GOLDEN RAWBOW CLAIM GROUP
OKANAGAN FALLS AREA
OSOYOOS MINING DIVISION
MURRAY S. MORRISON, B.Sc.
CLAIMS: Gold 1-14, Fort Knox l-10, Fort 1-25, Lucky Star 1-16, Rainbow l-4 & 7-24 (87 units)
LOCATION: ‘Ike Golden Rhbow Claim Group is locatedat Venner Meadows, 20 km southeastof OkanaganFalls, B.C. Lat. 49” 17’; Long. 119”2(Y N.T.S. Map 82-E-6W
OWNER: DoublestarResources Ltd. and M.S. Morrison
OPERATOR: DoublestarResources Ltd.
DATE STARTED: CktobeI 1,2002
DATE COMPLETED: October 23,2002
‘v Kelowna, B.C. TABLE OF CONTENTS
pAGE 1 Introduction 6 Location and Access 8 PhysicalFeatures and Climate 10 Claim Status 12 History 19 RegionalGeology and Mineralization 22 Property Geology 24 AU Prospect- LacanaMain Vein 24 Mapping Program- 2000 24 ExplorationModel For the VemrerMeadows Tertiary Outlier 25 Property Geology Basedon The 2002 Drilling Results 27 Drilling Program- 2002 30 b Site Preparation 30 Reclamation 31 The Drill 31 The Program 32 Sampling 33 SummaryDescriptions of Diamond Drill Holes G-01 to G-04 34 Discussion 45 Conclusionsand Recommendations 50 References 52 AppendixA Statementof Qualifications 54 AppendixB Statementof Expenditures 55 Appendix C Drill Hole Logs Appendix D Certificatesof Analyses ILLUSTRATIONS
Figure 1 Location Map (British Columbia) 4 Figure 2 RegionalLocation Map, Scale1: 250,000 5 Figure 3 Mineral Claims and Access 9 Figures4a&b Mineral Claims 17 & 18 Figure 5 RegionalGeology 23 Figure 6 RegionalGeology - Enlargement 23 Figure 7 DDH G-01 CrossSection in pocket Figure 8 DDH G-02 CrossSection 39 Figure 9 DDH ‘G-03 CrossSection iu pocket Figure 10 DDH G-04 CrossSection 44 Figure 11 ConceptualCross Section - Geology 49 u Figure 12 ConceptualCross Section - Conductivity 49 Map G-03-1 Location of Drill Holes in pocket 1
L SUMMARY
During October, 2002, a diamond dritling program consistingof four holes (613 metres) was conductedon the Gold 1 mineral claim of the Golden Rambow Claim Group by Doublestar ResourcesLtd. of West Vancouver,B.C. Doublestarhas the right to earn a 100%interest in the Golden Rainbow Claim Group subjectto work commitmentsand royalties.
The GoldenRainbow Claim Group coversthe southwesternside of the 12 km long Vemrer MeadowsTertiary Outlier which is situatedon a rolling portion of the OkanaganHighland betweenShuttleworth and VaseuxCreeks, 14 to 22 km southeastof Okanagm Falls, B.C.
The property is comprisedof 87,2-post mineral claims which were stakedbetween 1990 and 1999 by the writer, M. Morrison of Kelowna, B.C.
The dominantrocks comprisingthe Outlier are Early EoceneMarron Formation and sedimentsand Post-Marronvolcmics and sediments. Similar Tertiary age rocks host epitbermalprecious metal valuesat the well-known Dusty Mat and Vault propertieslocated near OkanaganFalls. A total of 93,653tonnes of ore with an averagegrade of 6.29 @tonne gold and 146.49g/tonne silver were mined from the Dusty Mat openpit mine during 1975- 76. One persistentcomposite epithermal vein on the Vault property has a reserve of 152,tKKl tonnesof 14 gltonnegold plus minor silver values. A large epithermaldeposit on the same property may contain an additional 1.3 million tonnesof 2 @tonnegold.
The main focus of explorationon the Vemrer MeadowsTertiary Oatlier over the yearshas beenthe AU prospect,located near Solco Creek, adjacentthe main loggingroad (R-200). Severalexploration companies including LacanaMining Corporation,Jnco Ltd. and Energex Mineral Ltd. worked on, or near, the AU prospectthrough the 1980’s. Thirty-one diamond drill holes totalling 3647 metres were drilled by various parties. Lacana’sdrilling returned gold valuesas high as 1.‘78ox/T over 2 metres,0.842 oz/T over 1 metre and 8.023 oz/T over w 2 b SUMMARY continued
0.50 metres from the Main Vein on the old AU prospect. The Main Vein is a compositevein of calcite, quartz and minor adulariawhich pinches(2 cm) and swells (2 m) over short distances.The gold values,although sometimes good, are very erratic.
All of the old explorationsites near the AU prospectare now covered .with the Golden Rainbow Claim Group.
The October 2002 drill holeswere designedto test brecciatedandesites of the Marron Formation which lie unconformablyover the MonasheeGroup gneissbasement. Two of the drill holes passedthrough the entire hangingwall sequenceof Marron volcanicsand a major fault zone (i.e. Fort Knox BasementFault) and on into the Monasheegneiss.
A late 60 metre thick rhyodacitesill was encounteredin the two deepdrill holes. The sill has ‘CI intmded the broken rocks of the BasementFault and it occupiesspace that, accordingto the original explorationmodel, was supposedto host preciousmetal deposits.
There is ampleevidence that late auriferousepithermal solutions have ascendedthe Basement Fault through highly disruptedrock along both the baseand the top of the rhyodacitesill.
Eighty-sevensamples of core with epithermalcalcite/quartz veins and/or silica replacement zonesand/or strong chlorite alterationwere submittedfor analyses. None of the samples returned “ore grade” intercepts,but 42 containedgeochemically significant gold and/or arsenic valuesand some containedelevated antimony, mercury, thallium and molybdenumvalues.
The geochemicalzoning indicatesa northeastsource for the epithermalsolutions. 3
SUMMARY continued
Although the rhyodacitesill is thought to predatethe auriferousepithemral solutions, it is believedthat both originatedfrom a common sourcewhich lies not far to the northeastof the Gold 1 mineral claim and a revisedexploration model has beenproposed for the property.
An experimentalsurvey of deeppenetration Induced Polarization (I.P.) is recommendedover portions of the Gold 1-14 mineral claims to outline the major componentsof the revised model basedon the variable conductivitiesof the rock units.
If the trial I.P. survey is effective, it has beenrecommended that it be expandedto investigate other areasof the 12 km long GoldenRainbow Claim Group. - 4-
I I 128” 120” cd. t ~.W- ,60’ --W.+, ~KON \ -.-.--. -.-.- :\ .-.------ALESERT~ BR=‘SH coL.,,M&A I
i l Fort Nelson . I
i
i
56” Fort St. John . i i i
52”
‘\ ‘\ GOLDEN RAINBOW CLAIM GROUP’ Dkanagan Falls Ame, Dsoyoos M.D., B.C. -‘L. l Kamloqx / \
PACIFIC OCEAN k. Penticton l m _._------49” ..__.-.. -..-- --. U.S.A.
DOUBLESTAR RESOURCES LTD GOLDEN RAINBOW CLAIM GROUP Okanagan Falls Area, Osoyoos M.D., B.C.
LOCATION MAP
OkIll 2OOkti mkm Drawn By: MM. N.T.S. 62-E-6W L’ I FIGURE 1 January, 2003 I
6
L INTRODUCTION
This report, written for governmentassessment work credits, discussesthe resultsof a four hole (613 metre) Diamond Drilling Programwhich was conductedon the Gold 1 mineral claim for DoublestarResources Ltd. under the direction of the writer during October, 2002.
The Gold 1 mineral claim is one of 14, 2-post mineral claims (Gold I-14) that were optioned by DoublestarResources Ltd. of West Vancouver,B.C. in September,2002. Doublestar financedthe drilling program as part of a commitmenttowards eaminga 100%interest in the mineral claims.
The Gold 1-14, 2-post mineral claims form just a part of a 12 km long parcelof land that is comprisedof 87,2-post mineral claims which cover the southwestside of the Venner Meadows Tertiary Outlier. The Outlier is situatedon a rolling portion of the Okanagan b Highland betweenShuttleworth and VaseuxCreeks, 14 to 22 km southeastof OkanaganFalls, B.C. The 87,2-post mineral claims belongto the Golden Rainbow Claim Group in which DoublestarResources Ltd. can eam a 100%interest subjectto conditionsand royalties.
All of the mineral claims comprisingthe Golden Rainbow Claim Group were stakedby the writer over a period of years(1990-1999). The mineral claims were stakedto cover altered and veinedEarly Eocenevolcanics and sedimentsthat were known to contain significant preciousmetal valueslocally. The Early Eocenerocks comprisingthe Venner Meadows Outlier were also recognizedas bemg very similar to those which host preciousmetals at the Dusty Mat and Vault propertieslocated near OkanaganFalls.
Prior to this year’sdrilling program, DoublestarResources Ltd. financedtwo percussion drilling programs(in 1995 and 1997)which totalled 1253metres. Most of the drilling was concentratedon the Fort mineral claims locatednear the centre of the Golden Rainbow Claim Group, but three drill holes were drilled on the Lucky Star mineral claims near the northwest w b INTRODUCTION cominued
end of the Claim Group. The October, 2002 drilling was conducted2.5 km from the southeastend of the Venner MeadowsOutlier.
The geologyacross the GoldenRainbow Claim Group is relatively uniform and it has been describedin severalprevious assessment reports by the writer (see References).The geology outlined in this report will be restricted to the Gold 1 mineral claim in the immediatearea of the October, 2002 drilling program.
Ground coveredby the Gold mineral claims, and the Gold 1 mineral claim, in particular, was exploredextensively by severalprevious operators(Teck CorporationLtd., Granby Mining CorporationInc., CanexPlacer Ltd., EnergexMinerals Ltd., LacanaMining Corporation,Rio Algom Exploration Inc., K. L. Daughtry and AssociatesLtd. and Tigris Minerals Corporation) u and in the 1980’s,a numberof diamonddrilling programswere conductedon, or near, the Gold 1 mineral claim. Somevery interestingdrill interceptswere encounteredand these included:D.D.H. 82-l from lO.OO-12.OOm,2.00 metres of 1.78 oz/ton gold; D.D.H. 83-9 from 52.15-52.65m,0.50 metres of 8.023 oz/ton gold; and D.D.H. 83-16 from 146.00- 147.OOm,1.00 metre of Ct.842oz/ton gold, (Peatfield,1989).
A new explorationmodel has beendeveloped for the Gold property sincethe 1980’sdrilling programs. The new model suggeststhat the major fault (i.e. Fort Knox BasementFault) which separatesthe Tertiary rocks of the VemrerMeadows Outlier from the MonasheeGroup gneiss“basement rocks!’ was the main conduit for the epithermalsolutions which have depositedgold within the Tertiary rocks on the Gold property.
The October, 2002 drilling program was designedto test the model and two of the four drill holes were drilled down to the Fort Knox BasementFault. All four drill holes were also drilled to test the down dip projectionsof brecciatedand altered andesiticrock units that on w surfacehad yielded gold valuesup to 5380 parts per billion. 8 k INTRODUCTION continued
All of the information gatheredduring the October, 2002 drilling program is presentedwithin this report with the support of Cross-SectionalDiagrams (Figures 7-lo), Drill Logs (Appendix C) and Laboratory Analyses(Appendix D).
The drill hole locations are illustratedon Map G-03-1.
LOCATION AND ACCESS
The Gold 1-14 mineral claims (referred to as the “property” on this page)are locatedat Solco (Fish) Creek, 20 km southeastof OkanaganFalls, B.C. (Lat. 49” 16’ 30”; Long. 119” 18’; N.T.S. Map 82-IX-6W). b Accessto the property from OkanaganFalls is via the WeyerhauserSawmill Road to the AllendaleLake Road which by-passesthe sawmill and then continuesbeyond the millsite as the OkanaganFalls Forest ServiceRoad. The road climbs the mountainon the south side of ShuttleworthCreek as the main haulageroad. A secondarylogging road branchesto the right at kilometre 12.3 and continuessoutheast another 13.7 km to the property. This road, which is generallymaintained year-round, runs through the centreof the property (seeFigure 3). Old explorationroads which branch from the main road (seeMap G-03-1) were rehabilitated for the October, 2002 drilling program. 4
Rainbow l-4 & 7-24 mi,, : Iclaims (22 units)
I 1 2 Yrn -49’17’
Please see Figures 4a & 4b
DOUBLESTAR RESI ii1JRCES LTD GOLDEN RAINBOW CLAIM GROUP Okanagan Falls Area, Osoyoos M.D., B.C.
II MINERAL CLAIMS AND ACCESS
I----.. AoxssAoads Drawn By: MM. N.T.S. 82-E-6W L’ / January, 2003 FIGURE 3 10 L PHYSICAL FEATURES AND CLIMATE
The Gold 1-14 mineral claims (referred to as the “Gold property” on this page)are situated on a rolling uplifted region known geographicallyas the OkanaganHighland. Elevationson the Highland generallyrange from 1400to 1800metres with someridges reaching 2100 metres. Mount Baldy, located 13 km southeastof the Gold property, is the highest point of land in the region at 2300 metres.
