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STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES Alaska Geologic Materials Center Data Report No. 369 No. 369: Pyramid Project: Aleut- Quintana -Duval Joint Venture Report on 1975 Drill Programme l e Received September, 2009 All data reports may be downloaded free of charge from the DGGS website. GMC Data Report 369 1 of 56 PYRAMID PROJECT ALEUT- QUINTANA -DUVAL JOINT VENTURE REPORT ON 1975 DRILL PROGRAMME by J. S. CHRISTIE PROJECT GEOLOGIST Dec. 15, 1975 GMC Data Report 369 2 of 56 SUMMARY TABLE OF CONTENTS INTRODUCTION 3 LOCATION 4 ACCESS 4 CLIMATE 5 TOPOGRAPHY 5 GEOLOGY 6 Lithology 6 Surface Oxidation and Leaching 8 Alteration 9 Mineralization 9 DRILLING 11 CORE RECOVERY 12 SAMPLING AND ASSAYING 13 MINERAL RESERVE ESTIMATE 14 Geological Mineral Reserve Summary 14a Additional Geological Potential 14b EVALUATION AND REMAINING POTENTIAL 15 RECOMMENDED MINIMUM PROGRAMME - 1976 16 REFERENCES 17 APPENDIX 18 FIGURES AND MAPS page 1 LOCATION MAP 3a GEOLOGY AND ALTERATION in pocket MAGNETOMETER SURVEY in pocket CROSS SECTIONS in pocket CROSS SECTIONS - Showing Area Included in pocket in Mineral Reserve Calculation CROSS SECTIONS AND LONGITUDINAL SECTIONS- " Showing Area Included in Mineral Reserve Calculation GMC Data Report 369 3 of 56 SUMMARY PYRAMID PROJECT ALEUT- QUINTANA -DUVAL JOINT VENTURE REPORT ON 1975 DRILL PROGRAMME Pyramid prospect was given Identified Area status in 1974 as set out in the Aleut-Quintana-Duval Joint Venture. Diamond drilling began in early September 1975 after considerable delay in construction of an access road, and by the end of October 19 shallow holes had been completed for a total footage of 5563 feet. Geology and hypogene sulphide mineralization at Pyramid are similar to that of porphyry copper deposits at many places throughout the world. As in many other deposits the secondary supergene enrichment process has given rise to a copper enriched chalcocite blanket at Pyramid, which is as thick as 300 feet in some areas. A mineral reserve estimate has been made using .25% Cu or the projected base of the chalcocite blanket as cutoffs as applicable, and 126 x 10 tons grading .403% Cu and .025% Mo have been indicated in a near surface zone consisting largely of chalcocite enriched rock. A large tonnage of even lower grade material is likely at greater depths (more than 150300 feet beneath present land surface), but very few high grade copper sections have been discovered. Wolfhard (1974), indicated that in his opinion local economic factors were such that at least a small amount of relatively high grade material (30 x 10 tons of better than .8% Cu) would be essential to GMC Data Report 369 4 of 56 2 the feasibility of an open pit mining operation. None has been found. If Wolfhard's figure is correct, as 1 believe it to be, then it is clear that the presently indicated grade at Pyramid is sub - commercial. Chances for discovery of enough high grade ore to change the economic outlook are considerably less than at the outset, but some untested areas remain and some faint hope therefore exists. The western extension of the system has not been drilled and room exists for some 49 x 10 tons of chalcocite enriched rock. In addition the system has not been totally delimited to the east. Potential for limited amounts of higher grade material in the vicinity of QP -6 and BBSI -3 (the best 1975 holes) is apparent. It is also possible that 1975 holes QP -13 and BBSI -6 which had very poor recovery in the chalcocite zone, might be significantly upgraded. The minimum programme at Pyramid in 1976 should consist of 6 diamond drill holes to further explore for higher grade copper mineralization within the areas indicated above. A very preliminary estimated cost for this pro- gramme is $250,000 which includes $35,000 for demobiliz- ation of drilling equipment from Alaska, and $50,000 for additional drilling contingent on the results of the first 6 holes. GMC Data Report 369 5 of 56 INTRODUCTION 3 The Aleut - Quintana -Duval Joint Venture originated in 1974, and initial field work consisted of a regional minerals exploration programme covering all withdrawn lands where the Aleuts were entitled to acquire mineral rights by selection. This exploration programme was successful to the extent that a significant copper molybdenum prospect was located near. Pyramid Mountain and several other less important prospects were found in the district. The Pyramid Prospect being by far the most important, was designated an Identified Area under terms of the 1974 Joint Venture. Identified Area status has been maintained by virtue of Quintana - Duval's comple- tion of the 1975 work commitment ($50,000) specified in the Joint Venture agreement. The 1975 programme began in early April when the landing craft Cape Douglas delivered 2 diamond drill rigs and related exploration and camp equipment to the beach near the head of Balboa Bay (Albatross Anchorage) some 5 miles from Pyramid. A small tent camp was established and construction of the Pyramid access road commenced and continued through May 15th, at which time roadbuilding was suspended when deep frost and snow were encountered at higher elevations. Roadbuilding was attempted again in early July but was soon discontinued on account of the extremely soft, wet condition of the ground at that time. In late August the road was finally completed and a tent camp was established at Pyramid. Drilling began during the first week of September and 19 holes had been GMC Data Report 369 6 of 56 GMC Data Report 369 P Y R A M I D P R O S P E C T LOCATION MAP SHOWING ACCESS ROAD SCALE gaRamew b�FI F 1 (L Prepared by: J SC Date : March 13/75 `JTS MAP AREA Prawn by AT K Revised: 7 of 56 J DRAWING No. 4 LOCATION completed when the programme was suspended and the camp and drilling equipment were winterized near the end of October. Pyramid prospect is located in the mountainous central part of the Alaska Peninsula about 23 miles north of the village of Sand Point on Popof Island,and some 600 miles southwest of Anchorage. The prospect lies between 1000 feet and 2000 feet elevation, about 5 road miles from Pacific Ocean tidewater at Albatross Anchorage, Balboa Bay. ACCESS Latitude 53 37'N, 160 41'W Port Moller C -2, 1 :63,360 sheets In 1975 a tractor - A.T.V. access road was completed from Albatross Anchorage to the prospect, and the upper 1/3 of this road is passable by 4 -wheel drive vehicles. Other- wise access is by helicopter, or by boat from Sand Point and then by foot. Sand Point is served by Reeve Aleutian Airways scheduled flights arriving 3 to 5 times weekly weather permitting. Charter aircraft are available from 2 operators in Sand Point as well as from King Cove and Cold Bay. Sand Point with a population of about 300 is a centre of operations for 2 commercial fishing companies. Coastal GMC Data Report 369 8 of 56 CLIMATE 5 freighters from Seattle, and a containerized shipping service connecting with Kodiak - Anchorage -- Seattle stop regularly at Sand Point. A large general store, post office, cafe, bar and motel serve the community. The climate is marine subarctic and clearly more inhos- pitable in the mountainous region near Pyramid than at nearby Sand Point. Although extreme low temperatures are rare, snow accumulates at the prospect from October through April and accompanying strong winds create a significant wind-chill factor and cause formidable accumu- lations of drifted snow. Effective drilling and exploration programmes cannot be extended beyond a 6 month season and work can be most efficiently done in the 4 month period June - September inclusive. TOPOGRAPHY The prospect is centred on a u- shaped (glaciated) east - west trending valley flanked by rocky peaks and ridges that rise as much as 1500 feet from the valley floor. Talus forms conspicuous overburden on these slopes, and the lower slopes and valley floor typically display thick accumulations of ferricrete cemented talus. Vegetation consists of sparse moss, grass and flowering plants, with alder below 700 feet elevation. Below 500 feet alder forms thick cover on well drained ground but many gently sloping areas tend to be wet and boggy. GMC Data Report 369 9 of 56 In construction of the Pyramid access road it became apparent that surficial deposits below 500 feet elevation in the vicinity of Albatross Anchorage