BOISVENU DIAMOND DRILLING LTD. C/O GRANVILLE STRJ3ET VANWER, B.C. V6H 3H4 INVOICE DATE: May 23, 1984 TO: Corporation Falconbridge Copper th Street Delta, B.C. v4k 4E2 I FOR: Surface drilling MfS -1 April 27 to April 30, 1984 Drilling ers nj hloving hlaterials Tropari testing
8 - 5- STATEMENT OF QUALIFICATIONS I, Alex J. Davidson hereby certify that: 1. I hold a Bachelor of Science Degree (Geology Major) and a Master of Science Degree in Economic Geology from McGill University, Montreal, Quebec. 2. I have practised my profession in exploration continuously since graduation. 3. I have based conclusions and recommendations contained in this report on knowledge of the area, my previous experience and the results of the field work conducted on the property. THUNDER BAY, ONTARIO. - ALEX J. DAVIDSON MSc.
9 -.... I HOLE NUMBER MTS 1 PROJECT Postuk-Fulton 1 CORPORATION FALCONBRIDGE COPPER DRILL HOLE RECORD x METRIC UNITS IMPERIAL UNITS GRID L Z DEP ELEV COLLAR COLLAR HOLE FINAL CFC GRID (1983) COORDS FIELD 3+12N BRNG 2o0 DIP -52 SIZE BX I I I I CLAM a SURVEY DATESTARTED PURPOSE 1) to test the strike project o the SRM 16 exhalite. 2) to extend the massive chlorite alteration trend located at surface. DEPTH 175.6m April 28/84 CONTRACTOR F. Boisvenu Drilling Ltd. COORDS N 2+22*8W DATECOMPLETED Mfid,184 CORESTORAGE Hykawy Road,CASlNG Yes Uuncan ROD LOG COLLAR SURVEY PULSE EM SURVEY ULTISHOT SURVEY ACID TESTS TROPARI TESTS MULTISHOT DATA DEPTH1 m I CORRECTED ANGLE CORRECTED DEPTHI 1 ANGLE DEPTHlm I AZIMUTH DIP DEPTHI 1 AZIMUTH DIP ' O ' ' O O I HOLE NO ZIPP" PQtNT ' - BD'C:EPGRT MTS 1 91CU..*3'iD L ~ G ~ ~ D. D ~ Lefebure Y
10 '\ F Overburder ROCK TYPE COLOUR GRAIN SIZE TEXTURE AND STRUCTURE ANGLE TO CORE AXIS ALTERATION SULPHIOES to In t e rme dia t Lapilli anc Ash tuff. Lt. Grey t c Greyisk -Green f.g. to m.g. - fine grained to aphanitic at top of unit grading downwards into mediumgrained clastic rock - sil.iceous clasts most pronounced, angular, i r regu I. ar shape s 0 - weak 60 to CA - quartz (minor carbonat ve i n I. e t s 20-35' NIL - diss. cp and py (< 1%) to % py to 22. a5 Gray MassiA Chert or Rhyo 1 ite Gray iphanitic, I - upper contact irregular with fragnents of siliceou: unit in overlying 1apill.i and ash tuff - massive NIL Barren to Mafic Ash Tuff Dark Green f.g. - some portions are aphanitic, massive with possibl amygdules filled with chlorine - carbonate veinlets 30' Chl.orite in tuff and filling amygdules. Trace diss. py to Layered Chert Grey iphan. - layers partially broken UP - basal contact 50' NIL Barren to Mafic Ash Tuff - simil.ar to to Also strong chlorite on fractures. HOI NO MTS 1
11
12 ~~ ~ FROM TO ROCK TYPE COLOUR GRAIN SIZE TEXTURE AND STRUCTURE ANGLE TO CORE AXIS ALTERATION SULPHIDES 35.4 to 175 con't shear zone with quartzcarbonate veinlets with silicified wallrock. 10% sulphides over 10cm with 3% cp and 7% py andesite dykes - f.g. grey with in the dyke at amygdu le s to 175m EOH
13 ROCK TYPE COLOUR GRAIN SIZE TEXTURE AND STRUCTURE ANGLE TO CORE AXIS I ALTERATION -I SULPHIDES CONCLUSIONS 1. The cherty exhalite wit1 diorite intrusion. 2. The hole was col.1.ared i i of the casing. 3. Shear zones in the quar texture. Disseminated 1 Minor chalcopyrite occu are to be assayed for gl 4. No fault was encounterel south shal.1.owl.y and the pyrite intermediate diorite rite and in some d. in the d as t -wes t irtersected in SRM 16 is d 1apill.i and ash tuff are silicified and chlor quartz-carbonate veins a quartz veins. Several. s I i1.l.ing. The quartz dior fault at the trench must ed out by the quartz imilar to outcrops east ized with a weak rnylonitic common in the shear zones p1.es from the shear zones e must dip towards the ip to the south as we].].. I D. Lefebure I.. May 2, 1984 i, HOLE NO MTS 1 7,,. r I,
14
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