The OkanaganHighland is deeplyincised by Shuttleworthand VaseuxCreeks which dram into the OkanaganRiver at the 330 metre elevationjust 13 km west of the property.
The Gold property is located at Solco Creek and covers a portion of VennerMeadows (at 1370 metres elevation)and a roundedhill which rises to an elevationof 1600metres, 14 w kilometresnortheast of the meadows.
The gentle slopeson the property are mantledwith 1 to 5 metres of boulderand clay till. There were very few rock exposureson the property prior to the exploration,logging and road building activities of the 1980’sand 90’s.
Lodgepolepine and Douglas fir are the dominant forest species,and very little of the property has been logged. Where logging has beenconducted, new forests of 2 to 4 metre pine trees are growing vigorously.
The region is alsoused as a summerrangeland. SolcoCreek and its tributaries provide ample drinking water for the cattle. SolcoCreek was also used as a sourceof water for the October, 2002 drilling program. 11 w PHYSICAL FEATURES AND CLIMATE continued
The OkanaganHighland receivesconsiderably more precipitation than the arid Okanagan Valley. Annual precipitationon the Gold property equals60 cm - half of it in the form of snow. The snow beginsto accumulatearound the fust of November and generallylingers on shadedslopes until May.
Summertemperatures can reachas high as 30” C in the upland country, while winter minimums can drop to -30°C. 12 w CLAIM STATUS
The Gold 1-14, Fort Knox l-10, Fort l-25, Lucky Star 1-16 and Rainbow l-4 & 7-24, 2-post mineral claims, which comprisethe Golden Rainbow Claim Group, were all stakedby the writer, M. Morrison, of Kelowna, B.C. The mineral claims are recordedin the Osoyoos Mining Division and are on Mineral Title Maps 82EO23,024, 033 and 034.
Agreementssigned by the writer in 1996 and 2002 give DoublestarResources Ltd. the right to earn up to a 100%interest in the Golden Rainbow Claim Group subjectto work commitmentsand royalty payments.
DoublestarResources Ltd. is a public companybased in West Vancouver,B.C. The company’sshares trade on the TSX Venture Exchange. w The writer currently owns approximatelya 50% interest in the Claim Group.
The following table Liststhe mineral &ii comprisingthe Golden Rainbow Claim Group:
CLAIM TENURE RECORDED DATE OF EXPIRY* NAME UNITS NUMRER OWNER RECORD DATE Fort Knox 1 1 247342 M. S. Morrison Dec. 7, 1990 Dec. 7, 2004 Fort Knox 2 1 247343 M. S. Morrison Dec. 7, 1990 Dec. 7,2004 Fort Knox 3 1 247344 M. S. Morrison Dec. 7, 1990 Dec. 7,2004 Fort Knox 4 1 247345 M. S. Morrison Dec. 7, 1990 Dec. 7,2004 Fort Knox 5 1 247346 M. S. Morrison Dec. 7, 1990 Dec. 7,2004 Fort Knox 6 1 247347 M. S. Morrison Dec. 7, 1990 Dec. 7, 2004 Fort Knox 7 1 247348 M. S. Morrison Dec. 7, 1990 Dec. 7,2005 Fort Knox 8 1 247349 M. S. Morrison Dec. 7, 1990 Dec. 7,2005 Fort Knox 9 1 247350 M. S. Morrison Dec. 7, 1990 Dec. 7,2005 w Fort Knox 10 1 247351 M. S. Morrison Dec. 7, 1990 Dec. 7, 2006 13
‘u CLAIM TENURE RECORDED DATE OF EXPIRY* NAME UNITS NUMBER OWNER RECORD DATE Fort 1 1 306875 M. S. Morrison Dec. 1, 1991 Dec. 1,2007 Fort 2 1 306876 M. S. Morrison Dec. 1, 1991 Dec. 1,2007 Fort 3 1 306877 M. S. Morrison Dec. 1, 1991 Dec. 1, 2007 Fort 4 1 306878 M. S. Morrison Dec. 1, 1991 Dec. 1,2007 Fort 5 1 306879 M. S. Morrison Dec. 1, 1991 Dec. 1,2006 Fort 6 1 306880 M. S. Morrison Dec. 1, 1991 Dec. 1,2007 Fort 7 1 306881 M. S. Morrison Dec. 1, 1991 Dec. 1,2006 Fort 8 1 306882 M. S. Morrison Dec. 1, 1991 Dec. 1,2006 Fort 9 1 306883 M. S. Morrison Dec. 1, 1991 Dec. 1, 2004 Fort 10 1 323725 M. S. Morrison Feb. 5, 1994 Feb. 5, 2005 Fort 11 1 323726 M. S. Morrison Feb. 5, 1994 Feb. 5,2004 Fort 12 1 323727 M. S. Morrison Feb. 5, 1994 Feb. 5,2004 w Fort 13 1 323728 M. S. Morrison Feb. 5, 1994 Feb. 5,2004 Fort 14 1 323729 M. S. Morrison Feb. 5, 1994 Feb. 5,2004 Fort 1.5 1 323730 M. S. Morrison Feb. 5, 1994 Feb. 5,2004 Fort 16 1 327054 M. S. Morrison June 19, 1994 June 19,2004 Fort 17 1 327055 M. S. Morrison June 19, 1994 June 19,2004 Fort 18 1 327056 M. S. Morrison June 19, 1994 June 19,2004 Fort 19 1 327057 M. S. Morrison June 19,1994 June 19,2004 Fort 20 1 327058 M. S. Morrison June 19, 1994 June 19,2004 Fort 21 1 327059 M. S. Morrison June 19, 1994 kne 19,2004 Fort 22 1 360754 M. S. Morrison Nov. 13, 1997 Nov. 13,2004 Fort 23 1 360755 M. S. Morrison Nov. 13, 1997 Nov. 13,2004 Fort 24 1 360756 M. S. Morrison Nov. 13, 1997 Nov. 13,2004 Fort 25 1 3607’57 M. S. Morrison Nov. 13, 1997 Nh. 13,2004 14 w CLAIM STATUS (continued)
CLAIM TENURE RECORDED DATE OF EXPIRY” NAME UNITS NUMBER OWNER RECORD DATE Lucky star 1 1 327066 M. S. Morrison June 26, 1994 June 26,2004 Lucky star 2 1 327067 M. S. Morrison June 26, 1994 June 26,2004 Lucky star 3 1 327068 M. S. Morrison July 3, 1994 July 3, 2004 Lucky star 4 1 327069 M. S. Morrison July 3, 1994 July 3, 2004 Lucky star 5 1 327070 M. S. Morrison July 3, 1994 July 3, 2004 Lucky Star 6 1 32707 1 M. S. Morrison July 3, 1994 July 3, 2006 Lucky star 7 1 327072 M. S. Morrison July 3, 1994 July 3, 2004 Lucky Star 8 1 327073 M. S. Morrison July 3, 1994 July 3, 2004 Lucky star 9 1 360758 M. S. Morrison Nov. 14, 1997 Nov. 14,2004 Lucky star 10 1 360759 M. S. Morrison Nov. 14, 1997 Nov. 14,2004 Lucky star 11 1 360760 M. S. Morrison Nov. 14, 1997 Nov. 14,2004 w Lucky star 12 1 360761 M. S. Morrison Nov. 14, 1997 Nov. 14,2004 Lucky star 13 1 360762 M. S. Morrison Nov. 14, 1997 Nov. 14,2004 Lucky star 14 1 360763 M. S. Morrison Nov. 14, 1997 Nov. 14,2004 Lucky star 15 1 360764 M. S. Morrison Nov. 14, 1997 Nov. 14,2004 Lucky Star 16 1 360765 M. S. Morrison Nov. 14, 1997 Nov. 14,2004 Gold 1 1 368960 M. S. Morrison April 22, 1999 Oct. 25,2007 Gold 2 1 368961 M. S. Morrison April 22, 1999 Oct. 25,2007 Gold 3 1 368962 M. S. Morrison April 22, 1999 Oct. 25,2007 Gold 4 1 368963 M. S. Morrison April 22, 1999 Oct. 25,2007 Gold 5 1 370600 M. S. Morrison July 16, 1999 Oct. 25, 2007 Gold 6 1 370601 M. S. Morrison July 16, 1999 Oct. 25,2007 Gold 7 1 370602 M. S. Morrison July 16, 1999 Oct. 25,2007 Gold 8 1 370603 M. S. Morrison July 16, 1999 Oct. 25, 2007 Gold 9 1 372015 M. S. Morrison Sept. 28, 1999 Oct. 25,2007 ‘r Gold 10 1 372016 M. S. Morrison Sept. 28, 1999 Oct. 25,2007 15
CLAIM STATUS (continued)
CLAIM TENURE RECORDED DATE OF EXPIRY’ NAME UNITS NUMBER OWNER RECORD DATE Gold 11 1 372017 M. S. Morrison Sept.28, 1999 Oct. 25,2007 Gold 12 1 372018 M. S. Morrison Sept.28, 1999 ~Oct.25,2007 Gold 13 1 372019 M. S. Morrison Sept.28, 1999 Oct. 25,2007 Gold 14 1 372020 M. S. Morrison Sept 28, 1999 Oct. 25,2007 Rainbow 1 1 327074 M. S. Morrison Jane 26, 1994 June26,2003 Rainbow 2 1 327075 M. S. Morrison June 26, 1994 Jane26,2003 Rainbow 3 1 327076 M. S. Morrison Jane 26, 1994 June26,2003 Rainbow 4 1 327077 M. S. Morrison Jane26,1994 June26,2003 Rainbow I 1 362887 M. S. Morrison May 18, 1998 May 18,2004 Rainbow 8 1 362888 M. S. Morrison May 18, 1998 May 18,2004 Rainbow 9 1 362889 M. S. Morrison May 18, 1998 May 18,2003 Rainbow 10 1 362890 M. S. Morrison May 18, 1998 May 18,2003 Rainbow 11 1 370604 M. S. Morrison July 18, 1999 July 18,2003 Rainbow 12 1 370605 M. S. Morrison July 18, 1999 July 18, 2003 Rainbow 13 1 370606 M. S. Morrison July 18, 1999 July 18, 2003 Rainbow 14 1 370607 M. S. Morrison July 18, 1999 July 18,2003 Rainbow 1.5 1 370608 M. S. Morrison July 18, 1999 July’l8, 2003 Rainbow 16 1 370609 M. S. Morrison July 18, 1999 July 18,2003 Rainbow 17 1 372483 M. S. Morrison Sept.30, 1999 Sept.30,2003 Rainbow 18 1 372484 M. S. Morrison Sept.30, 1999 Sept.30, 2003 Rainbow 19 1 372485 M. S. Morrison Oct. 3, 1999 Oct. 3, 2003 Rainbow 20 1 372486 M. S. Morrison Oct. 3, 1999 Oct. 3, 2003 Rainbow 21 1 372487 M. S. Morrison Oct. 4, 1999 Oct. 4, 2003 Rainbow 22 1 372488 M. S. Morrison Oct. 4, 1999 Oct. 4, 2005 Rainbow 23 1 372489 M. S. Morrison Oct. 4, 1999 Oct. 4, 2005 Rainbow 24 1 372490 M. S. Morrison Oct. 4, 1999 Oct. 4, 2005 16
CLAM STATUS (continued)
* (The Expiry Dates are basedon the acceptanceof this report for assessmentwork credits.)
It shouldbe noted that there is considerableoverlap of someof the mineral claims. Although the mineral claims have not been surveyed,an estimateof the degreeof overlap is illustrated on Figures4a & b accompanyingthis report.
The earlier stakedmineral claims have priority over later stakedmineral claims. The Dates of Recordlisted aboveindicate the chronologicalorder in which the mineral claims were recorded.
t
19
HISTORY
The Tertiary Age rocks of the OkanaganFalls areawere not seriouslyexplored for precious metal depositsuntil the late 1960’swhen Noranda Mines Ltd. discoveredsilver and gold mineralizationwithin a silicitied outcrop of Tertiary rock 14 km northeastof OkanaganFalls on the Dusty Mat property.
Extensivedrilling by Norandaproved that the depositwas too small consideringthe low metal prices of the day and the property was returnedto the vendor, Dusty Mat Mines Ltd., in 1970. Shortly thereafter,precious metal pricesincreased dramatically and Dusty Mat extractedthe depositwith a profitable open pit operationduring 1975-76. In all, 93,653 tonnesor ore grading6.29 g/tonnegold and 146.59g/tonne silver were mined.
The principalsassociated with Dusty Mat Mines Ltd. alsodiscovered gold mineralisation within Tertiary Age rocks 20 lan southeastof OkanagauFalls, near Solcocreek, in the early 1970’s. The AU property was stakedand optionedto Teck CorporationLtd. which conducted preliminary explorationprograms on the ground. The Gold 1-14 mineral chumscover the old AU property.