consist predominantly of sand and clay and little if any rock. Thus solid roadfill is scarce. Above 500 feet slopes tend to be steeper and rock is considerably more abundant thus making good roads possible at least in well drained areas. Above 1000 feet elevation rock is sufficiently abundant to allow good roads in most terrain. GEOLOGY Lithology Mineralized rocks forming the Pyramid prospect include a succession of fine grained clastic sediments intruded by several quartz bearing porphyry stocks and dykes of probable quartz diorite composition. The sediments belong to formations assigned to the Upper Cretaceous and Early Eocene by Burk (1965), and the porphyry intru- sives are therefore Eocene or younger. Flinty hornfels has been developed from these sediments within the thermal aureoles of the porphyry bodies, and a strong hydrothermal sulphide system centred on the largest stock is superimposed on both rock types. Late and postmineral intrusive phases occur, and 5 late mineral post- copper breccia pipes contain- ing strong interstitial pyrite are known. Within the intrusive rocks hydrothermal alteration tends to be extremely pervasive, especially within the quartz - sericite zone, and original textures have been destroyed. GMC Data Report 369 10 of 56 - 7 - Relicts of feldspar phenocrysts and quartz eyes are all that remain of the primary igneous texture, and inas- much as quartz eyes vary considerably in size, form, and abundance from place to place, it is possible that the main intrusive body is a complex polyphase pluton. Where primary igneous textures survive such as within the biotite core zone, and beyond the outer limit of pervasive quartz sericite alteration as at 11,500N- 11,500E, a crowded porphyritic texture is apparent. Subhedral plagioclase phenocrysts 2-5 mm in length and rounded quartz eyes are most prominent while mafics are strongly altered, but have forms suggesting primary hornblende and biotite. The main intrusive body has been shown to differ in size and shape from that indicated by the preliminary mapping. Most significantly, a large panel of weakly mineralized hornfels centred on Section 8600E has been exposed in a number of bulldozer trenches and roadcuts where well mineralized quartz sericite rock was anticipated_ Several late and postmineral intrusive phases are present and these in general are porphyries characterized by larger subhedral to euhedral plagioclase phenocrysts and more quartz. Textures tend to be less crowded than the early porphyries, and range to include near hypidioniorphic granular varieties. The breccia pipes contain variously altered and mineralized metasediments as well as premineral and postmineral intru- sive clasts. Breccias in the eastern part of the system differ in that they contain clasts of metasediment which GMC Data Report 369 11 of 56 8 are conspicuously less altered than adjacent rocks sug- gesting that these clasts have been transported considerable distance within the pipes. Surface Oxidation And Leaching Drilling has shown that the depths of oxidation and leach- ing range from 0 to 450 feet at various localities on the property. The main factors controlling depth of oxidation appear to be a) elevation above local water table b) permeability of rock c) relative abundance of sulphides. Elevation is clearly an important factor as exposures along the main drainage show little more than surficial oxidation while those on adjacent slopes and ridges are oxidized and partially leached to an average depth of about 100 feet. Permeable rocks such as breccias and sugary textured quartz sericite rocks tend to be more deeply leached than less altered, less porous rocks. High pyrite contents such as in holes QP -2 and QP -3 also clearly contribute to a greater depth of oxidation and leaching. GMC Data Report 369 12 of 56 Alteration Distinct hydrothermal alteration shells have been mapped about a high intensity core zone containing strong second- ary biotite and 3 -10% magnetite as fracture fillings and disseminated clots and grains. A ground magnetic survey with interpretation substantiated in part by outcrop, and by 1 drill hole, clearly indicate the position of the core. Minor chalcopyrite and molybdenite mineral- ization occur in the core, often in association with quartz veinlets,and minor pink k- feldspar is present. A 200 -800 foot wide transition facies separates the core from a broad zone of pervasive quartz sericite alteration which contains subzones having strong quartz veining and silicification. Primary Cu -Mo mineralization and super- gene chalcocite enrichment are strongest within pervasive quartz sericite rock of both metasediment and intrusive rock types. Outward through a narrow transitional facies alteration becomes non- pervasive and sericite in fracture selvage modes grades rapidly to chlorite. Mineralization Primary sulphide mineralization shows a zonal arrangement overlapping the silicate alteration shells. Highest total sulphide content (5-10%) overlaps the inner part GMC Data Report 369 13 of 56 10 -- of the chlorite zone and the outer part of the quartz- sericite. High pyrite /chalcopyrite ratios (50:1 or more) are associated with low copper grades ( {.15% Cu) and very low molybdenum grades (.00x% Mo). Total sulphide content and pyrite /chalcopyrite ratios diminish inward through the quartz sericite zone, and copper grade increases to .3 - .4% Cu. Molybdenite also becomes more abundant inward as intensity of quartz veining increases reaching .03 - .05% Mo in the innermost parts of the quartz sericite zone. Inward with the first appearance of biotite total sulphide content drops below 1% and both Cu and Mo grades diminish. Within the biotite core beyond the inner limit of sericite, total sulphide content is less than .25% and both Cu and Mo grades are on the order of .00x %. In general sulphide grain size diminishes inward such that within the most copper rich parts of the system the majority of sulphide is finely disseminated, although a significant part occurs as thin fracture fillings. Thick chalcopyrite filled fractures are extremely rare. Secondary supergene copper minerals which contribute significantly to grade are chalcocite and covellite, but traces of copper pitch, copper - manganese, copper- carbonate, chrysocolla and cuprite occur. Chalcopyrite is most strongly replaced by the secondary copper minerals but skins of chalcocite also occur regularly on pyrite, and since the sulphides tend to be very fine grained,estima- tion of copper grade is a problem. GMC Data Report 369 14 of 56 DRILLING Supergene enriched chalcocite blankets as much as 300 feet thick are indicated in some areas at Pyramid, although the best copper grades are found in the upper 100 feet or so of the chalcocite zone where the highest degree of chalcocite replacement has occurred. The thickest chalcocite blankets do not coincide exactly with the zones of deepest oxidation, for example in hole BBS1-3 the oxidized zone is only 62 feet thick, but the chalcocite zone exceeds 300 feet in thickness. It is presumed that this situation is one where lateral -down- slope transport of copper has occurred, or alternatively part of the oxidized cap may have been stripped away in the most recent glacial episode. If the latter were the case, the chalcocite blanket at Pyramid is not entirely due to present day conditions. Canadian Longyear Drilling, under contract to Quintana - Duval, supplied 2 diamond drill rigs for the Aleut pro- gramme, a hydraulic Longyear 38 equiped for NQ drilling and a screw -feed Boyles BBS- -1 equiped for AQ. The BBS -1 was primarily intended for use on the helicopter supported anomaly programme but became available and was mounted on skids and used to drill 6 holes at Pyramid. The total AQ footage drilled was 1738 feet. The 38 completed 13 holes for a total NQ footage of 3825 feet. The 1975 programme at Pyramid totaled 19 holes for 5563 feet, and drill logs with recovery and assay data are appended. GMC Data Report 369 15 of 56 CORE RECOVERY Core recovery was not satisfactory in 4 of the 19 holes drilled (QP -10, 11,13 and BBSI -6). Recovery was especially bad within the chalcocite enriched zones of these holes averaging about 47%, and even less in shorter more highly enriched sections. It is likely therefore that the copper assays reported are lower than the actual grade. It is important to learn