In 1982,the writer discovereda large silicified zone within Tertiary rocks 4 km northwest of OkanaganFalls and stakedthe Vault property. The Vault property was exploredaggressively by RiocanexInc. (1982-g3),Dome ExplorationLtd. (1984), Sevenmile High ResourceInc. (1985) and Into Ltd. (1986-1990). Expendituresexceeding 43 million dollars went into exploration on the property in an effort to establisha preciousmetal reserve.
The North Vein on the Vault property was drilled extensivelyto a depth of 200 metres and reservesof 152,000tonnes with 14 g/tonnegold and minor silver valueswere calculated. A large epithermalsystem (Central Zone) which lies 400 metres south of the North Vein was 20 w HISTORY continued
also drilled extensivelyand gradesas high as 15 g/tonneover 8.8 metres and 10.0 g/tonne over 13.4 metres were reported. However, the geologywas found to be complexand an ore reservecalculation was never announced.It is expectedthat the Central Zone could contain 1.3 million tons of 2 glto.unegold.
In the 1980’s,the old AU prospectwas simultaneouslyrestaked by two parties. Lacana Mining Corporationstaked claims which coveredthe Main Vein eastof logging road R-200, while EnergexMinerals Ltd. and K. L. Doughtry and Associatesstaked ground to the west, south and southeastof the Lacanaground.
During two drilling programs(1982 & 83) Lacanadrilled 20 diamonddrill holes totalling 2153 metres with most of the holes directedtowards the Main Vein. Tigris Minerals Corporationoptioned the Lacanaground in 1988 and in two programs(1988 & 89) drilled an additional942 metres to investigatethe Main Vein. Gold valuesas high as 1.78 ox/T over 2 metres,0.842 oz./T over 1 metre and 8.023 oz/T over 0.50 metres were interceptedduring the drilling programs,but the Main Vein was found to pinch and swell over short distancesand the gold distribution within the vein was found to be very erratic. Assessmentwork was recordedfor ten yearsiu advance. LacanaCorporation was taken over by Corona Corporationand they, in turn, by HomestakeCanada Ltd. Homestakelost interest in the area, and in March 1999 all of the original Lacanaground had lapsed.
The Energex,et al, ground had a history parallel to the Lacanaground. In the early 1980’s, Energexdrilled three diamonddrill holes totalling 457 metresto investigatevarious targets on the property. In 1988, Into Ltd. optionedthe ground and drilled an additionaleight holes totalling 1637 metres. Someof the drilling was designedto find the westernextension of the LacanaMain Vein and someof the drilling was conductedto test parallel structures. The best valuesobtained were from Drill Hole 72474 from 42.78-43.32m, 0.54 m of 15.5 @tonne w 21 b HISTORY continued
gold and from Drill Hole 72478 from 109.90-110.12,0.22metres of 13.6 gltonnegold (Morin, 1989). The drilling was filed as assessmentwork for ten yearsin advance.
The writer stakedthe GoIld l-4 mineral claims in April, 1999after the original Lacanaground lapsedand the Gold 5-8 (in July, 1999)and the Gold 9-14 (m September,1999) after Energex,et al, allowed their mineral claims to lapse.
In 2000, the writer mappedthe geology on the Gold 1 and adjacentportions of the Gold 2, 8, 9 & 10 mineral claims at a scaleof 1: 2500. In 2001, three surfacesamples were collected from rock on the Gold 1 mineral claim, one of which returneda value of 5380 parts per billion gold. 22 w REGIONAL GEOLOGY AND MJNERALIZATION
Figure 5 accompanyingthis report outlinesthe regionalgeology of the OkanaganFalls area. The geologyhas beenreproduced from G.S.C. Map 15-1961by H. W. Little with some modifications.
The oldest rock illustratedon Figure 5 is a Pre-Pewan Monasheegneiss. It underliesmuch of the country for 16 kilometreseast and southeastof OkanaganFalls. The gneisshas been intruded by the Cretaceous(?) Nelson Intrusivesnortheast of OkanaganFalls. The Nelson Intrusives also occur at three sites on the easternside of the map area. Later Cretaceous(?) ValhallaPlutonics intrude both the MonasheeGroup and Nelson Intrusives and underliemuch of the easternhalf of the map area.
Tertiary Age sedimentsand volcanicsrest unconformablyover all earlier rock formations and
‘u occur within fault-boundedbasins at OkanaganFalls and at VemrerMeadows, 20 kilometres to the southeast,as illustratedon Figure 5. The Tertiary rocks have been folded and cut by late faulting.
It is believedthat preciousmetal bearingepithermal solutions have ascendedlate fault structureswithin the Tertiary rocks, and that at somemineral prospectsrepeated faulting and the introduction of severalphases of epithermalsolutions have upgradedthe preciousmetal content of the Tertiary rocks to ore gradevalues. Important.precious metal depositsin the district are illustratedon Figure 5. They include the Vault, Dusty Mat and AU occurrences which have all beenreviewed underthe previoustitle “History”.
The Gold 1-14 mineral claims cover the old AU prospectand a 2 km segmentof the Venner MeadowsTertiary Outlier lying 4 km from the southeastend.
24
L PROPERTY GEOLOGE
AU Proswct - Lacana Main Vein
The Main Vein of the original AU prospectoccurs near the 26 km signposton the main loggingroad (R-200) which crossesthrough the Gold mineral claims. The vein is a banded and brecciatedcomposite calcite/quartz vein that is up to 1 metre wide at the road cut. The vein was locatednear the north-southboundary of the old Lacana/Energexproperties (see History) and it is presentlylocated near the boundarybetween the Gold 1 & 2 mineral claims (seemap G-03-1). Most of the 1980’sexploration and drilling programswere conductedin the immediatevicinity of the original AU prospect.
In 2000, the writer mappedthe property near the old AU prospectand studiedall of the availableoutcrop in the vicinity. The mappingat a scaleof 1: 2500 coveredthe Gold 1 w mineral claim and portions of the Gold 2, 8, 9 & 10 mineral claims adjacentto it. The geologymap (Map G-01-1) was submittedto the governmentwith an AssessmentReport written early in 2001.
MaDDing Propram - 2000
The mappingprogram in 2000 was hamperedby a generalcover of till on much of the property and a thick layer of tuff which covers much of the Gold 3 & 4 mineral claims. The volcanic flow rocks that were mappedare all very interestingin that most are highly brecciatedand stainedwith limonite or hematite. The andesiticrocks are alsocut by veinlets and veins that are bandedand multiphaseand which look very much like the vein at the original AU prospect. Three grab samplestaken from the brecciatedandesites in 2001 yielded valuesof 430,440and 5380 parts per billion gold. Samplescollected by later visitors to the property yielded gold valuesranging up to 1820ppb. 25 w PROPERTY GEOLOGY_ continued
Summary of the Gold 1 Mineral Claim Geology
There are at least three dominantporphyritic andesitesthat belongto the Early Eocene Marron Formationin the vicinity of the Gold 1 mineral claim. Type 1 andesite,referred to in this report, is a porphyritic plagioclaseandesite; Type 2 is a porphyritic plagioclase/augite andesite;and Type 3 is a porphyritic augite andesite. There are also severalother minor porphyritic andesites.
The andesitesare, for the most part, very brecciatedand they rest as hangingwall rocks over the Fort Knox BasementFault. Pre-PermianMonashee Group gneissunderlies the Basement Fault. w The andesitesare coveredby rhyodacitetnff to the northeast.
A large (60 metre thick) rhyodacitesill which has ascendedthe BasementFault from the northeastis probably an offshoot from the volcanothat producedthe rhyodaciteash (tuff) which overliesmuch of the Venner Meadows Tertiary Outlier.
Late auriferousepithermal solutions have also ascendedthe BasementFault from the northeast,and they are believedto be responsiblefor the epithermalveins on the Gold 1 & 2 mineral claims.
ExDloration Model for the Venner Meadow Tertiary Outlier
An explorationmodel for the Gold mineral claims was developedby the writer basedon the 2000 mappingprogram, and data obtainedfrom mappingconducted elsewhere on the Vemrer MeadowsTertiary Outlier. w 26
PROPERTY GEOLOGY_ continued
Exuloration Model for the Venner Meadow Tertiary Outlier continued
The model recognizesthat a major fault (Fort Knox BasementFault) underliesthe southwest side of the Outlier and separatesthe Tertiary rocks of the Outlier from the Pre-Tertiary basementrocks. The model suggeststhat the BasementFault was the conduit for auriferous epithermal solutionsthat have ascendedfrom the northeastand have penetratedthe most permeablerocks of the Tertiary sequence.
The highly brecciatedandesites of the Early EoceneMarron Formation,which underliethe Gold 1 mineral claim, form the hangingwall of the BasementFault. The rocks of the hangingwall are particularly permeableand there is ample evidenceof the passageof epithermalsolutions through theserocks. The Main Vein drilled extensivelyby Lacanais a composite,vein of calcite and quartz that was clearly formed by episodalinjections of epithermal solutions. Severalsmaller compositeveins on the Gold 1 mineral claim indicate the samehistory.
The BasementFault was thought to dip 45 degreesto the northeastprior to the October, 2002 drilling program. Such a dip would have brought the fault nearersurface on the southwest comer of the Gold 1 mineral claim, and it was believedthat an economicgold depositmight be found near surface.
In actual fact, the BasementFault dips 25 degreesto the northeastand it lies 150 to 200 metres below surfaceon the southwestcomer of the Gold 1 mineral claim. 21 PROPERTY GEOLOGY_ continued
Promrty Geolo~v Basedon the 2002 Drillhe Results
After studying the core of the four drill holes drilled during the October, 2002 program, the geologycould be describedas a “mess”. Almost ah of the rock is brecciated. It appearsthat much of the rock originatedas talus comprisedof a mix of porphyritic andesitesthat eroded from nearby cliffs. The cliffs were apparentlycomprised of three dominant audesites,Types 1, 2 & 3, which are describedin the drill logs. Over the centuries,the talus blocks which rangefrom 5 to 50 cm have beenshuffled and pressedtightly togetherto the extent that there is very little interstitial space(there was apparentlyvery few fine rock clasts within the original talus). Early micro veinlets of calcite/quartzwhich filed the narrow spacesthat were availableare now highly disruptedand these veinlets suggestthat the rock has been subjected to continuedpressures and movement.
Late tectonic brecciazones of a few centimetresto metres are recordedthroughout the drill logs and attest to the fact that the rock has undergonecontinued disturbance. The clastsof the tectonic breccia zonesmeasure from 0.1 to 2 cm. In somecases, the smallbreccia zones are mendedwith calcite/quartzveinlets or silica, but most often they are not. There could be severalstages of tectonic brecciationrecorded in the drill core, and this is not unexpected consideringthat the rocks form the hangingwall of a major fault.
The introductionof the multiphasebanded calcite/quartz veins into the andesiticbreccias is consideredto be a late event. Most of the veins exhibit little disruption comparedto the micro veinlets mentionedearlier. Someof the late veins are brecciatedor offset small distances,however, indicatingat least somelate movementof the rocks.
There are, most probably, severalages of veins. Somehave calcite cores,some have clear quartz cores and a few have pyrite coresor selvages. The pyrite is late and most of the better 28 v PROPERTY GEOLOGY_ continued
Prowxtv Geology Based on the 2002 Drilling Results continued
gold, arsenic,antimony and molybdenumvalues recorded from the drilling program occur with veins that containpyrite or with veins that have pyrite haloes.
Many of the late bandedcalcite/quartz veins dip very steeply,or steeplyto the northeast, while someappear to parallelthe dip of the rock units and dip moderatelynortheast.
A very thick (60 metres in D.D.H.‘s G-01 & G-03) porphyritic rhyodacitesill has intruded the large clast brecciasdirectly abovethe Fort Knox BasementFault. The sill fills in a position which, accordingto the explorationmodel, was supposedto be the ore zone. (i.e. The rock immediatelyabove the BasementFault was expectedto be a highly brecciatedandesite v mendedwith a stockwork of auriferouscalcite/quartz veins and silica.)
Although the sill is very siliceousand brittle, it is much lessbrecciated and veinedthan either the overlying andesiteor the underlying Monasheegneiss, and it is obviously a late geologicalfeature.
The rhyodacitesill appearsto have the samecomposition as a rhyodacitetuff that covers much of the Vemrer MeadowsOutlier, and it could representan offshoot of the main volcanic event that generatedthe rhyodaciteash (tuff).
The strong effects of the Fort Knox BasementFault are seenin the andesitesabove the rhyodacitesill and in the Monasheegneiss below the sill. The gneissis disruptedand replacedwith 20-60% chlorite and 10-40%quartz over a vertical distanceof 15 to 20 metres in D.D.H.‘s G-01 & G-03. 29
PROPERTY GEOLOGY
Prowrty Geolow Based on the 2002 Drilling Results continued
Evidence,based on the.drill logs and samples,suggests that epithermalsolutions have originatedfrom the northeastand travelled upwardsto the southwestthrough strongly faulted rock lying aboveand below the rhyodacitesill. The solutionsthat ascendedthe Fort Knox BasementFault, along the top of the sill, have penetratedlate tectonicbreccia zonesand fractures within the andesitetalus, abovethe fault, resulting in the veins seenon surfaceor in drill core. The veins, which dip steeplyto moderatelyto the northeast,provide more evidencethat the sourceof the solutionslies to the northeast(see CrossSections on Figures 7-10). 30
DRTLLING PROGRAM - 2002
Site Preparation
The SolcoCreek logging road, which branchessouth from the main loggingroad (R-200) near the 26 km signpost,cuts through the centreof the Gold 1 mineral claim and provides good accessto the area coveredby the October drilling program. A network of old explorationroads branch to the west of the SolcoCreek road and coverthe northwest comer of the Gold 1 mineral claim and portions of the adjacentmineml claims. All four of the October diamonddrill holes were drilled from three sites on the northwest comer of the Gold 1 mineral claim.