the actual grade of these holes and most critically the grade of BBS1-6 and QP -13 which are the only samples available within the eastern part of the system. If for example, the 1975 assays were upgraded by as much as 50o they would substantially change the econo- mic evaluation at Pyramid. it seems unlikely that a 50% upgrade will be realized, but a twin hole for one of BBS1-6 or QP-13 is warranted to make certain of the enriched grade within the chalcocite blanket. Poor recovery in the above 4 holes appeared to be related to several common causes. All poor recovery sections were in extremely pervasive quartz sericite altered intrusive rocks which are soft, friable, granular, easily washed materials. During the coring operation it appeared that as a result of erosion by the circulating fluid the core was reduced in diameter by the time it reached the core tube, such that it would no longer engage the spring. In addition these rocks all display to some degree horizontal almost penetrative micro-fracturing and the core tended to separate into thin discs which rotate and grind. In many instances only quartz veins and their silicified selvages were recovered, the softer inter-vein material having been completely ground or washed away. It seems GMC Data Report 369 - 12 - 16 of 56 SAMPLING AND ASSAYING - 13 - likely that some of the higher grade chalcocite sections were lost in this manner. I have been informed that use of larger diameter HQ core equipment drilled with a 5 foot corebarrel and face discharge bits would likely make a significant difference to recovery in the chalcocite zone. Samples for assay were obtained by splitting the core with a conventional Longyear coresplitter, coarse crushing to about -4 mesh and then reducing the volume of sample by 50% or 75% with a Jones riffle. This procedure yielded about 2 -3 1b. crushed samples depending on core size and recovery, that were amenable to compact packaging and air shipment. Copper and molybdenum assays were run on all samples shipped, check assays were made with 2 additional labs, using pulps from the original samples. In addi- tion the sampling procedure was checked and found adequate, by assaying a number of Jones riffle rejects which had been saved at the property. Composite samples were made up in approximate 50 -75 foot intervals and these were assayed for gold and silver. In addition 4 representative composites were selected for 30 element spectrographic analyses (results appended), and a small suite of representative samples are being prepared for reflecting microscope examination. GMC Data Report 369 17 of 56 MINERAL RESERVE ESTIMATE - 14 - Sets of cross sections and longitudinal sections were prepared to illustrate the geology and estimate grade and tonnage. They also point to the potential of some areas that as yet have not been drilled. The reserve estimate was made using .25% Cu or more commonly the projected base of the chalcocite blanket as cutoffs, where applicable. As a result, chalcocite enriched rocks form the bulk of the estimated tonnage, which constitutes a near surface volume ranging from about 150 feet to 300 feet beneath the present land surface. As detailed in the table below, and illustrated on accom- panying sections the near surface reserve at Pyramid is estimated to be 126 million tons grading .403% Cu and .025% Mo. In addition potential exists of another 49 million tons of chalcocite enriched rock of unknown grade in blocks R-S-T, west of the area drilled in 1975. Down - slope transport of copper as well as enrichment from over- lying leached rocks could combine to give a high enrichment factor in area R-S-T. Hypogene grades of .3% Cu (grade of QP -5) or better can be inferred for at least part of area R -S -T. The east end of the system remains open as hole QP -9 penetrated only postmineral intrusive and breccia. At least 1 hole is needed east of QP -9 to measure the grade of premineral rock, in what is projected to be a large area of favourable geology. GMC Data Report 369 18 of 56 SECTION BLOCK TONS x 10 CU GRADE % MO GRADE % BASIS OF GRADE ASSIGNMENT 9,000E r UAw w0xH hxa z 0 w 5.17 .309 .027 Grade of QP-5 5.39 .510 .021 Average of BBS1 -3 and QP -4 (27'-221 9,400E 1.38 .390 .027 Grade of QP -6 (213' -323 9.79 .309 .026 Grade of QP-5 15.75 .410 .021 Average of BBS1O3 and QP -4 (27'-221') 10,000E 2.52 .351 .032 Grade of QP -6 (25' -88') 2.92 .596 .029 Grade of QP -6 (88' -213' 5.46 .390 .027 Grade of QP -6 (213' -323 14.1 .450 .036 Grade of BBS1 -3 (36' --30 10,400E 5.10 .351 .032 Grade of QP -6 (25T_88 6.58 .596 .029 Grade of QP -6 (88' -213' 8.62 .390 .027 Grade of QP-6 (213' -323 6.41 .330 .031 Average of BBS1 -3 and BBS1 -5 10,800E 5.03 .286 .011 Grade of QP -11 (104' -- 230') - QP-10 dis- regard because of poor recovery 11,800E 10.67 .360 .014 Grade of BBS1 -6 (70.5' -187') 7.55 .480 .025 Grade of QP -13 (168' -248') 12,600E 13.89 .420 .020 Average of BBSa-6 and QP-13 TOTAL 126.33 .403 .025 - 14a - GEOLOGICAL MINERAL RESERVE SUMMARY Notes: Cutoff grade - .25% Cu Tonnage factor -- 12 Sections - projected z distance to adjacent sections E and W. Core Recovery - very poor in holes QP- 10,11, 13 and BBS1 -6 - copper assays may be low. GMC Data Report 369 19 of 56 7200E R 21.54 8000E S 18.27 3600E T 8.98 TOTAL 48.8 ADDITIONAL GEOLOGICAL POTENTIAL - (no drilling in area) - 14b - - this untested geologically favourable area could contain in the order of 50 million tons of rock that could possibl be strongly enriched with chalcocite. We have no indication of what the grade might be. GMC Data Report 369 20 of 56 15 EVALUATION AND REMAINING POTENTIAL Wolfhard 1974, in his Preliminary Evaluation of Pyramid, expressed his opinion that "Operating economics in this part of Alaska are thought to be such that a reasonable tonnage of fairly good grade (say 30 x 10 tons @ better than 0.8% Cu) would allow the eventual mining of several hundred million tons of grade greater than 0.25% Cu." In view of recent sharp increases in operating and capital costs even 0.8% Cu may be a low estimate of what would be required to allow a mining operation to begin at the present time. Pyramid is undoubtedly a legitimate porphyry copper deposit and there is no doubt that it contains a substantial ton- nage grading better than .25% Cu. Unfortunately the chances that the required 30 x 10 tons of better than .8% Cu will be found are not good. None has yet been found, and the best hole to date (QP -6) contained at best a section 125 feet long which assayed .596% Cu and .029% Mo. Geologically, there is room for about 10 x 10 tons of similar grade material around QP -6 although there is hope for a smaller tonnage of higher grade rock on the north, uphill side of QP -6. If a more optimistic view were taken, the holes drilled to date are widely spread in some areas, and these may have missed relatively narrow shells or areas of better hypo - gene grade. Perhaps a well mineralized breccia exists and remains undiscovered? Any higher hypogene grade section could be expected to give rise to a well enriched section, if the enrichment process had gone on to the degree seen elsewhere. Small areas of considerably better grade than anything seen to date could conceivably exist. GMC Data Report 369 21 of 56 In addition, as discussed previously there is a chance to upgrade a considerable tonnage of rock in the east part of the system by twinning QP-13 or BBS1-6 and improving recovery. Also the system is open to the east, and a target with about 49 x 10 tons potential exists west of the area drilled. RECOMMENDED MINIMUM PROGRAMME - 1976 A minimum programme for 1976 should consist of at least 6 -350 foot holes drilled with HQ equipment, a 5 foot corebarrel, and face discharge bits. HOLE A C D E F Alaska. GMC Data Report 369 CO- ORDINATES 11600N- 10400E 9800N- -8000E 11400N- 14000E? 10600N-- 1.0000E 8700N -9400E -- 16 -- DESCRIPTION - to offset Hole QP -6 on the uphill side where greater enrichment could exist. -- to test the unknown west end of the system. Blocks R-S-T. - to close system on east. -- twin hole for QP -13 or BBS1-6. -- offset on QP -6 looking for better hypogene grade. - offset on BBSI -3 looking for better hypogene grade. The preliminary estimated budget required to carry out a 6 hole programme is $250,000 of which $50,000 is contingent, and reserved for additional drilling in the event results from the first 6 holes warrant followup. The budget also includes $35,000 for demobilization of all equipment from " v ( r : � �r - of 56 rf %� f1' REFERENCES - 17 - Burk, C. A., 1965: GEOLOGY OF THE ALASKA PENINSULA ISLAND ARC AND CONTINENTAL MARGIN: G.S.A. Memoir No. 99. Christie, J. S., 1974; ALEUT-QUINTANA-DUVAL JOINT VENTURE- - 1974 -FINAL REPORT. Christie, J. S., 1975; ALEUT -- QUINTANA -DUVAL JOINT VENTURE- 1975-PRELIMINARY REPORT. Wolfhard, M. R., 1974; PYRAMID PROSPECT, PRELIMINARY EVALUATION. GMC Data Report 369 23 of 56 Abbreviations Q -- quartz Kf - k-- feldspar Bi - biotite Chl - chlorite Cl - clay Ser - sericite Mag - magnetite Hem - hematite Explanation of Alteration Log a) Qualitative x - indicates presense of a mineral as part of the hydrothermal alteration assemblage. b) Semi- Quantitative APPENDIX (1) DIAMOND DRILL LOGS Holes QP -1 to QP -13 -- NQ Core Holes BBS1 -1 to BBS1 -6 -- AQ Core Ep - epidote Cb - carbonate Sul - sulphate Cc - chalcocite Cv -- covellite Py -- pyrite Cpy - chalcopyrite Diss - disseminated Indicates on a scale of 1 to 3 the relative strength of devel- opment of hydrothermal mineral phases (F) along fractures and (D) - disseminated. (2) SPECTROGRAPHIC ANALYSIS RESULTS GMC Data Report 369 24 of 56 H H H 1-i 0 CANADIAN LONGYEAR DRILL RECORD Commenced I _1 ai l 1 1 E - 1 11 NMI 1 1 MEI 1 z y I I I zy ax I �s 11 I I 3 . 1 1111 11 III - 11111 1 11 1111111111111- , 11 1 , 111 , 111 .11 11 -111-111 1 11111 -III 11 11 11 111 -II - LII 1 11 1 11 1 E 5 g' g* sz• 1SZ sZ• SZ' SZ' I sz• sZ• S'T 1 sup, II 111111111111 11111 11111 I II I 111111 II 11111 III I II I III 11 11 MI III , , 11111111111111 II III 11111 1111111 I I 1111 u n 11 111111111111111 1111111 w 11111 II I 11111 1111 III I III I IIIII I II II I 11111 III , I1 11111111.1 1 aT uT 13 qaa; ST - ONISVD Quartz diorite porphyry near pervasive quartz sericite alteration but relicts of biotite in cores 1 between fractures. Deep oxidation to 14. As above - dis. chalcocite up to approx. 2.5% inc-A1 minor fracture limonite to 25 As above - slightly more silicified stronger quartz veining As above. • anoge sy • anogs sy Alteration intensity diminishes. 1 Alteration intensity diminishes. lgzsuaquz 110 p caul aiquTaun anq anoge se sazngxaq ao snoiamnN •anogs sy •anoge sy • anoge sy •anoge sy As above. Quartz diorite pervasive quartz sericite alteration minor relicts. Primary texture feldspar phenocrysts dis. chalcocite. 1 anogs sy 1 anoge sy 76 OT Z00T LZ g MOM 11211111= MEM L6 ;'OT 9001 EL 66 1 ", - OT SOOT S'Z9 014 IL 6ZT 11 1 L6 1 OT 1 HOT EOT 01 66 OT ZOT or g 11 .1 86 OT ZO1 01 1 86 1 0T 1 LTOT i OT 600I al 0I OTOT SAMPLE No, ! ZTOT ETOT hT01 0 _ . , FOOTAGE MEI Z01 ZIT ZE T ZST 1 Z81 0 LT LE LZ S'Z9 7.S ZOT H H H 1-i 0 CANADIAN LONGYEAR DRILL RECORD Commenced no 0 w N G7 J 2 It 0, 0 m c U 0 CANADIAN LONGYEAR DRI LL RECORD J. S. CHRISTIE 11111111111411 'III 111111 1111111 I xy 11 8 11111E11111 III ..i 1111114 WM A4 III IF ay ay ay ay 11111111 11111111111111 11111111111- -1111 I 11 11111-1111 111111111111 11111 1111 11111 -11 111111U 1 III 1 mill S1 5'T S'i s'1 1 T 1� s'1 11111 1111 ,III mill IIIIIIIII - AI.,TERATFON 1 1111 111111 I I 11111111 1111111111 I 11111111111 N1 I 1 1111 1111 1 , 1111 114111 , 1111111111 IIK , 11 Mill 1111111111 I 111111.11111 I 11 III I 011111 II 1111111111111111 1111 II 111111111 1111111 1111 � 1111, .11 _. sup. • anoga sv Quartz diorite pervasive quartz sericite alter- •agT000Tago 'sill •aaraotq apTIaa saosal •uoTaa Quartz veining. As above with more relict igneous texture . agtgoTq As above (216 - 222 fault gouge in several zones) •eAogs sv I angssnaad aaom uoTgsaagTv 'anoge sv As above. As above but alteration and quartz.veinins •a4zooaTsU3 1 - •anoge sv As above. Quartz diorite pervasive quartz sericite with only minor traces relict biotite. Strong quartz sulphide •Vi se 112'rg se agTaooTega •s •2uTu]aA As above but near total destruction of biotite. •avTgogq To uoTganagsap Taloq aaau lug anoga sv As above but more highly silicified. 'paT3ToTTzs - aeoga sv As above - coxcomb structure along quartz veins. ii Ull SAMPLE Length Rc Y• 86 86 66 1 , 10T 66 Z6 08 .,_ _ _ " ... ,—,, 1 68 . 0L 0T Z£OI g -- ® 01 £E0T 1 0I 0T 0T 2 2 p'01 r 'ZT m 2 2 04 2 01 8Z0T 2 w 2 `''' 1 9 I ICOT 01 4 7ED1 2 . 6101 OZOI 1 04 CSI EZ01 4 7201 NI N FOOTAGE of s•E47z L'SSZ 4 70E 4762 8ZE SEE 1 1 '6Z +7SZ 1 8TE # m no 0 w N G7 J 2 It 0, 0 m c U 0 CANADIAN LONGYEAR DRI LL RECORD J. S. CHRISTIE :F1 : $. P I P : : : : : III I : HO MIN 11E1111111111111111111 I MEW 11111 11.1111.111 t - II 111111111 1111111111111111 61 MI111111 I 111111 11111 III II I 1111111111111 III 4 111 11 III 11111111 III I 11111111111111111 CI 111111111 I II III III 1111111 II GENII , , 111111 x O 11111111111111111 11111111111111 Aaeiu}LQ to uo.p eaa3TTgo 1E401 4somTe - aaogE sv -azngxa2 •aeogE sv I As above. As above. As above - very intense silicification from 392' on. „ - eaoge sv As above - traces of relict biotite and primary texture. 54 ES 66 EMI SAMPLE Leng[h No. 8 9E0T £9E 1 SSE ECM lie I - -_- ET 6E01 96E E8£ IIIIIIIII 11111. 01 8E01 £8£ - S- OT LEOT ® E9£ ;': 0701 5'907 1 96E asvuaAd 170T FOOTAGE o S wo,d E ,„ 1 1 ( ------- a m 0 J 0 a a DI AMONV DR I LL RECORD CANADIAN LONGYEAR S. CHRISTIE DRILL RECORD J. S. CHRISTIE Il 11111 Ill HIHI 111111111111111111111::1 �� Ada/ ©11 11 1111111 -III 4dlns 11111111 111111111111 ALTERATION 111111111 ®® d3 � II11111111IIIIIIIIIII 11111111111 11 11111111 111111111111111111111111■ 111 IlII I x 1111111©1!...1 1111111 111111I '140 III IIIIIIII1111IIIII ■IIIIII 11111 II II 1111111 d� X111111111111111111111111 IIII 1 1 111 x X111111 1..111 IIIIIIII L F- U Q L" Breccia -- quartz - feldspar porphyry - quartz eyes to 4 mm - strong fracture sericite with quartz veining and silicification - 100% leached with reddish to deep brown and black limonites "live "? Not much rotation or milling in breccia. Estimate 10 - 15% primary sulphide. Traces chalcocite ?? in some less altered cores -- Strong quartz veins , cut some clasts - Contains pre - mineral (qtz veined) clasts x gdzod asdsp1a; zaisnb - isaauTU1- sod pun '££h 4s duo pagasaw aSsE • s :se 1 TET d '8Zg oq ££7 m0x3 20TgaeaT IsTlied t }41-4;.a.0a4u1. eTaaaxq uT agraAa 3O 2fuigOEaT 1 cavities. Dis. pyrite not leached. Total sulphides up to 20 %. Trace covellite.. la3Taoalsgo aaszy 4.al_Taicdooretio palnoa Fine MoS, associated with quartz veinlets. PWCTT3 ATa3aTamoa gsomTe eTooaxq uT s2nA •al.TAKd g zaxsnb 3o sgatloagaalu 43TM_ 8L o Q d L 7Z 85 L £ I 917 S L 1 I' Z S LI ,O 1 91 S T '0i O+ SAMPLE No. r. t'.. O r.f z c UCH 01-.1 t• C` I 0 0 .■ rq ■ SLOT 1 7401 CLOT iO NI 0 .-r 1 I LLOi CO N 0 .-r ■ 1 6L01 FOOTAGE of it M M T W N Ln W d' -.d- I . S' M in d N CO 0 T d u 1 M in u'1 CO .-a In N P M v1 .Y Lri rn in 4f1 wOJd C v1 r 1 M M v M M d 0o d el O M M W . 7 c N v d O CO '-r WI M M d T 1 DRILL RECORD J. S. CHRISTIE t/5 cu L c J C mw 0 Mg ' W 4 O C C Z v O 2 c 0 1 , c m 0 E Q D a DI AMOr..-J DR! LL FiECORD SEPT. 22, 1975 J. S. CHRISTIE VERTICAL Commenced IIIH LS 1 c5 II ■ ■ ■■■ ■l ■ ■ ■ ■ ■ ■. i ■ •uiu ■1 ■ ■■■I - ■C ■ ■ ■■ ■■■■mil 1 ■ ■ ■ ■■■■ ■ III ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■■ ■ ■ ■ III IIII■IIIIII■ ■■■11 ■■111111111■ ■ ■ ■■ 11111111 ■1■III III ■I ■ III IIIIII ■ ■■ ■ ®11 © ■ ■I ■■ x ■ ©■� ■ ■ ©1© ■■ ill1111 ■■ x 1 ■■1■■©■ x 111 u■1 ©1■ 1111 11111 ■ ■I 11111 ■MI1111111111II ■ ■ ■1111111111■ ■1111111 ■I1■ ■11111 ■ ■1 ■ ■ ■■■11 ■■ ■111111 ■■ III 1■ ■ ■ ■ ■ III II NW 1■ 111111x . ■ ■ ■ ■ ■e OMISV0 Leached cap strongly fractured quartz,eye porphyry strong quartz veining. Live limonite present. Areas of non pervasive recrystallization are greenish grav feldspar porphyry without quartz eyes. Very few if any quartz eyes below 43 ft. Possible rock type change. From 156 ft. to 196 ft. rock is about 50% leached feldspar porphyry as above. Weak fracture leaching to 205'. Strong chalcocite below 156 ft. ............ Alteration is pervasive sericite clay. No chaicopyrite seen -- all replaced by chalcocite? Strong MoS locally. Dis. hematite from 196'. Partial leaching of pyrite on fractures of dis. pyrite. Pyrite is deeply corroded and tarnished. Materials previously referred to as chalcocite may be corroded pyrite grains. However some coatings on pyrite do appear to be chalcocite. Unable to identify finely dis,, black materials. Relict porphritjc textures are frennantiv wvir3 a„r 1 Strong fracture controlled pyrite along steeply inclined fractures is the mnet atriUinn „7 „},i Ae mineralogy. Dis. magnetite is associated with isolated chlorite bearing zones whera rho original porphyritic igneous texture is most pronounced. From 250 onwards alteration intensity 1 increases to pervasive quartz sericite and 1 copper content increases accordingly. Finally dis. black materials may be in part chalcocite quartz _pyrite veining with some MoS.. 1 From 291' to 298' and 111' to 122' partiai leaching with limonite occurs. From 311' onwards rock is extremely friable and broken and much fracture pyrite is tarnished. Dis. black materials are in large part coatings on pyrite and may not be chalcocite but covellite . may also be present. = N N -I M 6 �7 � O ti0 4 d 1 26 96 i� M S6 N C 6TT 'y M cal 1 71 C CO W n OT 0 C Cr T 0 'o N aldW7S Co M rn 1 7601 a c C 9111 ri N w ,1 16111 O N TM '. r�ZTT 17z'T 3OV'JOOd 0 ul , L -1 ^ m w m .-a C N .1 N N N N N I ssz m N 1 tsz .c Y. I SLZ S2Z wo,d P M ,ti V' ^" M sO "' N W s.0 C •-+ in 0 N M ,--i NNN ,- N m MM M N d N N v- N 'O 'O N t/5 cu L c J C mw 0 Mg ' W 4 O C C Z v O 2 c 0 1 , c m 0 E Q D a DI AMOr..-J DR! LL FiECORD SEPT. 22, 1975 J. S. CHRISTIE VERTICAL Commenced z 0 2 P, O • <4 O • 0' Z 0 I - E 01 0 -J • 0 LU crl -C 127 c co - a 0 O. E 0 0 0 0 0 GMC Data Report 369 30 of 56 DI ANION,_, DR I L L RECORD SEPT. 22. 1975 J. S. CHRISTIE Commenced VERTICAL 'BVyy Ada /Ad OT t LIRA rssl O ,.. • 4dlns 0T ALTERATION_ 'MS "GO d3 'gag t..) '14J m d>1 d m i Bole stopped in badly broken caving rock -- a ,. e. . ‘.0 9L T9 891 ', L8 a 1.--. . 4.... 1..-- ce c s• Til s•0T of 4: 'c SAMPLE No. ir N. — z c . 9ZIT 1 LZTT 1 SZTT ZIT -- a. cr ,-- te• V.: -a 39V.J.A7Md of u.• 0' c-,, s•90C LT£ LZE i m m a e re wo+d u- cc n _ ...____ 1.-1, as N ,...--, '90E 1 .. , LIE — ... r-... r.., C' .. Cr c t . ............... z 0 2 P, O • <4 O • 0' Z 0 I - E 01 0 -J • 0 LU crl -C 127 c co - a 0 O. E 0 0 0 0 0 GMC Data Report 369 30 of 56 DI ANION,_, DR I L L RECORD SEPT. 22. 1975 J. S. CHRISTIE Commenced VERTICAL F va 0 0 DI AMOlvii DRILL RECORD J. S. CHRISTIE VERTICAL II MEMNON 11 MOM MENNE 1 I MENEM I 0 IME e oi HI 1 II MEM EH MI NEI I *: 1 11111111111 -II -11111111M MI 11 - NOILVlS31.1V 1 MI 1111 1111 I II II NMI . Ins - II 11111111111 II om - - - 11 111111111 t n � X X . Jos x I I I III 1111 - 147 11111 1111 Ell a I 11111 III 11111 MIN I 1 1111 I 1111111111 111111111 El I - 3N III 11111111 I I. =III II I MIEN le 61 A' - 16' Hornfelc light prey in color, strongly re_ crystallized, contains fracture and dis. pyrite much of which is tarnished and resembles covellite •quasaad osla agz:ldoofsgo pagsoo agTTlanoO1 Lg1 EH IIRIR 16' -- 23' brecciated and gougy intrusive - probable fault zone partly leached. 86 23' onwards quartz feldspar porphyry with much dis. fine grained bluish black chalcocite? covellite? corroded pyrite? alteration. 98 Serasifp clay gnarl - z. Tarnishe nd corroded pyrite is more likely than chalcocite. Chilled contact at 161' with hornfels. I xa)l1ap anq anocra ss sia3uxotI li9T mold sgi gray in color and less recrystallized. Tarnished pyrite abundant. Covellite coated • atgsun gnq quasazd aq osTu Asm agtaAdoo -silo 56 •m1EJuo0 04 I i From 225' onwards hornfels lighter grav in carries more sulphides. Tarnishing of sulphides less pronounced. MoS„ present in quartz veinlets. Probable covellite ep¢qutnb bL�J dq.y iU 45O14 'OLZ gE suteA zgxnno UT Z SON pun agT1AdooIagO •agzaAdooIsgo pagneoo EN Spraritp becoming coarser grained _150S becoming more abundant downwards. 100 From 324' intensity of alteration and weakan 1 66 8L; ISOT g TT '9 II SAMPLE Na, - z£IT 111 I '' 111 9£1T 1 s'E9 II SETT 1 E8 ill IMIMMIIII O+7I T Z +�zT , 1 7 1 7I1 8£I 30V1003 of wo,3 II - 1 LZ 91 111 L L' II s•as . ZL _ _ 1 STT _ F va 0 0 DI AMOlvii DRILL RECORD J. S. CHRISTIE VERTICAL .... ro -J LU z 0) E4 1:4 F.1 0 N EH -0 >- .0 r2 cL a E DI AMON'O DRILL RECORD J. S. CHRISTIE LONGYEAR 1 111 111 III 1 1 11 1 'Be Ado /Ad III Il 111.10111111111 1 Hal I II I WM 1 p II Elmo HAI •1 El u1aA I EN R EM • mr " I so I I ALTERATION 1 °n uI .ulHhIuIIIIIIIuIIIHhIIuIIIHhIHHHhII I1UIIIIIIIIIIIHIIIIIIIIIIIHHIIIIIIIH1II 'q1 n 1 Ins I qo I d3 1 Aos 1 • HIHIIHIIIUUIIIIII IIIIIIHIIIIIIIIIIIIIII I s`£ [ 1 1 1 IIIII •• •• , •I in UM= EVIMBLIFILmoom MEI IMINIMINE I I 111111111111 •IIIIIIIIIIIIIIIIIIIIIIIIHIIIIIHHIIIII IIIHIIIIIIIIIIIHIUIIIIHIIIIIIIIIIIIIIII '10 1940 I 18 I — 1 H IIIIIIIIIIIIHIIIIIIIIIII1IIIIIIIIIIIIH 11 111 I 1 MEMINEMEMMINMEMI I I 1 1 MEI HEMI MEMIMMINFIEI ; El e0I I S•Zf 1 1 I r 86 1 6 E E'1PI19lIi 7815'01 I MIME ME IlLii .• OI 86 01 EOII ME SAMPLE No. - -11111 ••1111111111 patdmss 911 Ni paTdmu§7 1OK E911 No paTdmvs ION Z911 • paTdmaS 1 9911 Na 1 paTdm>?s 1 FOOTAGE 01 1 MIE MEM MIE 81£ lSU� ( 866 ( 88Z 8LZ ( 89Z ( 8SZ 87Z I( 8£z ( 5'i£z S'IZZ 1 [Z S "LUG 1 ( OS£ ( 8 Z7E ( SEE ( SZ£ 111111 S'1ZZ IIZ S 'IOZ 161 vL S' SSI 43 8 8E '1 Z 1 8SZ 1111 HE 87 see 8I .... ro -J LU z 0) E4 1:4 F.1 0 N EH -0 >- .0 r2 cL a E DI AMON'O DRILL RECORD J. S. CHRISTIE LONGYEAR MIMEO 1111 11 III MUM MEM MEM MO M MEM 11 11 III III I 11 I III 11 111111 111111111111 1 Ada /Ad 11 14 11 11 11 11 1a upon rss!0 I 1111111 11111 1 11111 11 1 1 u 11 11 11 1 1 II 11 11 ll 11 0111S °.5 I 1111111 11 I 1111111111 11 11 1 11 I 11111111 44 11 1, 1 ALTERATION I pis 1 as 1 1111111 II I II II 1 1111 1111111111 11111 II II II 'd3 III 11111111W 1 III IIII1 II I 1135 11 11 ££ 11111111111111111111111112 it ll I 14 1 11 1 !1 11 ll 11 11 la 11 11 11 EE 1111 III II II 1111111 111111 I 1 11111 '14a I '9 11111 1111 II 1111 II I II 1111111 II I 1111111 1111111 III II RI I°1 1 LIN oNIS`d0 [ looapaq pagoea1 Ail ied 4 Iggmi I 111111 III 11111 1111 I 1111 II 1 Qtz - feldspar porphyry - strong pervasive qtz - ser1 23 1 alt. with qtz veining - MoS., - Unidentified black 1 23 1, E ogAum - 1 d0 ajoq uz su pauTuaz auTJ 1 in part secondary copper or tarnished pyrite. 1 " Suspect wolframite - some weakly magnetic. ! " 111E111 1 11 ! 11 ,1 I III 11 I 11 1 __. pellydS ` 1 1 " 41 44 11 EZ 661 861 0011 66 86 8fi 661 00I1 S5 86 86 561 56 56 S6 56 56 56 861 861 86 86 E6 L6 C6 L6 S6 Sfi 114ual ON 3ldWVS 1111 1 1 1111111 081 r8 ZS - 98 S8 78 118 1 1 68 10611 1 1 I Z6 11111 76 E6 S6 P L6 1 86 66 1 00ZT lili I zo I I £o 1 1 7S 1 190 I ILO 1 160 - 1 z1 1 ET 171 51 1 91 FOOTAGE 01 87 1 89 1 8L 1 88 1 ca:c 8ZI 811 80I 86 1 87T 1 1 881 I 1 89T 1 8L1 21E £7Z ZEZ S'EZZ SIZ gOZ 861 881 EsZ : 2 1 89Z ' 1 BZ r , 8 1 81C c, : 1 ? 1 85E , 0 1 8LE 1 88E 86E wa.j 85 I 1 8L 1 . 811 801 86 88 8 E1 1 87T 1 1 851 1 891 UMBIEMII ®_ 50Z 861 881 SL1 E9Z 1 1 8LE 1 d ro DI AMOv, DRI LL RECORD S. CHRISTIE Approved by Commenced '6eW Ado /Ad 1111111111111111111111111111111•1 11 eleA / ssip 11 , . 4tlin$ 1 1 ALTERATION 11 � I 11 111 tl� I _Jes 1110111111111111111111111=1111111•1111 Mill 1111111111•111111■1111111=1•11M111 01111111M1111=11111111•1111•111111 111 0 13 1.14J ._.I. r8 I " I 27 I M 56 MI SAMPLE Length No. • I RI M=1111111111111.11M11.111 d0a.LOOd 01 CO CO . W014 CC Crl C CO 0 -7 i smi 1-4 >4 ro —10W E JOD 0 6 r 0 0 E E E - 0 c a a 0 0 0 0 71, 0 0. 0. GMC Data Report 369 34 of 56 DI AMC DRI LL RECORD SEPT. 26. 1975 Q 0 DRILL RECORD Commenced I IIIHIIIHII 11111111 11 I 1111111111 1 • rnish 11 11 IIHHIHHILHHHhI[tIH 11111 -g /o, • 1 1 1 1 -. Ilia • 111-1 UI - IIIIEI' 111111111i1111111111111111 IF T S' S S C S' S' S' S' S' 1: RIEII IIIUI H N IIIIl H 111111 -111® .. 1-1-1-11111-1111111-11111-1111111 __--__, NOLLVHJj1V um � IIImuuIm mil IIIIIumI1o ■,",,,,ill IIIImumm,,■,■„ ■ -■■ �it a""' �i ©�'ai'i© © ©© © ©© ©iRir.�O©�a - " 1111■■ ■■11■■■■ 1■■ — ■■ - ■■■■■■■�■■■■■■ ■ ■ ■■■■■■ ■■ ■■ ■■■■ •IIIIHH HIIIIIHHH HHH III ■IIII11111 �11111 11 11 I III 11111111 11� "me u 1 n c 1 'Light grey to tan hornfels - 95% leached. 1 1 As above - cpy strongly replaced by Cc - 65% leached 121 N jor Cv it - 50% leached 2 a 11 PauoaaT %OS - anTsuAzad sz uoTquaa3Ty mracalc Quartz sericite with mod 70% leached 1 ;1 to strong quartz veining, 60% leached 1_ ,Tn most sections hornfels 30% leached i _L to sugary textured quartz 5% leached 1 L: ericite rock but finer 2% leached 2 rained hornfels relicts 2% leached 1 H ... 