The old explorationroads were coveredwith lodgepolepine deadfall,and had to be cleared with a chainsaw. A total of 1100metres of old roadswere clearedto provide direct routes and alternateroutes to the drill sites and the main water supplyat SolcoCreek.
Once the roadswere rehabilitated,a Case 580SK Turbo 4x4 Tractor equippedwith a front- end scoop and a backhoewas contractedfrom A & R Excavatingof Penticton,B.C. for site preparation. The preparationwork includedthe levelling of somesites and the digging of 2x3 metre sumpsto a depth of 2 metres at each site for the containmentof drill water run-off and sludge.
A total of 8 hourstractor time was chargedwhich includedmobilization and demobilization from Penticton.
The writer spent 2 days with a chainsawopening the old explorationroads through the deep piled deadfall and one day supervisingthe tractor operations. 31
DRILLING PROGRAM - 2002 continued
Reclamation
At the completion of the drilling program, the drilling contractorfilled in the sumpsand gradedthe drill sites with a SOG John Deere Dozer. Grassseed and 13-16-10fertilizer were appliedto the drill sites and to areasof soil disturbanceon the accessroads just prior to the winter snows.
The Drill
A Longyear38 drill momted on skids was contractedfrom BeaupreDiamond Drilliig Ltd. of Princeton,B.C. The drill had the capacityto easily drill BQ wireline holesto the depths requiredby the contract.
The drill, John DeereDozer Tractor and equipmentwere deliveredto the property on a low- bed truck. Once on the property, the tractor was usedto skid the drill and drill shackto each drill site.
A one-ton,4x4, pick-up with a large dieseltank accompaniedthe drill to each drill site. 32
DRILLING PROGRAM - 2002 continued
The Program
The drilling program was carried out from October 8-23, 2002. The drilling crew commuted from Princetoneach day and approximately8 hours of drilling were conductedeach shift.
A total of 613 metres were drilled in four holes, which rangedfrom depthsof 84.43to 222.59 metres. Two holes were drilled from a single site, a third hole was drilled 130 metres to the northwest and the fourth hole was drilled 180 metres to the northeast(see map G-03-01). Water was pumpedto the drill sites from Solco Creek and the pump was left running all night to prevent waterlinesfrom freezing.
The key objectiveof the program was to test the preciousmetal content of the brecciated w andesitesof the Early EoceneMarron Formation which form the hangingwall of the Fort Knox BasementFault.
The specificsof eachdrill hole are listed in the Table below:
DRILL HOLE COORDINATES AZIMUTH DIP ELEVATION CASING LENGTH NUMBER NORTH SOUTHEAST _ ___ metres) (metres) (metred G-01 10+39 2+00 225” -70 1429 7.32 215.49 G-02 10+22.5 3+33 125” -65” 1437 5.49 90.53 G-03 10+21 3+30 225” -60 1437 6.71 222.59 G-04 12+10 3+00 225” -70 1450 4.27 84.43 Totals 23.79 613.04
A stmrmarydescription of each drill hole is given under a later title iu this report. Drill logs for eachhole may be found in AppendixC. Cross Sectionsof eachdrill hole have alsobeen L drafted (see Figures7-10). 33
DRILLING PROGRAM - 2002 continued
Sampling
Sampleintervals were determinedwhile logging the drill core and sampleintercepts ranged from 0.08 to 3.81 metres. The sampleswere selectedfor analysisbased on the type and intensity of veining or on.the degreeof alteration. Bandedquartz/calcite veins were sampled singly or as compositesamples including wall rock. Silica replacementzones and alteration zoneswith hematiteblebs or pyrite were generallysampled. Although pyrite is rare on the property, pyrite was given specialconsideration among the samplesselected.
The results obtainedfrom the first shipmentof samplesfrom drill holes G-02, G-04 and the upper portionsof G-01 were used as a guide for selectingfewer samplesfrom drill hole G-03 and the lower portionsof G-01.
Someof the core not submittedfor samplingmay contain geochemicallysignificant values, but it is doubtful that it containseconomically significant values.
The core was split with a standardscrew and wedge core splitter. Each samplewas placedin a standardpoly rock samplebag with an identificationtag and shippedvia Greyhound Expressto Acme Analytical Laboratoriesin Vancouver,B.C. In all, 87 samplesweighing a total of 173 kg were sent in three separateshipments.
At the laboratory,the sampleswere crushedto -10 mesh and then a split of 250 g was pulverizedto -150 mesh,a 10 g split of the pulverizedsample was then leachedand analyzed for 35 elementsby ICP-MS.
The 10 g split for leachingwas considerednecessary for more reliable gold analyses.
The analyticalresults, along with the laboratoryprocedures are listed in Appendix D. 34
L DRILLING PROGRAM- continued
SamrGug continued
The drill core is presently storedat the writer’s residence,but it will be returnedto the property and storedwith the old Lacanacore on the Gold 1 mineral claim.
Summan Descriptions of Diamond Drill Holes G-01 to G-04 D.D.H. G-01
Diamond Drill Hole G-01 is located at grid 10+39N,2+OOSE. The hole was drilled to the southwest(225”) at an angle of minus 70 degreesto interceptnortheasterly dipping brecciated andesiteswhich outcrop on a bluff to the southwest. Two surfacesamples that were collected from a small knoll near the top of the bluff yielded 193 and 208 ppb gold.
The drill hole was drilled to a depth of 215.49 metres and it was designedto test all of the andesiticrocks which lie unconformablyover the Fort Knox BasementFault. It was believed that the brecciatedandesites might be well mineralizedwith gold near the fault considering the elevatedvalues that were obtainedfrom the surfacesamples.
The drill hole penetrated142.80 metres of large clast talus breccia of andesiticcomposition before encounteringa porphyritic rhyodacitesill. The sill was penetratedfor an additional 60 metresto 202.55 metres. The MonasheeGneiss was then drilled to the end of the drill hole at 215.49metres. Highly faulted rocks (i.e. Fort Knox BasementFault) were interceptedfrom 201.15 metresto the end of the drill hole.
The large clast talus brecciaencountered in the top half of the drill hole was comprisedof Type 1,2 & 3 porphyritic andesiteclasts with intervals wherethe predominantclasts were 35 t DRILLING PROGRAM - 2002 continued
Summm DescriDtions of Diamond Drill Holes G-01 to G-04 continued D.D.H. G-01 continued
Type 1, or Tyne 2 or Type 3. A thick sequenceof augite andesiteflow rock was encountered from 45.17 to 72.78 metres within the talus brecciasand a hematitic, very fine-grained amygdaloidalandesite was interceptedat the baseof the talus breccia from 137.80to 140.72 metres.
The talus brecciasare cut by severalzones of late tectonic brecciaover intervals rangingfrom a few centimetresto a few metres throughout. The breccia zonesare noted in the drill log (Appendix C), but they are too numerousto plot on the Cross Section(Figure 7).
‘CI, Chlorite/calcitealteration of the andesitesis common and is most intensewhere the rock has been well fractured in the late breccia zones.
Becauseof all of the brecciation,contacts between the units comprising the volcanic sequence are difficult to measure,‘but the rocks near the top of the drill hole appearto dip 40” to the northeast,while those lower down dip 35”. The rhyodacitesill appearsto dip 30” to the northeastand the BasementFault appearsto dip 25” to the northeast. Moderately steep,late shearzones cut the volcanic rocks and there is no doubt displacement(slumping and rotation) of the rock units occurs acrossthe shearzones.
Small bandedcalcite/quartz veins are common within the large clast breccias. Someare vertical, or near vertical, and othersseem to parallelthe northeastdip of the rock units. The veins are generally0.5 - 2 cm in thickness,but a 20 cm compositecalcite/quartz vein was interceptednear the top of the drill hole at 13.95metres. Very few late calcite/quartzveins occur within the rhyodacitesill. u 36 L DRlLLING PROGRAM - 2002 continued
Summarv Descriptions of Diamond Drill Holes G-01 to G-04 continued D.D.H. G-01 continued
Twenty-nine sampleswere selectedfrom various portions of the drill core for analysesand most of the results were poor. The 20 cm compositevein yielded 190 ppb gold, but no other elementsof note. Samplescollected from below the vein from 14.45to 22.22 metres containedlow gold values(13.4 - 23.4 ppb) and minor arsenicvalues (42.7 - 114.4 ppm). Three samples(58307, 58309 & 58311) selectedfrom core lower down the hole (between 49.56 and 81.55 metres) containedhigh arsenicvalues (242 - 709 ppm), but low gold values (2.7 - 76.9 ppb). Thesesamples included small calcite/quartzveins and/or minor silica replacementzones. u Samplescollected from the rhyodacitesill yielded low valuesas did one samplecollected from the quartz/chloritereplaced Monashee gneiss.
The thick rhyodacitesill was unexpectedand it occupiedthe intensefracture zone above the BasementFault wherethe potentialfor locating an economicprecious metal depositwas consideredto be the greatest.
D.D.H. G-02
Diamond Drill Hole G-O%was drilled from the samesite as D.D.H. G-03 at grid 10+22.5N, 3+33SE. The hole was drilled to the southeast(125”) acrossthe strike of the generalgeology at an angleof minus 65 degreesin an attempt to examinea 1 m wide quartz vein which outcrops at lO+lON, 3+56SEand which aligns with a breccia zone on surfaceat 10+5ON, 3+50SE. Surfacesamples collected from the brecciazone yielded 185 to 256 ppb gold. 31 w DRILLING PROGRAM - 2002 continued
Summan Descrktions of Diamond Drill Holes G-01 to G-04 continued D.D.H. G-02 continued
The drill hole was drilled to a depth of 90.53 metres through brecciatedandesitic rocks, but the quartzvein was not discoveredat depth.
The drill hole encounteredthe samebrecciated andesites that were penetratedin D.D.H. G-01 (and later in D.D.H. G-03). The large clast talus brecciaswere comprisedof a mix of andesiticclasts which includedType 1, Type 2, Type 3 and other minor varieties. Certain clasts were common over various intervals and the drill log indicateswhich clasts were the most predominant,Type 1 or Type 2 or Type 3. w Like elsewhereon the property, the large clast talus brecciashave been cut by numerous zonesof late tectonicbreccia over intervals rangingfrom a few centimetresto a few metres. One particularly strong shearzone, which may be vertical, occurs from 61.52 to 68.57 metres. The lesserbreccia zonesare two numerousto illustrate on the Cross Section(Figure 8), but they are noted in the drill log (Appendix C).
Chlorite/calcitealteration of the andesitesis common and is most intensewhere the rock has been well fractured in the late breccia zones. The shearzone mentionedabove is very chloritic.
Bandedcalcite/quartz veins are commonin the upperhalf of the drill hole. They are believed to dip steeplynortheast. Most of the veins rangefrom 0.5 - 2 cm, but one vein of 8 cm and anotherof 10 cm were intercepted.
Sixteensamples were selectedfrom various portions of the drill core for analysesof which 14 w containedsignificant gold (29.6 - 889.9 ppb) and/or arsenic(61.6 - 1034.1ppm) values 38 DRILLING PROGRAM - 2002 continued
Smnmarv Descriptions of Diamond Drill Holes G-01 to G-04 continued D.D.H. G-02 continued
(pleasesee the Table on Figure 8). Other elementswith elevatedvalues included antimony (up to 84.7 ppm) molybdenm (up to 343.1 ppm) mercury (up to 0.11 ppm) and thallium (up to 20.5 ppm).
The best valueswere recordedfrom a 4 cm bandedquartz vein near the top of the drill hole at 10.00metres (seeTable). Other very good valuesof key elementswere recordedfrom a strong silica replacementzone from 26.52 to 27.46 metres. Five samplesfrom 8.22 metres (i.e. 18.30 - 26.52 m) abovethe silica replacementzone and five samplesfrom 10.94 metres (i.e. 27.46 - 38.40 m) below the silica replacementzone alsoreturned elevatedvalues for v many of the key elements(see Table on Figure 8).
40
DRULING PROGRAM - 2002 continued
Summary DescriDtions of Diamond Drill Holes G-01 to G-04 continued D.D.H. G-03
Diamond Drill Hole G-03 is located 133 metres to the southwestof D.D.H. G-01 at grid 10+21N, 3+3OE. The hole was drilled to the southwest(225”) at an angle of minus 60 degreesto interceptthe samesequence of rocks that were drilled in D.D.H. G-01. Surface rocks to the southwestof the drill hole are alteredand hematitestained brecciated andesites which dip moderatelyto the northeast. The drill hole was designedto test the down-dip projection of thesewell altered rocks.
The hole was drilled to a depth of 222.59 metres to test all of the brecciatedandesitic rocks which lie unconformablyover the Fort Knox BasementFault.
In general,the drill hole encounteredthe samesequence of brecciatedandesites that were penetratedin D.D.H. G-01. The drill passedthrough 139.72metres of large clast talus breccia, 62 metres of rhyodacitesill (to 202.37metres) and 20 metres of Monasheegneiss (to the bottom of the hole at 222.59 metres). The Fort Knox BasementFault extendsfrom 202.37 metresto the bottom of the drill hole and it involves andesiticrocks sandwiched betweenthe sill and the gneissand the gneissitself to the bottom of the drill hole.
The large clast talus brecciasencountered in the top two-thuds of the drill hole were compriseda mix of andesiticclasts which includedType 1, Type 2, Type 3 and other minor varieties. As the drill log indicates,some of the rock was comprisedpredominantly of Type 1, or Type 2 or Type 3 andesiteclasts.
Like elsewhereon the property, the large clast talus brecciasare cut by mrmerouszones of late tectonic brecciaover intervals rangingfrom a few centimetresto a few metres. The 41
‘cl, DRILLING PROGRAM - 2002 continued
Summary Descriptions of Diamond Drill Holes G-01 to G-04 continued D.D.H. G-03 continued
zonesare not illustratedon the Cross Section(Figure 9), but they are noted in the drill log (Appendix C).
Chlorite/calcitealteration of the andesitesis common and is most intensewhere the rock has beenfractured in the late breccia zones.
Contactsbetween the rock mrits comprising the volcanic sequenceare difficult to measure becauseof all of the late brecciation,but shearplanes, which may coincidewith contacts,dip 45 to 50” to the northeast. The rhyodacitesill appearsto dip 30” to the northeastand the v BasementFault appearsto dip 25” to the northeast.
Small bandedcalcite/quartz veins are common within the large clast breccias. Someare vertical or dip steeplyto the northeast,others dip moderatelyto the northeastand may parallelthe dip of the rock units. The veins are generally0.5 - 2 cm in thickness. The thickest vein is 9.5 cm near the top of the drill hole at 9.40 metres. Very few late calcite/quartzveins occur within the rhyodacitesill.
Twenty-onesamples were selectedfrom various portionsof the drill core for analysesof which elevencontained significant gold and/or arsenicvalues. Six samplesbetween 28.10 and 126.57metres within the large clast andesiticbreccias contained elevated gold (32.7 - 170.6ppb), arsenic(232.9 - 1651.4ppm), antimony, molybdenumand thallium values(see Tableon Figure 9).
A strong silica replacementzone from 122.50to 126.57metres yielded the highest arsenic ‘r value and someof the higher gold values. 42 L DRILLING PROGRAM - 2002 continued
Summaw Descriptions of Diamond Drill Holes G-01 to G-04 continued D.D.B.G-03 continued
Three of the elevensignificant sampleswere collectedfrom highly disruptedrock (Basement Fault) immediatelybelow the rhyodacitesill from 202.37to 210.00metres. Thesesamples containedelevated arsenic (381.3 - 917.3 ppm) as well as elevatedantimony, mercury and thallium values(see Tableon Figure 9).
Samplescollected from the rhyodacitesill yielded low values. Two samplescollected from highly disrupted,chlorite and quartz replacedMonashee gneiss, within the fault zone, also yielded low valuesfor most elements. w Just as was the casein D.D.H. G-01, the thick rhyodacitesill occupiedthe intensefracture zone abovethe BasementFault where the potential for locating an economicprecious metal depositwas consideredto be the greatest.
D.D.H. G-04
Diamond Drill Hole G-04 is locatedat grid 12+1ON,3+OOSE. The hole was drilled to the southwest(225”) at an angle of minus 70 degreesto interceptnortheasterly dipping, brecciated andesites.Surface samples collected from the andesitesat grid 11+45N, 3+80SEyielded gold valuesranging from 1820to 5380 ppb.
The drill hole was drilled to a depth of 84.47 metres and penetratedlarge clast talus breccia over its entire length. The brecciawas comprisedof Type 1 porphyritic plagioclaseandesite predominantly. Severalzones of late tectonic breccia cut the large clast talus breccia over intervals of a few centimetresto a few metres from the top of the hole to the bottom. These k late brecciazones are noted in the drill log, but they are too numerousto illustrate on the Cross Section(Figure 10). 43
DRILLING PROGRAM - 2002 continued
Summary Descrbtions of Diamond Drill Holes G-01 to G-04 continued D.D.H. G-04 continued
Chlorite and calcite alterationof the andesiteis common, but it is most intensewithin the fmer late brecciazones. Small bandedcalcite/quartz veins from 1 - 14 cm thick are also common, but not all carry economicminerals.
Twenty-one sampleswere selectedfrom the core for analyses. Only sevenof the samples returnedvalues of significance,and only three of the sevencontained significant gold (187 - 408 ppb) or arsenic(62 - 129 ppm). The arsenicvalues are low comparedto the gold values, and this may indicatethat the sourceof the epithermal solutionswas nearby. The three sampleswhich yieldedthe higher valuesall containedbanded quartz/calcite veins ranging from 1 - 10 cm. The thickest vein (14 cm) at 24.18 metres returnednegligible gold values.
Although pyrite is rare, there is a close associationof pyrite with the bandedcalcite/quartz veins and it is most abundant(0.25 - 1%) adjacentthe veins which yielded the better gold values.
The larger and later calcite/quartzveins cut the core at anglesranging from 5 to 80” to the core axis, and the most common anglesare 30 to 60”. Theseveins are believedto dip 50 to 80” to the northeast.
It is impossibleto identify a breccia zone in the drill core that is equivalentto the brecciated andesiteat grid 11+45N,3+80SE, because all the rock encounteredin the drill hole is highly brecciatedandesite.
A 12 cm siltstonebed near the bottom of the drill hole indicatesa dip of 50 degreesto the northeast,but the severedisruption of the rocks throughoutthe drill hole bring into question the validity of the northeastdip.
45 b DISCUSSION
No economicprecious metal interceptswere encounteredin the 589 metres of bedrocktested by the four diamonddrill holes of the October 2002 program. The holes were designedto test the down-dip projection of brecciatedveined and alteredrock units that on surfacehad yielded gold valuesup to 5380 ppb. According to the explorationmodel, the gold values within the brecciatedrocks were supposedto increasewith depth toward the Fort Knox BasementFault.
The drill holesencountered brecciated, veined and alteredandesites equivalent to those seen on surface,but the gold valuesdid not increasewith depth. In fact, many of the gold values in the drill interceptswere lessthan those on surface.
It is obvious,in hindsight,that the surfacesamples were not representativeof the rock as a
‘c1 whole. ‘Ihe sampleswere collectedfrom knobs of outcrop with silica replacementand stockwork veining. The samesilica and stockwork veining that causedthe rock to be more resistantto erosionthan the surroundingrock also yieldedthe anomalousgold values. The localizedzones of silica replacementand stockwork veining encounteredin the drill holes simply did not contain gold valuesequivalent to the surfacesamples.
Although the generalexploration model held up well during the drilling program, there were a coupleof surprises. The first surprisewas that the Fort Knox BasementFault was found to dip at a more shallowangle (25”) to the northeastthen was originally thought. The new geometryplaces the fault at a depth of 180 to 190 metresbelow drill sites G-01 & G-03. The depth of the fault eliminatesthe possibility for finding near-surfaceconcentrations of preciousmetal depositson this portion of the property.
The secondsurprise of the drilling program was the discoveryof the late, thick (60 metre) rhyodacitesill that was intrusive into the Fort Knox BasementFault Zone. The sill occupies b 46
DISCUSSION continued
the BasementFault Zone in a position that the model predictedwould be Wed with stockwork veining and silica floodmg (with preciousmetal values).
The results of the drilling program were not all negative,however. The drill results provided ampleevidence that epithermalsolutions have ascendedthe BasementFault both below and abovethe rhyodacitesill. The epitlrermalsolutions have depositedelevated values of arsenic, antimony,mercury and thallium below the sill iu D.D.H G-03 (seethe Cross Sectionon Figure 9). The epithermalsolutions have also depositedcomposite veins within the brecciatedhanging wall andesitesabove the rhyodacitesill. Many of the veins dip steeplyor moderatelyto the northeastindicating a northeasternsource of the epithermalsolutions. The veins contain elevatedgold values(to 890 ppb), along with elevatedarsenic, antimony and sometimesmolybdenum values.
W Although the data is thin, somegeochemical zoning has beenrecognized in the drill samples. For instance,gold and key indicator elementvalues in samplesfrom D.D.H. G-03 are generallyhigher than those from D.D.H. G-01 to the northwest. There is also a notable increasein the gold/arsenicratio in samplesobtained from D.D.H. G-04 comparedwith the samplesobtained from D.D.H.‘s G-01, G-02 & G-03 drilled 200 metres to the southwest. Just 200 metresnortheast of D.D.H. G-04 the gold valuesincrease dramatically at the main vein where the Lacanadrilling program interceptedgold valuesof up to 8.023 oz/T over 0.50 metres (seeHistory).
All of the geochemicaland physicalevidence indicates a nearby sourcefor both the epithemralsolutions and the rhyodacitesill, and althoughmost of the epithermalsolutions are thought to postdatethe sill, it seemsclear that the point of origin of both the sill and the solutionsis the same. L DISCUSSION continued
Basedon all of the data collectedto date, the explorationmodel has beenrevised to suggest that a heretoforeunrecognized strong vertical fault cuts through the basementMonashee gneissat someshort distanceto the northeastof the LacanaMain Vein. The inferred fault is believedto have beenthe conduit for the Post-Marronvolcanism which coveredmuch of the Vemrer MeadowsGutlier with rhyodaciteash (now tuft). The rhyodacitesill which ascended the Fort Knox BasementFault is believedto be an offshoot from the samevolcanic event.
As mentionedabove, the auriferousepithermal solutions are believedto have originatedfrom the inferred vertical fault at some time after the intrusion of the rhyodacitesill.
The thick sill is very imperviousand the fact that epithermalsolutions have ascendedthe BasementFault alongboth the bottom and top of the sill indicatesthat the sill must be fractured and permeableat somepoint down-dip to the northeast. bf
The key to finding a sizeableeconomic precious metal deposit within the overlying andesites will be to locate where the rhyodacitesill is fractured, and to this end, a deeppenetration Induced Polarization(I.P.:) survey may be very useful.
Figure 11 has beendrawn to illustrate the main featuresof the revisedexploration model for the Gold mineral claims and the VemrerMeadows Tertiary Gather in general. Although conceptual,the diagramhas been drawn partially to scale. ln addition to the rhyodacitesill, the main featuresof the model are the vertical inferred fault, the Fort Knox BasementFault, and the intersectionof the two faults.
Figure 12 representsI. P. results that might be expectedto be coincidentwith the geology illustratedon Figure 11. It is expectedthat the unalteredMonashee gneiss basement rocks and an unbrokenrhyodacite sill will be outlined as resistiverocks, whereasthe andesite t 48
DISCUSSION continued brecciasand highly fractured fault zones(including those cutting the sill) will be outlined as conductiverocks.
I. P. surveys are also generallyuseful in defining pyritic rocks, and althoughpyrite is rare on the property, it is associatedwith someof the gold on the Gold 1 mineral claim.
Much of the Gutlier is coveredby overburdenor late rhyodacitetuff, and it is recommended that a trial survey of deep penetrationI. P. geophysicsbe conductedover the Gold 1-14 mineral claims to identify the main geologicalfeatures outlined above. If successful,the survey could be expandedto cover other portions of the Gntlier.
50 w CONCLUSIONS AND HECOMMENDATIONS
The four diamond drill holes drilled on the Gold 1 mineral claim during the October, 2002 program failed to locate economicconcentrations of preciousmetals within the highly brecciatedandesites of the Early EoceneMatron Formation. The best gold value (346 ppb) was obtainedfrom 25.26 to 26.38 metres in drill hole G-04 and the best combinedgold (162 ppb) and arsenic(1651 ppm) valueswere obtainedfrom 123.00to 125.30metres in drill hole G-03.
Of the 87 samplessubmitted for analyses,only 42 samplescontained geochemically significant amountsof gold and/or arsenic. Elevatedgold and arsenicvalues were found to occur with late, multiphasebanded and/or brecciatedcalcite/quartz veins; with silica replacementzones; and with chlorite/calcitealtered andesites containing blebs of hematite (after pyrite) or pyrite. Someof the sampleswith elevatedgold and/or arsenicvalues also u containedelevated values of antimony, mercury, thallium and molybdenum. Silver values were generallylow.
None of the drill core samplesyielded gold valuesequal to the best of the surfacesamples (1820 to 5380 ppb) collectedfrom the drill program area. The stainedand brecciatedsurface andesitesthat were sampledcontained stockwork quartz/calciteveinlets and somesilica replacement. It is now recognizedthat the outcroppingsthat were sampledstood up to erosionbecause of the stockwork veining and silica replacementand that they are not representativeof the andesitesin general. The drill holes simply did not encounterstockwork veining, or silica replacementzones with gold valuesequivalent to the surfacesamples.