2% leached Cc or Cv 111 2% leached replacement ill ME _ N 61 ug4 z %Oc iauoani ) zgaenb pup uoTeaal.Tfl N ©©© vein intensity weaken leaching top 2 slightly downwards - pyrite 1 content increases. MoS w 252 aakrr than 1 ■®©©1,11111 1 dog •asuatouI og sauaade 1 L. S6 L6 S6 z6 °i M•• = w itMr MIII SAMPLE Length No. 11111 ■ ■■1111111111 T N ,1,1 q O 00 N H c000 AN r t I, 108 I QN 1242 77ZT 8 - -,- E7ZT 81T [tJ S7Zi 8ET 8ZI S 97ZT 87T 1 SCI III ��Ly ®® 10Z MaIIMICANIMMIIN i 7SZZ f SEZ l2LZ ESZ1 I hZZ 6IZ N S ZI 8 Z Z a N N - 0921 90E 76Z , 65Z1 76Z 78Z G9(1 tGE S l6 19ZI STE 90E FOOTAGE of f P '.O 'O O .o n N au ill Q 0 DRILL RECORD Commenced 0 E Corninenmd OCT. Approved by CHRISTIE 111 MIN III 1 •Beal IIIMIIIIMIIIIIIMIIMI 1111111111111111111M11111101 1111 OK - II _MI 001 EN= 001 MUM OS ®© MEM MIN _- AdorAd °!mn 4dms / 55 10 NOILVe31'1V 1 11 , ins 11111111111111111111MMININ =II III 'a3 1111111M11111111111111111111111111111111 III III • d3 11•11111111111111111111111111111111111M1 IEEEII 1 INN 11111111 11 111111 11111111 MEN '13 '143 !8 11M11111■111111111 1111=1111111111111111111 11=11111111111111111111111111111111111M IMIll IMII 1 3>1 111111 11=111111M11111111 NM ,, EINIIIIIIIIIIIIMINIIIIIM 01 01 01 CASING 1 Ferricrete and deeply leached - hornfels hard and naapuooas a - 3 • - - .• -1 auo-e mnsanO - sTa;uzoq daaa 0 1 •payi asuap 1 copper throughout. Alteration is fracture controlled • anisanzaa -uoN la : Lfi Imummimommum is 1 Imminimmi SAMPLE ' No. LSZi NO FOOTAGE 41 ss l 11111 wo. ° I S I 0 E Corninenmd OCT. Approved by CHRISTIE 10) 1.4 › rcc.■ Z • . Z a. • 0. 0 4) -0 8 - a 6 Z E E. = E E "a 8 8 GMC Data Report 369 37 of 56 DRILL RECORD S. CHRISTIE Ado /Ad� + I .-1 1 ALTERATION q0 'd 3 X ) K > '140 m AN ON15VD 1 > .1- , }-1 a. cr. a ..- R 4- C C 1 fc ..- C. L .0 I 0, 0 L •C c. ..c (.. 0 i. suian z3aunb gipm AxAgdioa zlb •q'TE •xas - alxsnb dALSanxdd yULe4UUJ •- t'LJJd.LLi - de's potloyd•1 0 .ri t‘i 0 0 .1-1 W > 4.-. a $. .).0. CO ? 1- CO > 4t1 -W c) 0 I. u .,.. 0' ..-- 0 L. 0 s- a .0 - a 0 re some clasts but some granites and hornfels weakly •paxalje1 uTzoaig I 1 1 1 , 1 Partly leached - up to 10% pyrite - disseminated . and fracture in some of the porphyry clasts - As •wETTszA aaddon oN - 4uamipasj o!.siajuxoq 71a delo SISOS UT a7?xCd sa mo[l 0 0 SZ O*! 0£ 1 II' 'oN 31,11NIVS 68Z1 NO 06ZT 1 Z6ZT I6'LE £6ZT NO FOOTAGE Oi 1 C) 0 .— ...t C.1 r.-1 VET a, Lek .-1 0 ............ 0' ,./ ...._ .... ... .... . -1 0 ,--. 4--L ....1 .... 01 - 7£T bZT -....1 ....1 1-4 ..... 10) 1.4 › rcc.■ Z • . Z a. • 0. 0 4) -0 8 - a 6 Z E E. = E E "a 8 8 GMC Data Report 369 37 of 56 DRILL RECORD S. CHRISTIE co 0 0 GMC Data Report 369 38 of 56 MARIO DRI LL RECORD J. S. CHRISTIE 0 rd 1-1 f..... . LI nzi 3-1 Fr 1 . Ado /Ad I I I I u,aA /'..lo N 04 N —i ,-1 —, —t . 4 � InS ,--1 ..--1 ,--i F Lrl ALTERATION In --.----, d3 I OS I X X X > ...- Ago X X X dN Leached cap. • - I - • . . . • • • a . > Q .ca co 0 4 1 i-I 0 .1-. .• !"-• ' anzsuaauz aaom nap saz;gatjzs Zaao' anq anogs s�I v. .rq ,-i 0 0 al K Clk ..0 co .4..k .3.) g * 4- ci in ,--1 0) LW 0 /-• 0 = •- r-- i. as matrix appears to be intrusive - or alternatively a ao paasiaaa.zq aq &au[ anzsniauT oql. so u aq 1 zed eToaaxq c 0*t� c GC in 061 06 ... ON 3ldWHS -.1 a cs. Z c• 9621 1 a cq Z c• I QN 1298 66Z1 NO of cc 801 cc - cc r - cc - 88i 1 ZOZ FO O' WO! j, o _... ..... ....... cc . 86 cc ,_ .... cc _ cc --d- ,.... . 8L1 . 881 .. . co 0 0 GMC Data Report 369 38 of 56 MARIO DRI LL RECORD J. S. CHRISTIE HIIIIIIIII1II ftIHHIIIIIHhI_____ IIIHINCHII!_____ a ] 1III 111111151= N ® El Ti En' FI I IuI ,,,,,,,, IHhIIlLF1U ■U� Ili I imom UI� a Q II1EREDIEI■' ®„ ,,,,FH■' ,,,,N_■� � U,,, E 1 INNN0 p ail - iii rASTNG. Leached cap - quartz teptapar porphyry. QFP as abnvp hilt only si � l r; _ a _ l 'rn1F rernvprasl. _ Strongest primary and secondary copper on cpy and oy - best eco er of a --se o OFP aa_above but only ill,. d C C a G C rJ C c(. c at 4i .,� CJ : V • t I • • • - w a • • i c • C • c . ¢ C N C a V NE • w N Cr c. • . • C w 't • s ¢ Ere C a .r , a 2 ° 2 Q t c .- c .— C .-r m ,--a c - .- p- m .- m ,-I m .-r et .-I •- - r a J• C' ,- � - O c*' FOOTAGE 1° r~ — of al CC aC u' CO m CO « .. .. cc - .. CC a• a. rr .y .. • N W .°I c•l cr, .--1 r•l .i N W. N .y .,j it iC c• c .7 n c. E a LL 0 1 N ^ c' K cC .Y CO ic1 i o C ,4 • • • CC • CC • •• CC .- .- CC c. .- • .- -E r• ., N CO .� M Q+ n' t- N C. d .T u` c. r .t ,C c. I tttl 4 :4 CNI C '0 C J rQ V 0 rtl c 0 C_ 0 c 0 a 0 ..J a E U 0 GMC Data Report 369 39 of 56 DRI LL RECORD Commenced zn 0 0 0 0. 0. DRI LL RECORD CANADIAN LONGYEAR J. S. CHRISTIE Vertical •Seyy !A /Ad ONEINUM G£ In LZ elm Homo mom u1aA rssw li in moirmicm L. ,a m •• .un Ind Z -T Min sommomom ALTERATION 1 'IBS umilhonamon damn n mom i 'q3 1 N o n En mum n 1 1 i m d . nu NE I mop 1 is 1 mil 1 E LaS nog II •el I 1111 nu Ine . al IMEENIMMEMP 111 I . 13 I "NO I !LI I O I x 1IIIIIIIIIIIIIHh11IIl1I11HI1I1IHI IHIIIIIII1HIIIII1IHIIIIIIIIIIIIII 111111MINEW "Ill"MONE I 1011 1. I IN I 141..... NI 1 •auiutan zab yawn •aas z1b •naad - 86T s3 4 pequo3 'SaS<JLLL a zsuo UT - 1Ty • • x °daialdzod •p[off za x NUILI mmo •9NISVO Leached cap - traces py -cc. E Partly leached - quartz feldspar porphyry to J about 110 feet. i iiiii I AMEMEMEEICEEMIE ELECE HEM 1 OL gall I maam maam 56 S6 • 0 • 56 56 06 MENEM HEE II I II INIMMIE MINEMEMEN 1111E MINCEMEMMEIN 1 II, II 111111011111 57£1 76Z 18Z 771.1 T 8Z UL G £7E1 ULZ 6S1 Lit L bSL LSL l7ti LSL 1 U7tl [VG USG 6E1,1 UEZ UGL 81LT 0ZZ TLZ L£E1 1TZ LUG 9£E1 Z0Z 5'961 5EET 5'961 681 7£ET 68T 8LT SSS1 8LL 891 Gehl I19L LSL ltt€ LSL Sil U££L S7L 8hl 6ZE1 8E- 661. BZET" 6Z1 1Z1 LL6L ILL Sll 9GEL Sll VOL SUL 7UL 7b 7Z£ l 76 S8 EZE1 L8 89 ZZE1 89 85 TZ£T 85 87 OZ£T N. 87 8E BE £T 1 SAMPLE No. FOOTAGE 01 Weld zn 0 0 0 0. 0. DRI LL RECORD CANADIAN LONGYEAR J. S. CHRISTIE Vertical cts L al C O L C N 'an' C C ..1 w a, DRILL RECORD 6eLry III EMI I I HIM HEE 1 1 Add /hd IN I T° EH I 1 11 11 Ell • I 1 dla A s!.a HOMMEHE ME I 1 R RE T' 11111 II I 1 1 1 1 IHO MUM 1111 • NOiltruari V 11 € IBS 4O il 1 E II 1 IN 111111111111 11 I HEE m mom 1 da Emommommommumni 1 1 iii II r pm IMMI 1 'Ja3 11 il 1 NEM ME I II MI II I 11 1111111 I ME 11111 '140_ I CHOI 111 II ... III a) MEI I ME I I 111111111 di II x II I I •aaaaaTaie3 I Porphyry intrusive - strong secondary biotite Weak xacture and dis. cpy 1 1111111111111111111 11 I ME S6 HE II El HIEN II I EMMEN i ll MU M MINIM EMI MOM 9hET N.4Pua Eh yt 6t, N aIdWVS 3 OVJ 111 EMI 1 I HENN IN II I II I 11111111111111110 IN II IN LOO __ wa,d 1 1 cts L al C O L C N 'an' C C ..1 w a, DRILL RECORD 11 ,..... ! immme. ......... ... 111111111111111 11111 1 ........ 1.1 1111 1111111 III m I m ..... . 11 A . . 11 imam dirimm—s.m mill" 1 . 111 111111...... .. ... H... . .... ... . ........... ...... ...... ". ..... . I 1 ...""""" 12 1" 1111 Ilml 111111 11 WE aliliiilliiiiliels IIIIIIIIIIIIIM MI= 1 I I III :slusmZPaj (•alias zab) anzsnauz 3 sTa;uaoq -. arusy pyrite - much with chalcocite coatings. 1 CI II I OVERBURDEN Leached (38 -133). 11 rr Qtz sericite (intrusive). S9 HL-' =I 1 1111111111111111111 0£ III Ill FOOTAGE SAMPLE 8£ 0 o L wasj ON 81 1.9 86 88 88 8L LET NO LSI S7I S�]l 8Ll 8Z1 8ll 81T SOT MI ZS£I ZS Ell 1 • • 1 95 T 8S£T 1 111 -11.1._ MIME 881 891 891 1111211'_ i 0£Z 1 71Z 1111 - 6Z_ 81.Z 5 06Z cn Q y 0I cn m . z 0 DRI LL RECORD L 11 1 111111M11 II 'Bogy 1111 M EM IMO= I 1 MN= -- Act3/Ad °IeA 'N % ss1Q % MEI HIE S• ST S' ST ET ST Mal S' S . I s AWE - - -1111MIE 1 NOIJ,yly31'ltl .ins •13 MIME 1=11111111 =MN •d3 MEI 1111111MIIMIIIIIII �� •Jas x 1 _ _ 1 1 11 11 143 111 IN IIIE E IIMIIEIIIIIIMIIII III AN 111=111 m II II CASING oTsia ;uzoq pazagiu £,iquTxun duo pagousq 1 anTsunaad oq a2u4ias san4oux3 zquamTpas 1 .(iasuaIUT azom - uoTgaaagiu saTo?aas zgaunb altered parts sugary textured but fine grained and non porous. Strong fracturing. 1 1 1 •qS su 142T11 si quaquoo apTgdins iuuT2T1D Live liminite present. Relicts of sulphide from 1 -duo uT aoaid oq sou EMI Sericite selvage alteration in sulphide veinlets. 1 x 1 1 - •anoqu sv Alteration slightly more pervasive. 1 x ME X 1 • anTSUnaad axom LTgg2TIs uoTavisaiv Stronger alteration and re-- crystallization. 