D.D.H.‘s G-01 and G-03 were drilled through the entire Marron sequenceof andesitesand faulted rocks of the Fort Knox BasementFault. The holeswere stoppedin the Monashee gneissbasement rocks.
The BasementFault was found to dip more shallow (25”) to the northeastthan was previously thought, and the fault zone itself was found to be occupiedwith a 60 metre thick 51
CONCLUSIONS AND RECOMMENDATIONS continued rhyodacitesill. Each of these discoverieshad a negativeeffect on the October, 2002 program. The shallow dip of the BasementFault movedthe targetsdeeper on the southwest comer of the Gold 1 mineral claim and eliminatedthe possibility of finding near-surface preciousmetal depositson this portion of the property. The late rhyodacitesill occupiedthe BasementFault Zone in a positionthat was expectedto be tilled with stockwork veining, silica flooding and preciousmetal mineralization.
The samefeatures that were negativefor the October, 2002 program may prove to be positive for future drilling programs. The shallow dip of the BasementFault meansthat targetsto the northeastwill not be as deepas previouslythought. Also, the rhyodacitesill may be usedas a guide leadingto the ultimate sourceof the auriferousepithermal solutions.
The drill data indicatesthat most of the amiferous epithermalsolutions are late and that they have ascendedthe BasementFault both below and abovethe rhyodacitesill.
The geochemistryof the October, 2002 samplesillustrates zoning and a strongindication that the auriferousepithermal solutionshave invadedthe Marron andesitesfrom the northeast(see Discussion).
A revisedexploration model for the Gold property, and the Venner MeadowsTertiary Outlier, in general,is describedunder the previous-title and illustratedon Figure 11.
It is thought that a survey with deeppenetration Induced Polarizationmight produceresults that supportthe exploration model, and at least two trial lines of I. P are recommendedfor the Gold 1 mineral claim.
If the I. P results are effective, the entire 12 km long GoldenRainbow Claim Group should be consideredfor an expandedI. P. program. 0 \ January15,2003 - A+Pky& -- Kelowna, B.C. Murrafi orrison, BSc. 52 w REFERENCES
Exploration in British Columbia; Ministry of Energy, Mines and PetroleumResources; Annual Reports: 1975,p. E21; 1976,pp E 26-27; 1980,p. 33, 1981,p. 285; 1982,pp. 34-35; 1983, pp. 42-43; 1984,p.25; 1988, p. C21.
Geology, Explorationand Mining in British Columbia; B.C. Departmentof Mines and PetroleumResources, Ammal Reports: 1969,p. 294; 1970, p. 402; 1973,p. 47, 1974p. 56.
Larabie, E.N. 1987 Report on the O.K. Falls Gold Property,Osoyoos Mining Division, written for Tigris Minerals Corporationand Filed with a Prospectusfor listing on the V.S.E.
Little, H.W. 1961 : Geology, Kettle River (West Half) British Columbia;Geological Survey of Canada,Map 15 1961.
Meyers, R.E. 1988: preliminary EconomicGeology of the Vault Gold Deposit; Explorationin British Columbia 1988; Ministry of Energy, Mines and PetroleumResources, pp. B5B13.
Morin, J.A. 1988: Drilling Report on the Gold Property,Osoyoos Mining Division*.
Morrison, MS. 1992: GeophysicalAssessment Report, Fort Knox Claim Group, OkanaganFalls b Area, OsoycosMining Division.* 1993 : GeophysicalAssessment Report, Fort Claim Group, OkanaganFalls Area, OsoyoosMining Division.* 53 L REFERENCES continued
Morrison, M.S. (continued)
1994: GeologicalAssessment Report, Fort Knox Claim Group, OkanaganFalls Area, 0:soyoosMining Division.*
1995: Geophysical& GeochemicalAssessment Report, Fort Knox Claim Group, OkanaganFalls Area, OsoyoosMining Division.* 1995: GeophysicalAssessment Report, Rainbow Claim Group, OkanaganFalls Area, OsoyoosMining Division.* 1996: PercussionDrilling AssessmentReport, Fort Knox Claim Group, Okanagan Falls Area, OsoyoosMining Division.* 1997: Geophysicaland GeochemicalAssessment Report, Lucky Star Claim Group, OsoyoosMining Division.* 1997: GeologicalAssessment Report, Rainbow Claim Group, OkanaganFalls Area, OsoyoosMiming Division.* ‘c, 1997: PercussionDrilling AssessmentReport, Fort Knox Claim Group, Osoyoos Mining Division.* 1999 GeophysicalAssessment Report, Fort Knox Claim Group, OsoyoosMining Division.* 1999 & 2oooz GeologicalAssessment Reports, Rainbow Claim Group, OsoyoosMining Division.* 2001: GeologicalAssessment Report, Gold Claim Group, OsoyoosMining Division.* 2001: Geologicaland GeophysicalAssessment Report, Vault Claim Group, OsoyoosMining Division.* 2001& 2002 GeologicalAssessment Reports, Rainbow Claim Group, OsoyoosMining Division.* Peatfield,G. R. Data Review and Interpretationon the O.K. Gold Property,Osoyoos Mining 1989: Division. Private report preparedfor Tigris Minerals Corporation. u Wells, R. C. Report on O.K. Falls Projects. Private report preparedfor LacanaMining 1983: Corporation. *AssessmentReports filed with the Ministry of Energy and Mines of British Columbia. STATEMENT OF OUALIHCATIONS
I, Murray Morrison, of the City of Kelowna, in the Provinceof British Columbia, do hereby statethat:
1. I graduatedfrom the University of British Columbia in 1969with a B.Sc. Degree in Geology.
2. I have been working in all phasesof mining explorationin Canadafor the past thirty- three years.
3. During the past thirty-three years,I have intermittently held responsiblepositions as a ‘v geologistwith various mineral explorationcompanies in Canada.
4. I have conductedseveral geological, geochemical, and geophysicalsurveys on mineral propertiesin SouthernBritish Columbia during the pastthirty-three years.
5. I directedand supervisedthe diamonddrilling program outlined in this report.
6. I own an approximate50% interest in the Golden Rainbow Claim Group as of date of signingthis report.
January15,2003 Kelowna, B.C. 55 APPENDIX B
STATEMENT OF EXPENDITURES - ON THE GOLDEN RAINBOW CLAIM GROUP Statementof Expendituresin connectionwith a Diamond Drilling Program carried out on the Golden Rainbow Claim Group, located20 km southeastof OkanaganFalls, B.C. (N.T.S. Map 82-E-6W) during 2002.
DRILL SITE PREPARATION AND RECLAMATION Case580 Turbo 4x4 Tractor with front scoopand backhoe including operator and mobilization and demobilizationfrom Penticton,B.C. A & R Excavating1989 of Penticton,B.C. drill site levelling and digging of sumps 8 hrs. @ $75.OO/hr.plus $42.00 G.S.T. $ 642.
Reclamationwith Drilling Contractor’s550G John Deere Tractor with dozer blade: fIing in sumpsand recontouriugdrill sites bt 8 hrs @ $85.OO.hr.plus $47.60 G.S.T. 728.
M. Morrison, geologist,3 days drill site lay-out and chainsawclearing of old roads, 1 day Tractor supervision, 1 day cleaningup drill sites and seedinggrass seed with fertilizer total 5 days @ $3OO.@I/day 1500. 4 x 4 pick-up including gasoline 5 days @ $75.OO/day 375. Meals and Lodging no charge Grassseed 40. Fertilizer 18. Chainsaw 2 days @ $20.OO.day 40. Sub-total $3,343. 56 DRILLING COSTS
Contractor: BeaupreDiamond Drilling Ltd. of Princeton,B.C. Costs of mobilisation and demobilisationof the drill from and back to Princetonwere inclusive in the drill contract. Size BW Casing 78 ft @I$12.OO/ft. (23.77m @I39.377/m) $ 936. Size BQ Wireline drilling to 5OOft. 1496 ft. @ $11.60/ft. (455.98m @ $38.058/m) 17,354. Size BQ Wireline drilling beyond 500 ft. 434 ft. @ $12.75/ft. (132.28m @ $41.832/m) 5,534. 86 core boxes @ $7.50 645. 7% G.S.T. on contract costs of $24,469. 1,713.
Drill Supervision: M.S. Morrison, geologist,of Kelowna, B.C. 17 days direct drill supervisionand on site core logging 3 days sampleselection and core splitting total 20 days @ $3OO.OO/day 6,000. 4 x 4 pick-up, including gasoline20 days @$75.OO/day 1,500. lodging and meals(average) 20 days @ $56.OO/day 1,120. off-site core loggingand selectionof sampleintervals 4 days @ $3OO.OO/day 1~00. core splitting 3 days @ $lOO.OO/day 300. rental of core splitter no charge ___ Sub-total $36,302. 57
L ASSAYING COSTS
Samplebags $ 83. ShippingCosts (bus expressto Vancouverlab) 128. 87 samplesanalyzed at a cost of $14.98 each 1,303. (10 g split and ICP-MS analyses) Sub-total $1,514.
REPORT PREPARATION COSTS
M. Morrison, geologist 10 days @ $3OO.OO/day $ 3,000. (organisingdrill logs for presentation,drafting, crosssections and maps,analyzing all data and writing report) Drafting of formal mapsand crosssections for the report 297. Typing: drill logs, tables,legends and report 200. ‘u Copying maps,figures and reports 60. Sub-total $3,557. GRAND TOTAL $44,716.
I hereby certify that the precedingstatement is a true statementof monies expendedin connectionwith the DiamondDrilling Programcarried out October l-23,2002.
January15,2003 Kelowna, B.C. Murray Morrison, Geologist Invoice # 012 October 3 1,2002
Doublestar Resources Ltd. #305-1549 Marine Drive Vancouver,BC V7V lH9
RF,: Venner Meadows Property
Hole Degree Size Depth Price Total G-01 70’ BW O-24 $12.00 $288.00 BQ 24-500 $11.60 $5521.60 500-707 $12.75 $2639.25 G-02 65’ BW O-18 $12.00 $216.00 BQ 18-297 $11.60 $3236.40 G-03 60’ BW o-22 $12.00 $264.00 BQ 22-500 $11.60 $5544.80 500-727 $12.75 $2894.25 G-04 70’ BW O-14 $12.00 $168.00 BQ 14-277 $11.60 $3050.80 -& G-05 70 BW O-13 $12.00 $156.00 BQ 13-500 $11.60 $5649.20 500-537 $12.75 $471.75 Core Boxes BQ core boxesused on Holes G-01 to G-05: 109 boxes@ $7.50 $817.50 Tractor Time Dozer usedin moving and reclamationof site 18 hours@ $85.00 $1530.00 Water Hauling G-05 Hauledreceiving tank to propertyfrom Princetonand back. $300.00 Hauledwater 10 kilometersreturn trip. 3 days@ $400.00per day $1200.00
Sub-total $33947.55 Gst $2376.32 Total Invoice $36323.87
LessAdvance $15000.00
Total Owing $21323.87
Thankyou,
j&j /g ,$&L&&& Beaupre Diamo&brilling Ltd. R. Beaupre,Pres. 652 East Hastings..VanWuVar. B.C., CANADA Phone: (604) 2634158 Fax: (604) 253-1716 Our GST # 100035377RT ‘L DOUBLESTAR RESOURCES LTD. Inv.#: A205354 305 - 1549 Marine Drive Date: Dee 16 2002 Wgt,~-wxuver, BC F,T, Fmb k/lo k
i QTY ASSAY ,;,.).:.;‘.::,‘.~ PRICE AMOUNT , 1 30 GROUP IDA (10 gm) @ 30 R150 -CORE @
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Please pay last amount shown. Returp one copy of ihi Invoke with payment. TERMS: Net two weeks. 1.5 % per month charged on overdue accounts. [COPY21
PB 3Wd ACME ANALYTICAL LABORATORIES LTD. 652 East Hastings,, Vancouver,B.C.. CANADA V6A IR6 Phone: (604) 253-3156 Fax: (604) 253-1716 # Our GST %loo035377 RT
DOUBLESTAR RESOURCES LTD. Inv.#: A205317 305 - 1549 Marine Drive Date: Jan 3 2003 West Vancouver, BC V7V lH9
519.85 36.39 556.24
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Please pay last amount shown. Return one copy of this Invoke wlth payment. TERMS: Net two weeke. 1.5 % per monlh’ charged on overduo accounts. [COPY11
EB 39Wd WEzrMlm 0828ZZ6PE49 LZ : t &BQZ/6T/EB ACME ANALYTICAL LABORATORIES LTD. 852 EastHasting& Vancouver, B.C., CANADA WA 1 R6 Phone: (604) 253-3156 Fax: (604) 253-1716 Our GST# 100035377FIT
DOUBLESTAR RESOURCES LTD. Inv.#: A300101 305 - 1549 Marine Drive Date: Jan 23 2003 Wff~t,~-icouver, SC
:: WY ASSAY ,.;.:,.:..‘.,. PRICE AMOUNT b ,.;; .,. .,. I I 26 GROUP 1DA (10 gm) @ 254.80 24 RI50 - CORE @ 102.00 2 R150 - ROCK @ 8.50
390.87 3
Samples submitted by M. Morrison FILE # A300101 & A300102 t
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39Vd tlvls3lElloa 88ZSZZ6P89 Lz :tt EBBZ&T/EE, APPENDIX C
DRILL HOLE LOGS DRILL HOLE D.D.H. GO1 iu DOUBLESTAR RESOURCESLTD - GOLDEN RAINBOW CLAIM GROUP- DIAMOND DRILL RECORD
DRILL HOLE: D.D.H. G-01 SECTION: 2+OOSE PAGE 1 of 7 PROPERTY LOCATION: 20 km southeastof OkanaganFalls, B.C. DRILL HOLE LOCATION: 142 m south and 470 m west of the L.C.P. of the Gold 1 Mineral Claim PROPERTY GRID: 10+39N, 2+OOSE AZIMUTB: 225” DIP: -70” LENGTH: 215.49m DRILL TYPE: Longyear 38 CORE DIAMETER: BQWL DIP TESTS: none ELEVATION: 1429m DATE STARTED: October 8,2002 DATE COMPLETED: October 13,2002 LOGGED BY: M.S. M?rrison, DRILLING CONTRACTOR: Beaupre Diamond Drilling Ltd., Princeton, B.C. COMMENTS: 1. Casing to 7.32; removed from drill hole at the completion of the job. 2. Core recoveriesare 100% unless otherwise recorded
DESCRIPTION: 0.00-0.3om drill collar 0.30-7.32m casing in boulder till 7.32~7.48m gneisic cobble (surfacerock) 7.48-142.80m EARLY EOCENE MARRON FORMATION
The Marron Formation is comprised of minor andesitic flows that are intercalatedwith talus breccias comprised of a mix of andesitic clasts. There are three dominant types of porphyritic andesiteclasts that are recognizedin the core along with varieties of andesitestoo numerous to single out. A grey porphyritic andesitewith 5-15% plagioclasephenocrysts of 3-5 mm and 5% black augite phenocrysts,up to 5 mm, is called Type 1. Type 2 andesiteis also grey or green and contains plagioclaseand augite phenocrystsequalling V 10% each. Type 3 andesiteis green with black augite phenocrystsof 3-5 mri~ comprising lo-20% of the rock. In all of the porphyritic andesites,the groundmassminerals are very fme-grained
The talus breccias are well indurated and they contain very little interstitial material. Early tight fractures are mended with l-3% calcite veinlets, O.l-3mm, most of which are highly disrupted.
All of the andesiteshave been subjectedto late tectonic movement and tectonic breccia zones of a few centimetresin width to a few metres are seen in the core. Only some of the breccia zones are mended with calcite/quartz veinlets or silica.
The andesitesare generally slightly to moderately altered to chlorite and calcite. The alteration is most intense in the late fme clast tectonic breccias.
The andesitesare also cut by later bandedcalcite/quartz veins of a few centimetres in width. Pyrite occurs in trace amounts throughout the rock, but there is a notable increasein pyrite near the late calcite/quartz veins. Blebs of hematite in some of the andesitesmay representoxidized pyrite.
‘Ihe talus breccias have been separatedfrom one anotherin the log that follows basedon which andesitic clasts are predominant: Types 1, 2 or 3.
Special featuressuch as veinlets, veins, tectonic breccias, silica replacementzones and mineralization (pyrite and hematite) are also recordedin the log that follows:
b Can’t G-01 Page 2
7.48-45.17m Large Ciast Talus Breccia 7.48-28.15m mixed large clssts (5-15 cm) of predominantly Type 1 andesitewith intervals of late brecciation with fmer clasts, moderateto strong chlorite/calcite alteration which is strongestin late breccias,Z-3% calcite/quartzveinlets, l-5 mm, most are highly disrupted, some late veinlets at 60 to SO”, trace to 0.25% disseminatedpyrite 7.48-7.6Qm soft gouge 7.80-810m brecciated,clasts up to 1 cm 8.23-8.50111 brecciated,clasts up to 3 cm 9.58-13.41m brecciated,but very little spacebetween clasts, 1% calcite/quartz veinlets, l- 4mm, some at 45 to 60’, most are highly disrupted 9.58-10.52and 10.81-l 1.36m soft, gouge 11.90-12.05and 13.35-13.41m soft, broken core 13.41-13.95m 2% calcite/quartzveinlets, l-4mm, highly disrupted,one late veinlet at 80” to con? 13.95-14.45m 20 cm (true width) composite, bandedand brecciatedquartz 70%/calcite 30% vein, no sulphides, late bandedquartz/calcite veins within brecciatedvein at 20”) upper contact at 20”) lower contact at 70” Samole 58301 = 13.95 to 14.45m composite vein 14.45-16.40m light green, moderatechlorite/calcite alteration, trace of calcite/quartz veinlets, 0.1-0.5 mm, highly disrupted, 0.25% very fine disseminatedpyrite Sample 58302 = 13.41 to 16.46m (excluding composite vein) ‘clr 16.40-19.77m grey andesiteclasts, original texture very dismpted, moderatechlorite/calcite alteration, 2% calcite/quartz veinlets, 1-4mm, disrupted 16.46-16.90m 30% moderately replaced with silica, 0.25-0.5% pyrite Sample 58303 = 16.46 to 16.90m Samale 58304 = 17.45 to 18.75m 0.5% pyrite disseminated at 18.92m 1.5cm late qnartzjcalcite vein at 70” 19.77-21.13m grey to green andesiteclasts, moderatechlorite/calcite alteration, moderate disruption, 5% calcite/quartz veinlets, l-20 mm Sam& 58305 = 18.75 to 20.55m at 20.86m 2 cm red hematitic zone at 55”, 5% stockwork of quartz/calcite veinlets, 5% PYrh-e at 21.06 and 21.12m two 1.5 cm quartz/calcite veins at 35 and 45’, 30% late calcite veinlets cutting quartz veins, trace of pyrite on contacts Samole 58306 = 20.55 to 22.22m 21.13-22.22m green to grey andesiteclasts, moderatechlorite/calcite alteration, 3% calcite/quartz veinlets, l-3 mm, highly disrupted,2% red hematite blebs with (residual?)pyrite to 1% 22.22-23.69m as above, but only 1% calcite/quartz veinlets at 23.W23.68m sheerzone with foliation at 45” 24.00-24.16m hi@y disrupted 24.16-28.15m grey andesiteclasts, slight chlorite/calcite alteration, 1% very fme Cakite/quartzveinlets, highly disrupted, one late quartz/hematiteveinlet at 50’ 26.75-26.82m 5% calcite/quartz/hematiteirregular broken veinlets w at 27.54m 1 cm quartz/calcite vein with 2 mm hematite selvage on upper contact at 75” G-01 Page 3
28.15-34.95m large clast breccia of predominantly Type.2 and&e, but also Type 1 & 3 and&es, slight to moderatechlorite/calcite alteration, 1% calcite/quartz veinlets, .02-3 mm, most are highly disrupted at 28.54m two 5 mm late calcite/quartzveins at 40’ 32.00-33.83m highly disrupted 32.17-32.27,32.35-32.83 and 33.30-33.83m late brecciated zones 34.45 - 35.32m highly fractured 34.95-45.17m large clast breccia of predominantly Type 1 andesite,moderate chlorite/calcite alteration, 2-3% calcite/quartzveinlets, OS-15 mm, most are highly disrupted at 35.25m 0.5 cm quartz/calcite vein at 2O”with 1 mm hematite selvage at 36.18m 1 cm zone of quartz/calcite/hematiteveinlet, highly disrupted at 36.91m 0.3 cm quartz/calcite/hematitevein at 80” at 37.3Om two, 1 cm quartz/calciteveins at 70” at 38.27m 1.5 cm late banded calcite/quartzvein at 35” at 38.76m 1 cm late calcite/quartz vein at 55” at 40.43m 1 cm late calcite/quartz vein at 70” 37.33-37.48,37.62-38.18, 38.52-38.71 and 39.47-39.58m small late breccia zones with 1 cm clasts and very little movement 40.66-41.76m same as above, but 2 cm clasts 41.87-42.32m late breccia zone at 43.2Om 1 cm late, banded calcite/quartzvein at 20” at 44.35m 1 cm late, banded calcite/quartzvein at 10” w at 45.17m contact with green augite andesiteat 60 to 70’ 45.17-72.78m Green Aueite Andesite Flow 45.17-72.78m green augite andesiteflow, 5-10% augite phenocrysts,l-5-, in very fme- grained green groundmass,moderate chlorite/calcite alteration, 2% calcite/ quartz veinlets, 0.5-10 mm, some highly disrupted 45.17-45.74m moderate alteration and disruption 45.74-48.51m strong alteration, highly disrupted 46.20-46.90m breccia zone, clasts up to 1.5 cm at 47.05m 1 cm late.calcite/quartz vein at 80” at 47.18m 0.5 cm late calcite/quartz vein at 80” at 47.5Om 1 cm late calcite/quartz vein at 20” at 47.98m 1 cm late calcite/quartz vein at 90” 48.51-48.71m breccia zone at 70”, highly disrupted and altered to green and grey very fine grain minerals, soft 48.71-54.90m all brecciated augite andesite at 48.8Om 1 cm irregular calcite/qua* vein at 10” 49.56-49.78and 50.20-50.55m late breccia zonesmended with silica and calcite/quartz veinlets SamDIe 58307 = 49.56 to 5055m 50.90-52.05m 3% irregular calcite/quartz veinlets l-20 mm, disrupted 53.05-53.48m 5% irregular calcite/quartz veinlets l-20 mm, disrupted 53.48-54.90m 1% irregular calcite/quartz veinlets l-3 mm, disrupted 54.90-63.OOm same augite andesite,moderate to strong chlorite/calcite alteration, 1% calcite/quartz veinlets l-10 mm, highly disrupted, very local zones (1 cm) of ‘v silica replacement 56.20-56.71and 57.21-57.37 fme clast breccia, 0.25-l cm clasts, possible contacts betweenflows (?) 60 to 80” G-01 Page 4 G at 61.05 and 62.OOmm 1 cm late calcite/quartzveins at 30” 63.00-70.22m same green augite andesite,generally massive with only small breccia zones 65.45-66.44, 67.15-67.50 and 68.56-68.88111 well brecciatedcrumbly core Samole 58308 = 65.45 to 67.15m at 69.93m 1.5 cm late, multiphase quartz/calcitevein at 70”, both clear and white quartz 70.22-72.78m same augite andesite,lighter green with stronger chlorite/calcite alteration 70.22-72.28m 6 cm multiphase, banded quartz 70%/calcite 30% vein at 70”) both clear and white qua* at 70.56m 1 cm quartz/calcite vein at 80” at 72.56m 1.5 cm bandedquartz/calcite vein at 85” at 72.74m 1 cm bandedquartz/calcite vein at 65”,dismpted, other minor 0.5 cm banded quartz/calciteveins at 60 to 80” Sam& 58309 = 70.22 to 73.43m 72.78-137.88 Large Clast Talus Breccia 72.78-77.3Om large clast breccia of predominantly Type 3 andesite,also some Type 1 & 2 andesite,moderate chlorite/calcite alteration Samole 58310 = 73.43 to 74.47m 75.00-77.30m highly fractured, 2% calcite/quartz veinlets, 1-3 mm, highly disrupted 77.30-91.4Om large clast (5-10 cm) breccia of predominantly Type 3 andesite,also some Type 1 & 2 and mixed andesites,moderate chlorite/calcite alteration, 2% calcite/calcite veinlets, 1-5 mm, highly disrupted, minor zonesof weak silica replacement V Sample 58311 = 80.80 to 8155m 91.40-102.85m purple and dark green large clast (5-15 cm) breccia of predominantly Type 3 & 2 andesites,but also several other types of andesite,moderate chlorite/calcite alteration minor veinlets, highly disrupted 91.42-91.71m late brecciatedzone 91.71-92.67m 1% calcite/quartz veinlets, l-2 mm, disrupted 92.41-92.61m late breccia zone 92.67-98.61m l-236 calcite/quartz veinlets, l-4 mm, some are at 1O”or 80”, but most are highly diSrUpted at 92.73m 1 cm late calcite/quartz vein at 30” 94.25-94.29m late breccia zone 94.68-94.75m shear zone at 50” 96.80-97.05m shearing at 50” 98.00-98.3Om late breccia zone 98.61-102.85m l-2% calcite/quartz veinlets, 1-4 mm, highly disrupted,trace of very fme- grained pyrite 99.67-99.97and 100.50-100.93m late breccia zones, 1 cm clasts 102.85-112.71m lighter green, large clast (5-50 cm) breccia of predominantly Type 2 andesite, moderate.chlorite/calcite alteration, some contactsbetween clasts are gougy, but no veining 104.65-105.7Om as above, but rock becomes more soft and altered down hole 105.70-112.67 l-2% calcite/quartz veinlets l-10 mm, highly disrupted 104.44-105.7Om gow ‘v 105.70-106.26m late breccia zones with 0.25-l cm clasts 109.54-109.7Om late breccia zones with 0.25-l cm clasts 109.95-l10.27m late breccia zones with 0.25-l cm clasts GO1 Page 5 bf at 106.89m 1 cm late calcite/quartzvein at 60” at 108.8Om 3 cm late, bandedcalcite SO%/quariz50% vein at 45” 112.50-l 12.6Om late breccia zone 112.71-126.80 purple and dark green large clast (5-30 cm) breccia of Type 3 & 2 andesites, moderatechlorite/calcite alteration, 2-3% calcite/quartzveinlets, l-3 mm, highly disrupted 114.05-l 14.58m late breccia zone with 0.25 - 1 cm clasts 115.72-115.98m late breccia zone with 0.25 - 1 cm clasts 117.50-l17.7Om banding at 70” 117.72-118.03m 1% orangeto brick red hematite 117.70-l 19.87m late breccia zone, some banding at 60” 119.08-l 19.81m 2% orange to brick red hematite 119.87L126.80m l-5% calcite/quartzveinlets, some at 5 to lo”, most are highly disrupted, l-5% brick red hematite blebs and streaks often near quartz/calcite veinlets 120.00-123.45m 3% orangeand red hematite Samole 58312 = 120.00 to 123.45m 124.51-125.40and 126.40-126.55m 3% orange and red hematite (hematite probably representsaltered