1 x Minor MoS,, associated with quartz veinlets. x I •anoqu sv x11111=11110 x 1 •anoqu sv 1 8Z E8 90 £6 B6 T6 ESTI 4S '96 OT OT zI ET FOOTAGE 1 SAMPLE f 01 WO .. j ON 1 IT 1 0 1 1 1 9E1 1 TT 111 ON 1042 1 QN 1043 1 QN 1044 QN 1045 9 NO L+7D1 NO QN 1048 anvaanv 1 7 1 71 EST E91 ELT 18T E61 90z 1 9E1 1 7 1 71 E91 ELT 1 1ST £61 N 0 a 0 y O rn 15 J C d � 0 G N E E E U U DRI LL RECORD J. S. CHRISTIE Mall Atl /Ad MMIENHOMMEM El MO MEM NM IMMENIME OM Eli 11111111111111 II MEM MEI El - OHM MN EMU Mill 4tllas 1 MON MU II MN HMO= IIM. I MOM= i. ® '47 Hill 11111111111 NH MEI 11111 11111111001111111MHEIN ®'gag 1111011111 ral= EH 111111111111110101111111 111 d I 1:11111111111111 I 17 "It17 I9 d; 0 I 111 1111 x I El I I dullmll ME Iffl 1111111111•N no I 11111111.11 11,1111 1 ME NOINKIM IN OM1SVO 1 Leached cap. Feldspar porphyry with some quartz eyes. Variable generally pervasive quartz sericite alteration. Local silicifi— 1 cation. Live limonite? Minor quartz veining. Alteration and lithology as above but with only minor leaching and chalocite enrich— f 7eool •s4aTulaa zlianb 2uoia Tu go quam 1 copper cartonate stains and thick rims of •a3TalCdo3Tego no Laal:oo3Teg0101TITTAao Less intensely altered feldspar porphyry. uo eaTzolgo fsTo olToTzas anTsunzad some fractures. Chalcocite present but • )pool aaTDTzas uT usga ssaT LTgagozd ni 5L: a}17o.A uluuogapa 1addo3 ga 1oo2 paaa3Te a;To;.zas zasano a 7CYaa- - anugrr su xooz aaTzoTgo heTo_aaToTxag i •zaddoa 5sa{ pua psiag-[a .CTasuauT ssaq se Siooz pazaaTe a4ToTies zazenb eATsEAaad • 21.1rsaazouT auaguoo aa?x.Cd anq aAoge Quartz veining increasing. MoS,, increasing. •aaeuogaeo zaddoa aou-r. 59% Pervasive quartz sericite with heavy Pyrite and quartz veining. Copper grade diminichp aaith nurdto ....,r.7.,r K ..�. ....» and MoS,, grade increasing. Partial to almost total leaching. 258 to 264 - I WE MEM= El i . 96 66 nnr 1 6L S 8L I ZL _ OL 94 1 6Z � 7l t 11 E 0 1 MENWIMMEENI MIN OT .9 L a , 9 - - t "aN 314WVS . 0 O' . . 0 Ce 6901 Nd Lr, QN 1070 S Avera . QN 1049 •N 1050 .,i u, .0 dd _ N 4 US:i b anva_ood Vy I }Z s6I ( 0 1 72 (ILZ 271 INTERVA 6L ILL wo ZLI I L'/(. 561) Ohz) 3 DL I 6L LL 0 } 0 0. 0. S. CHRISTIE J meg HEM HIMINNE II MEMO 6rlN MO iii EMI HE II I INN IMMENE. OM I II HO =MO Adz /Ad ulaA /-ssl0 in i ii HEME EM NENE i . y0=hs •i uiiininuiiiunuu iiinniiunun I Him HEM NOl1VFJ311V 1'5 EI II 111111 11 11111111111111110 NI u mononumm NH II 11111111111 moon n nummumw as Ell I •03 I vag I I NE 1 km il NI i i nmBpmommm I IN IIII . 14a _1 1 .�73 mom lummoin mum= mil mu 1 n 11111 MEE nn I MEI 11 11 MEM I I Ift MUNN III I I HE II 111 RI ; £L �hL L6 I £0T 11.111E111111111111 001 £0T 66 I COI I ZS 19 L9 MI 111111111111 r'01 j k -El OT 01 01 - 11 zT hi I!! 11 HI EH II MEI HI SAMPLE Na. 550T Nb 1 9501 NO QN 1057 '' 850T Nb ! s2 Z901 Nb i90i Nb 1£901 Nb QN 1064 9901 Nb IhZ ,5901 Nb 6ZZ 11111111111111111 111E ME I D08/1003 01 S'TEI 0i1 6+7I 11 hOZ 66T 681 6L1 691 681 ISJOAd TZT S' I£I 1 . 1 017i aaP, P .,J.L„,. t CiN 0 1 70Z 661 6ST 6LT 691 651 6 6ZZ STZ •• . 1 i i,� 0 z 0 0 0 Q .0 4 DRI LL RECORD J. S. CHRISTIE Commenced c c m m .a m C/] P�7 0 Z z ¢s IY7 � R+ u y >- 0 0.7 2 Q. a m E 0 o y 0 a x o u 0 n a Logged by J. S. CHRISTIE DRILL RECORD 111111 11 111 1 1 I II 1 1111 11 �.W III c5• 1111 I S ' 'III 1111 111111111111 11111 II I I 111111 n MI I- AdarAd u?aA f l rssip N dms S'T 1 S•T' 11 BEI :I ' S'T 1111111 1 111101 11 ALTERATION 1 1ms G3 d3 'A85' 1 ii II 11111111 III I 11 II 111111 11 I 3>I II 111111111111111111111 I I 11 alaenb ae senzad STamaaaxa ian X/Sgdxoa sericite alteration and recrystallization. Fracture 1 sulphide leached in part to depth of 62 ft. Chalcocil (,occurs as dis. grains after sulphide and as fracture 1 coatings. Relict sulphides are pyrite and AT3g$TTS aae sxboa •13 Y ZL 01 •alTaxdoDTega I _ 'PaTST ITi From 72.5 ft. onwards alteration is more likely sericite clay although quartz veins and silicified Igneous textures are evident. Strong chalcocite mineralization continues through- '13 i i o1 Tenxalui ag1 lno1 in faer,, he the mineral which forms dark sne -k k throughout the rock and previously called •ahooniego uo gaTm uoT3e3T3TnrTi8 spavmuo 'ET moi3 of original textures is the most common alteration. I Much fine grained black material may be chalcocite I or deeply corroded pyrite. Minor fault gouge at 1 I ATauoags aq nem uo TET moa3 uoTloa5 •13 S£Z recrystallized hornfels? Post mineral occasional post copPer pyrite veins, andl minor MoS, along quartz veinlets. Strong quartz sericite alteration. Quartz veining with fine dis. sulphide remains fairly constant for rest of hole. Coatings of covellite on Ghalcopyrite are 'aToq 3o molloq as luasaad TTTls l 99' Z s' l 6S 1 96 L81 LL 9C1 6E1 Z 81 I LLI ZT TT TI is•6 : S•fi 5'8 S'OTI SAMPLE No. ON 1080 I TROT £801 1 580T 1 980I 1 1.80T l 1 880T I cc 1 060T 1 T60T l 960T FOOTAGE 1 aL 9£ 55 S Z8 Y 06 l TOT l L1T l 7ZT £ET Wal I SZ 1 L7 E9 I S•zL I Z8 Y06 801 1 Fi ZI c c m m .a m C/] P�7 0 Z z ¢s IY7 � R+ u y >- 0 0.7 2 Q. a m E 0 o y 0 a x o u 0 n a Logged by J. S. CHRISTIE DRILL RECORD 0 0 0 DRILL RECORD J. S. CHRISTIE Approved by commenced VERTICAL LONGYEAR MIMI 13 W 1111111111111•111MIMM IM hdo,Ad 1=111 al Ill NowN■ri■ramminumm IIII MIMI Ell m MI .. ............. ALTERATION 1 % I IMMIIIIIIIMIIIIIIIIIIMMII 'In5 I '40 I 'da I ' +a5 1 'I' '4d1�8 1111111M111111111111■1111M1111•1111111111111111b 11=%Nimm..■■••• =MINI 1111111=1111=1111 11111111111111111=111111111111111 MIMI OMINIIIIIIIIIIII • 111= I — I !8 I del 10 IIIIMINI MIMIIII • 11111111•111111 • MIIIIIIIIIIIIIIIIMINEmimilIMIN =11111 111. ' , MENMEMEMENNEEMEMEMEEN 1 1 061 01 1 7 615 7I 1 ( £6.15'5 1 001T 1 I L81 8 I TOTT AMEMINEMENNEME1 1 1 881 6 1ZOTT 1 681 1 561 OTI ZOII I 661 1 1 661 oil +7oTI 1 60Z L815'8 I SOTI 1 S'LIZ 1 961 0119011 1 S'LZZ 1 TOT (5'T11 LOT 1 6£Z 1 c - 2 — c, " - " 1 SS! L 4 TM 69Z 111111 88 , S ZITI '7LZ 1 18 1 L f ST1I 1 £O£ 1 I 1 1 AVERAGE 1 1 84.7% 1 I ON e1dwvs i z 1 860I 1 6601 1 FOOTAGE __.......... . 0 ZsI 1 5'991 ZL T 081 WOl 1 1 Z+7I 1 Z5T 15'991 [ 1 ZLT 081 681 661 60Z S•LIZ 5'LZZ . , S■ , , C, c lf C • 69Z C u C 9.Z 0 0 0 DRILL RECORD J. S. CHRISTIE Approved by commenced VERTICAL LONGYEAR 1111111/11 tt II 1 1 mom loll ■1■■ Ado /Ad nlaA o-ssla ..■.. ��iII . III _ illi I IIIIIIIIIIIII mmalun ■ ■ ■ ■� ■ ■ _____ IIIIIIIIIIIIII INIMINIMMII =011 11■■ . 4d1 „ s l■ ALTERATION ■11111 . I.S III 'Go II II 'd3 11 II MI = I ■ 'Jas ■•• xi . ■■ 1■■■■■ ■ ■■ .. ■■■ ■� = 1 11111.1■■■ 11111111111 ■ IL. ■■■ �■ 1111111■■■ 11111111111 II MINIM ■ ■ ■ ■1 ■1 ■ii 11111111111 I ■ ■ ■111 � 1 ■ ■I■■ ■ ■■■11111 CASING . 16Z o/ SuTgp TETaaad - dsp pau'osa'I IL sT a ;TaAd. - aATsnaluT :Utp1ion paaa /Ta DTIITV.V 1 8E 1 ZI 1 67IT 1 9Z .__ 1 in part deeply corroded and in par t bright. I . M • r V a F I Q i t t 0. F C F a 4 R I - 111MINIIMEIll 11111111 anTsuAiad sus' nT /'OTTs zuTmopaq up- pale /TV I 1 1 -41311 S'911 M111111111111111 pus...sYT4s •azT.IT o -i 3o pT paI.atas1c TZL aq neat aATsnalui •saanaxel snoanzT pT1Tin.gaaod Lads uT TsaauTm agET - aauao0 /Boa 1 1 1 1 1 £9 1 6 1 191T NO 1 O£I 1 1 1 1 -40u 1 l 0171 . _- Q S � 1 70T 1 01 1 8911 MO 1 091 , C nn C M1 c I I I paTauss I( ZaI 1 • • NO Z•I 1E1 El °. 9 :9 Z9 1 t, 9 87iT Mb 71 INEIME ZI .•8 `0N 31,INVS 1 EIMEI 111111111111111 911 90L SSTT — L6 75IT 98 £SIT 7L ZSTI 19 NTT S'ZS 0I1 6E d9V1OOd 1 0l c W0J: C W 1 7T C7Y `L Q ,. L6 98 7L L9 S'ZS 6£ 9Z C7 M I - _ TZT .. r v M1 Z8T i 7 m —J 2 0 Approved by CANADIAN CHRISTIE Commenced 111111111111 111111 I II 11 I 111111 11111111111 III 111111 I- 111111 111111111111 1 1111 u!aA AdplAd issIO I - =1111111111 1 11 11 . gdins I 11111= S 11111111F Eli 11111:111 CI ' 6e1 N 11 16 ALTERATION 1 IIIIIIIIIIII Ins 1111 11 II IIII 'G7 'Oa II II I 1111 1111. 1111 ' x 41111 1111111 1E11111 !EA— I 1111111111E111 Mill El= 111.1 I 11 1 1 11111111 III 111111111111 III 11 II 11111111111 II 1111111111 m 1 ce d)1 .1 I , 111111111x 1111111111111Ni 9NISVD Leached cap - strongly recrystallized 1 porphyry intrusive -- pervasive quartz Suiu -an zaxsnb Nxotooas gaTM aaTzTxas sulphides totally leached. Pervasive qtz -ser. alt. porphyry. As above with pyrite (mostly corroded) and minor chalcopyrite with covellite veins - Trace Mos 2' As above - strong tarnishing and corrosion of gapp A`1Enn laud uT ail suTan zab - sap Wins •aanaanaas gwoasli000 As above but quartz veining more intensive. 1 1 • anoge sy 1 a�I�P P@IIT4 TT 0118 (ICE[ Suzan zaasnb uo saoeauoo • anogrr ss 441Cydaod pdad41 d41.oTxds- caaeub uo IEE 0 oa3 ▪ anoga sy •anoge sy1 From 403 onwards alteration intensity weakens and 1 •auaasdds axe saxnaxaa snoauWT ao-Taz At end of hole igneous texture is obvious. Rock is quartz feldspar porphyry with strone 1 I secondary biotite in matrix - Retrograde chlorite 1 •suTan aaT.Ad aril 3o sa2sATas duoiu auasaad sT End of hole 445' 06 s81 561 081 ISL1 SAMPLE N o. num LZLII 1 ELII SLIT 1 LLII 1 FOOTAGE 0 1 1 S9i III 661 1 6ZZ 1 L 'E Eo17 luosd 59I 061 6!Z c n mm 6EE 1 58£ fu CU 1 0 C U Et E U DRI LL RECORD Ei cJ FO fp al 2 —I 0 1.41 Z E 2 E o I0 E 0 GMC Data Report 369 50 of 56 DRI LL RECORD J. S. CHRISTIE '6ov1 111 IIIM M1111 11•11 11111111 111 111 l Ad o/Ad MIN 111 114111111MIMMIIIIIIII , IIII ulaA �•cslp NM I 'LOME as Illrlli==IMIMIIIIII MI ALTERATION 1 'Ins I IIIINIIIIIIIIMIIIIIMIIMII 1.111 1 I IUII 11111111111.IU J d3 _ 1111 •,as rr. -, MI d 1 I d'N 1 I OHI SVO I rn csi "1 • aUTUTSA zqp KXAtgaso0 aAa zqp - Quo pag'JeaZ _ — J II t; 1 ATTuPlud Traces chalcocite - becoming stronger downward. 1 r then diminishing from 130 ft. _...... 1 " 1 _ OLZ - TCZ) l r u•xo. ._. aJ z1 • .A..q - t - IOU ' 1 1 ,. ' " tzIE -z$z) c c a X C PI 01 ... •C d > C X CY A- C P: 4 it 4- a C c. t Alteration is extremely pervasive quartz do uT aTTzTaas N--- bi 5 8 'o>s 37dW VS 61Z1 HO OZZT ,4 ri C■ r■ CP 1■ .4 ,. Ir ,- .L r 1`.. C. CC 0. r - CP C`. r OCZT T£ZT Z£Zr en CA . — .1- C\ 1 — Lr C \ ,d kc C 1 r C. 1 — cc C. &• c c, , - H CA v■i 3OV1O03 al -- it h - CO £6 C7` C 1 — C. ,1 . — Lr H .t H h - I — CC I — 661 9TZ 9ZZ cr 01 ..y. CN th C ..0 C r - 04 cc C. c i r. CPI [ wo ?d C C. Cr cry 0 T8 i Cr cn a kc C HHHH a •-• cc c• ,. -: c- Art H -y , z T. e• N n. L81 661 ,6 <- l X r4 C•I Q CA 0" cl Cr c4 q• c. a- C cr C, a, Cr) Ei cJ FO fp al 2 —I 0 1.41 Z E 2 E o I0 E 0 GMC Data Report 369 50 of 56 DRI LL RECORD J. S. CHRISTIE PYRAMID COLOR ANOMALY 10 000 N Dock Prepared by: J 5 C Drawn by ATK Dale : March 13/75 Rev■sed: MAP AREA QUINTANA MINERALS CORPORATION GMC Data Report 369 P Y R A M I D P R O S P E C T LOCATION MAP SHOWING ACCESS ROAD SCALE NTS Landing Croft Discharge Pohl" 51 of 5.6 i DRAWING No. r r • .' Marble Pt Shingle Pt it - ° Bluff Pt' - -. + 11erende Bold Bluff , V''', -Gu11 I pt / trc "CtciwPt aW { encei 1 1 Pinnacl 4`'° i .,__Gravel '. f _zpo ...-• i : Pea +! • 1 Ccr. 0 .114' ''c? tD , O 1 ; `o ff I PyYahti �. . M tc7 L, eftharld Ba Vn9 5 Petty ? 5, V " . 4 i e `A I ks, ri " r ) t,t . .- Cove: , -7'n\. ,g 2QO1' —,\\ Coarsnarbor.., — , Round I • (:--)-:;,. { . ".,'� •� Q , 1�,' \` r, wi *" and t- ' L., \ 150 ,:., `+ . Dark Cliffs F \ `t .:F4 �' ) . v , � °0. \ �� '' ,� S(.' f � l , 1 4 � 0 1 t L i ' � ' I� nO' t c,---.. �s � 1 �rt, �tU . of i CoaalBtuJ -1 :iIt L fb cotitis ; r arr p ' > c 4 i ett 1 -,, -- " * Baiia - st I eolith. Pt Cabi 2 00 .. -, os ". X l .„_____ : , 7 tr U G A i N 1Gul3 While Bluff 1 � (:■-• Sw { Al u e1 C. Jerk • ,1 ,' "� ''' -_. Guillemot f r`J Lion r ( ) .�'i l * lwr Bay A li 1l�o ° (Z � _ f Swedania Point West Head I t r d O r p � ie i 5.1 San D L3ay 5 CG N orth 1ic, ',Jo d,1101„ . {` tl I r z d1 o p \ t \1 i i � U t . iinelr� f 3s p ° /� / �:9]. "ouFlll `Z - N v d,.� Area I w� ._1�� a n d LJ u o O, • poll, :arC' a f i o, \ io .., i� Q.... �'. ,. t 1 _g6 I \ ti .. g0 (- U JG o .St, AN . Da ��' K t p .,- ti ff t 1 h o\ D 6 .., � 1 • -- e� 8 v s,, , East Head EirxtC R ' H" h 1 *0 r • Renshaw Pt T 53 f " ti, u;O ' o Vi j �)` y\� i 1 }I: :rlv r I / c.),G1 4t)DatiReport 15,rrt:lu flu ft I Popof Head ru l .. 1 � . Q -. a _ • -•\. ^ \-\\ kPCk M1i Cr1 -. r��c e E31• :prrieYr J J_ .. _ \ 1 0 • U • r L ,4. i S �p0 ., - •' \, -.. y. -. Little Noruvt,u • 3395 0o 4 C, i 0 l o ,' Ndf „r! V rj✓ 1 Mt Stepo 0 o p � ')/ �• l I "It Elephant f `” ._.'Blunt Point � Karpa I + Scotland Rock 'lam ,tip I : , � � *+ / f 9,S c otland Point • l �h y_ I :7") ^FC ctrcvin. Is' and • [CK * +" ar,. - 1 55 (11416...) p0 V 'F J + pape Devine S }0 Gut'u' alt * Lt c7 r. , LF •. ! 3 Andronica ; YAEh1 ' Island ' X1175 z yo , c J The Vkhateback - {!r The 4 '• Haystacks 11 •r.s w a = r p 45 LESMILL ROAD RECEIVED SAMPLE(S) OF Element Sens* Antimony (4) Arsenic (4) Beryllium (2) Bismuth (2) Cadmium (4) Cerium (5) Columbium (4) Chromium (4) Cobalt (3) Copper (1) Gallium (2) Germanium (1) Iron (2) Lead (2) Lithium (4) H - 10% plus MH - 5-15% M - 1 -10% LM - 0.5 -5% GMC Data Report 369 DATE Dec. 15, 1975 LIMITED DON MILLS ONTARIO NO. TO. Min -En Laboratories Ltd. Concentration Element Sens* QN 1242 -1247 +1285 ND Manganese (1) ND Mercury (4) ND Molybdenum (3) ND Nickel (1) ND Silver (1) ND Tantalum (5) ND Thorium (3) ND Tin (2) ND Titanium (2) L Tungsten (4) ND Uranium (3) ND Vanadium (2) L Yttrium (3) ND Zinc (4) ND Zirconium (4) Key To Symbols 2373 LEGEND L - 0.1 -1% TL - 0.05-0.5% T - 0.01 -0.1% FT - 0.01% or less ND - Not detected Page 4 of 4 INVOICE NO. Note; Better sensitivities can be obtained with special techniques, if and when required. E 445 -5755 SUBMITTED TO US SHOW RESULTS AS FOLLOWS: *Sensitivity (limit of detection) 1- 0.0005 - 0.001% 2- 0.001-0.005% 3- 0.005- 0.01% 4- 0.01 - 0.05% 5- 0.05 - 0.1% Concentration QN 1242-1247+128 FT ND FT FT ND ND ND ND LM ND ND FT ND ND T X -RAY ASSAY LABORATORIES LIMITED 53 of 56 CERTIFIED BY 77 a 1 y 45 LESMILL ROAD TO. RECEIVED SAMPLES) OF Element Sens* Antimony (4) Arsenic (4) Beryllium (2) Bismuth (2) Cadmium (4) Cerium (5) Columbium (4) Chromium (4) Cobalt (3) Copper (1) Gallium (2) Germanium (1) Iron (2) Lead (2) Lithium (4) H - 10% plus MH - 5 -15% M - 1 -10% LM - 0.5 -5% GMC Data Report 369 DATE Key To Symbols Dec. 15, 1975 LIMITED DON MILLS ONTARIO C . rt ffcate of c .ti.v510 ISO. 2373 Min -En Laboratories Ltd. Concentration QN 1219 -1224 ND ND ND ND ND ND ND ND ND L ND ND ND ND L - 0.1 -1% TL - 0.05 -0.5% T -- O.OI -0.1% FT - 0.01% or less ND - Not detected Page 3 of 4 INVOICE NO. 445 -5755 SUBMITTED TO US SHOW RESULTS AS FOLLOWS: LEGEND Element Sens* Manganese (1) Mercury (4) Molybdenum (3) Nickel (1) Silver (1) Tantalum (5) Thorium (3) Tin (2) Titanium (2) Tungsten (4) Uranium (3) Vanadium (2) Yttrium (3) Zinc (4) Zirconium (4) Concentration QN 1219 -1224 ND ND FT FT ND ND ND ND L ND ND FT ND ND T *Sensitivity (limit of detection) 1- 0.0005- 0.001% 2- 0.001- 0.005% 3- 0.005- 0.01% 4- 0.01 -- 0.05% 5- 0.05 - 0.1% Note: Better sensitivities can be obtained with special techniques, if and when required. X -RAY ASSAY LABORATORIES LIMITED 54 of 56 CERTIFIED BY _,/".0 RECEIVED Antimony (4) Arsenic (4) Beryllium (2) Bismuth (2) Cadmium (4) Cerium (5) Columbium (4) Chromium (4) Cobalt (3) Copper (1) Gallium (2) Germanium (1) Iron (2) Lead (2) Lithium (4) Y h a t 45 LESMILL ROAD TO. Min -En Laboratories Ltd. SAMPLE(S) OF Element Sens* H - 10% plus MH - 5-15% M - 1 -10% LM - 0.5 -5% GMC Data Report 369 Concentration QN 1193 -1197 ND ND ND ND ND ND ND ND ND TL ND ND L ND ND DATE Dec. 15, 1975 Key To Symbols NO. 2373 L - 0.1 -1% TL - 0.05 -0.5% T - 0.01 -0.1% FT - 0.01% or less ND - Not detected LABORATOR 7r1 LIMITED DON MILLS ONTARIO Cterti icate of Anak3si5 LEGEND Page 2 of 4 INVOICE NO. SUBMITTED TO US SHOW RESULTS AS FOLLOWS: Element Sens* Manganese (1) Mercury (4) Molybdenum (3) Nickel (1) Silver (1) Tantalum (5) Thorium (3) Tin (2) Titanium (2) Tungsten (4) Uranium (3) Vanadium (2) Yttrium (3) Zinc (4) Zirconium (4) *Sensitivity (limit of detection) 1- 0.0005 - 0.001% 2- 0.001 - 0.005% 3- 0.005- 0.01% 4- 0.01 - 0.05% 5- 0.05 - 0.1% Note: Better sensitivities can be obtained with special techniques, if and when required. X -RAY ASSAY LABORATORIES LIMITED CERTIFIED BY X} 445-5755 Concentration. QN- 1193 -1197 T ND FT ND ND ND ND LM ND ND FT ND ND T 55 of 56 45 LESIVIILL ROAD TO. Min -En Laboratories Ltd., Specialists in Mineral Environments, Corner 15th Street and Bewicke , 705 West 15th Street, NORTH VANCOUVER, B.C. RECEIVED Dec. 12, 1975 SAMPLE(S) OF Element Sens* Antimony (4) Arsenic (4) Beryllium (2) Bismuth (2) Cadmium (4) Cerium (5) Columbium (4) Chromium (4) Cobalt (3) Copper (1) Gallium (2) Germanium (1) Iron (2) Lead (2) Lithium (4) H - 10% plus MH - 5 -15% M - 1 -10% LM -- 0.5 -5% GMC Data Report 369 DATE 4 pulps Dec.15, 1975 1 LABOR LIMITED DON MILLS ONTARIO 445 -5755 Teri ffra e A al 5i5 Key To Symbols NO. 2373 Page 1 of 4 Concentration QN 1096-1099 ND ND ND ND ND ND ND ND ND LM ND ND L ND ND SUBMITTED TO US SHOW RESULTS AS FOLLOWS: LEGEND L - 0.1 -1% TL - 0.05 -0.5% T - 0.01 -0.1% FT - 0.01% or less ND - Not detected CERTIFIED BY INVOICE NO. Element Sens* Manganese (1) Mercury (4) Molybdenum (3) Nickel (1) Silver` (1) Tantalum (5) Thorium (3) Tin (2) Titanium (2) Tungsten (4) Uranium (3) Vanadium (2) Yttrium (3) Zinc (4) Zirconium (4) Note: Better sensitivities can be obtained with special techniques, if and when required. 2373 Concentration QN 1096 -1099 FT ND TL FT ND ND ND ND L ND ND FT ND ND T *Sensitivity (limit of detection) 1- 0.0005 - 0.001% 2- 0.001- 0.005% 3- 0.005- 0.01% 4- 0.01 - 0.05% 5- 0.05 - 0.1% X -RAY ASSAY LABORATORIES LIMITED 56 of 56