PYrW 126.80-133.20m dark green chlorite altered and purple hematitic large clast (5-10 cm) breccia of Type 3 & 2 andesites,1% hematite with local 5 cm zones of 3% hematite, l-5% irregular calcite/quartz veinlets, l-3 mm, most disrupted, some at 30 to 50” w 126.80-128.05m late breccia zone with 0.2-lcm clasts 133.20-133.90m some large clast breccia as above, but lighter green and grey, becauseof stronger chlorite/calcite alteration 133.90-137.88m mixed large clast breccia of Type 1,2 & 3 andesites,plus other andesites, moderatechlorite/calcite alteration l-2% calcite/quartz veinlets, l-4 mm, disrupted Samale 58313 = 133.20 to 133.80m 133.90-134.18m late breccia zone, 0.2-1.5 cm clasts, lower contact at 55” 134.S134.70m 4 cm (true width) quartz 80%/calcite 20% vein at 20” 134.85-134.95m 2 cm (true width) quartz 8O%/calcite20% vein at 20” Samale 58314 = 134.38-135.OOm 136.25-137.41m 3-5% orange/redhematite (after pyrite?) Sam& 58315 = 136.25-137.41m 137.20-137.41m 21 cm late breccia zone with 40% calcite and 5% quartz mending 137.88-140.72m Par& to Brick Red Amvgduloidal Andesite Flow the andesiteis hematitic and very fine-grainedwith 10% amygctules,2% irregular calcite/quartzveinlets, l-4mm, disrupted, possible upper contact at 75” at 139.35m banding at 60” 139.45-139.95m well fractured 139.95-140.26and 140.65-14l.OOm late breccia zones, soft 140.72-142.80 Transitional Contact Zone with Rhvodacite Sill 141.00-141.44m late breccia zone, 50% quartz clasts, 20% volcanic clasts, 30% light green w calcite/clay matrix upper contact at 85”) lower contact with intrusive at approximately 50” Sample 58316 - 141.00-141.44m G-01 Page 6
141.44-142.1.Sm rhyodacite sill Samale 58317 = 141.38to 142.16111 142.15-142.52m dark grey andesite 142.52-142.8Om interbandedrhyodacite intrusive and andesite SamDIe 58318 = 142.52 to 14550m at 142.8Om main intrusive contact at 80” 142.80-202.55mm Porphvritic Rhvodacite Sill very homogeneousporphyritic rhyodacite with 20% rounded pink or orange orthoclasephenocrysts, 2-S mm, and 3% fiie-grained mafics set in a very fiie- grained groundmass,l-2% early micro calcite veinlets, most of which am highly disrupted, slight to moderatechlorite alteration (the alteration is most intensewhere the rock is well fractured), weak hematite stains the intrusive pink locally, late calcite/quartsveinlets and pyrite are rare. Special features within the sill are listed below. 146.67-146.75m late breccia zone Samole 58319 = 145.00 to 147.80m 142.80-154.6Sm light grey rhyodacite,joints at 25, 30, 40, 50, 65 & 80”) slight to moderate chlorite alteration, 112%calcite/qua* veinlets, OS-2mm, some at 50 & 70”, others highly disrupted SamDIe 58320 = 147.80 to 150.05m 150.05150.23m late breccia zone, 20% light green chips and gouge 150.23-152.OOm highly fractured, tight fractures, light green with strong chlorite alterations Samole 58321=150.05 to152.OOm 152.00-154.65m highly fractured with tight fractures, dusting of pyrite on late fracture surfaces Sample 58322 = 152.00 to 154.65m 154.65-161.90m some late calcite/quarts veinlets at 70 & 80” 154.65-155.9Om slight chlorite alteration, dusting of pyrite on late fractures Sample 58323 = 154.65 to 155.90m 155.90-158.50m slight chlorite alteration Samole 58324 = 155.90 to 158.50m 158.50-160.4Sm weak chlorite alteration, trace of pyrite Sam& 58325 = 158.50 to 160.45m 163.00-164.74m weak chlorite alteration. light green chlorite on fractures Sample 58326 = 163.00 to 164.74m 164.60-165.00and 165.25-165.45m well fractured with 1% micro calcite/quartzveinlets filling fractures, trace of pyrite Sample 58327 = 165.50 to 168.87m 168.87-175.7Om 1% stockwork of calcite/quartsmicro veins throughout,some late veinlets at 30 to SO”, trace of very fine-grained pyrite, rock is darker grey than above, with less chlorite alteration 175.70-182.62m light grey rhyodacite, moderatechlorite alteration, 1% stockwork of micro calcite veinlets 179.10-179.20,180.94-181.49 and 181.94-182.3Omwell fractured with tight fractures, chlorite on fractures 182.62-189.55m light grey, light green (chlorite alteration) and locally pink (weak hematite) u rhyodacite, 24% stockwork of micro calcite veinlets filling tight fractures, minor late veinlets at 50 to 80’ 182.75-182.8Sm 10% stockwork of calcite veinlets G-01 Page 7 b 188.70-189.05m late breccia zone with 3-5% calcite veinlets 189.48-189.64m 5% stockwork of veinlets, veinlets also disrnpted 189SS-19666m light grey rhyodacite, slight to moderatechlorite alteration, l-3% calcite veinlets, 0.5-10 mm, most are highly disrupted at 191.98m 1 cm late calcite vein at 35” at 197.8Sm 1 cm and 2cm calcite veins at 30 & 70” 199.19-199.85m dark grey, highly fractured 199.85-2006Om grey, well fractured, 2-456calcite veinlets, l-10 mm, most are highly disrupted, some late veinlets at 70” 200.60-201.15m dark grey to green rhyodacite 201.15-215.49m Fort Knox Basement Fault 201.15-201.18m my gow 201.18-202.55m green,highly chloritic, highly foliated (rhyodacite intrusive or andesite?) foliation (equals shearing)at 65 to 70”, l-2% calcite veinlets, OS-1 mm, most are highly disrupted 202.55-215.49m Pre-Permian Monashee Gneiss 202.SS-203.7Om green,highly disrupted rock replacedwith chlorite 6O%/quarta40%, trace of late quartz/calcite veinlets, OS-1 mm, at 70 to SO”, up to 0.25% pyrite locally 203.70-209.4Om generally highly disrupted and altered gneiss,20% chlorite and 20% quartz replacement,minor 2-10 cm zones of unaltered gneiss at 204.02m 2 cm late quartz vein at 80” at 204.67m 2 cm late quartz vein at 65” v at 204.9Om 1 cm late quartz vein at 70” 205.70-205.79m late quartz vein at 70” Samole 5&154 = 202.65 to 206.OOm 206.48-206.58m late quartz vein at 80’ at 207.30m 4 cm white. and pink pegmatite dyke at 50” at 208.77m 1 cm white and pink pegmatite dyke at 80” 209.40-210.94m black gneiss, much less disrupted and altered than above 209.55-210.2Sm well fractured gneiss 10% quartz/chlorite replacement,and mending fractures at 209.45m foliation at 50” at 210.6Sm foliation at 70” 210.94-211.38m highly brecciatedgneiss, 40% chlorite and 20% quartz mending breccia, trace to 0.5% pyrite 211.38-212.95m much less disrupted gneiss than that above, 3-S% quartz/chlorite veins, trace to 0.5% pyrite 211.68-211.79m well fractured, 10% qnartz/chlotite veins mending fractures at 211.81m 1 cm quartz vein at 80” at 211.94m 2 cm pegmatite dyke at 80” 212.40-212.9Sm well fractured, 5% quartz/chlorite veins mending fractures 212.95-215.49m highly disrupted gneiss, 15% quartz and 15% chlorite replacement 213.45-213.47and 214.52-214.SSm zones of 10% quarts, 3% pyrite, highly disrupted (possibly broken veins?) Sample 58455 = 212.95 to 214.56m 214.52-215.49m well fractured gneiss with 5% quartz/chlorite veinlets, l-2 mm, mending w fractures,veinlets are also highly disrupted, gneissic foliation 60 to SO”, average70” 215.49m end of Drill Hole G-01 Significant Values Obtained from Selected Drill Core Intervals of D.D.H. G-01 w Sample Interval Gold Arsenic Antimony Molybdenum Sulphur Special Number (in metres) E&. PDF pm ppm % Features
58301 13.95-14.45= 0.5Om 190.0 3.7 20 cm qtz/cal vein 58302 13.41-16.46- 3.05m 20.9 42.7 excluding vein 58303 16.46-16.90= 0.44m 23.4 76.0 14.7 1.52 somesilica 58304 17.45-18.75= 1.3Om 10.6 58.6 0.5% pyrite 58306 20.55-22.22= 1.67m 13.4 114.4 2.4 0.44 small veins 58307 49.56-50.55= 0.99m 76.9 311.0 3.5 17.4 0.60 some silica 58308 66.45-67.15= 0.7Om 8.1 77.4 brecciated 58309 70.22-73.43= 3.21m 54.7 708.9 7.9 0.75 small veins 58311 80.80-81.55= 0.75m 2.7 242.5 3.2 0.37 some silica 58455 212.95-214.56= 1.61m 29.8 quartz/pyrite
Pleasesee the drill logs for a completedescription of the samples.
Pleasealso seeAppendix D for the valuesobtained for all 35 elementsthat were analyzed, DRILL HOLE D.D.A. GO2
‘Ir DOUBLESTAR RESOURCESLTD - GOLDEN RAINBOW CLAIM GROUP- DIAMOND DRILL RECORD
DRILL HOLE: D.D.H. G-02 SECTION: PAGE 1 of 6 PROPERTY LOCATION: 20 km southeastof OkanaganFalls, B.C. DRILL HOLE LOCATION: 250 m south and 396 m west of the L.C.P. of the Gold 1 Mineral Claim PROPERTY GRID: 10+22,5N,3+33SE AZIMUTH: 125” DIP: -65” LENGTH: 90.53m DRILL TYPE: Longyeat 38 CORE DIAMETER: BQWL DIP TESTS: none ELEVATION: 1437m DATE STARTED: October 13,2002 DATE COMPLETED: October 16,2002 LOGGED BY: M.S. Mot&on DRILLING CONTRACTOR: DeaupteDiamond Drilling Ltd., Princeton, B.C. /$-A& COMMENTS: 1. Casing to 5.49m; removed from drill hole at the completion of the job. 2. Core recoveriesate 100% unless otherwise recorded.
DESCRIPTION: O.OO-0.20m drill collar 0.20-5.49m casing 5.49-90.53m EARLY EOCENE MARRON FORMATION
All of the Matton Formation encounteredin the drill hole is a talus bteccia comprised of a mix of andesite clasts of which three types ate predominant. Type 1 is a potphytitic plagioclase andesite,Type 2 is a potphytitic plagioclase/augiteandesite and Type 3 is a potphytitic augite andesite.(These andesitesate describedmote fully with the log of D.D.H. G-01.)
The talus bteccias ate well inchuatedand they contain very little intetstitial material. Early tight fractures ate y mended with l-3% calcite veinlets, 0.1-3 mm, most of which ate highly disrupted.
All of the talus bteccias have been subjectedto late tectonic movement and several bteccia zones tanging from a few centimetresto a few metres ate seen in the core. Only some of the bteccia zones ate mended with calcite/quartz veinlets of silica.
The andesitesexhibit several degreesof chlorite and calcite alteration tanging from slight to intense ‘Ihe mote fractured rock is generally the most altered and some of the finer later bteccia zones ate highly altered.
The andesitesate also cut by later banded calcite/quartzveins of a few centimetresin width. Pyrite occuts in trace amounts throughoutthe rock, but there is a notable increasein pyrite neat the late calcite/quartz veins. It is thought that the blebs of hematite which occut in some of the andesitesrepresent oxidized pyrite.
The talus bteccias have been sepatatedfrom one anotherin the log that follows, based on which andesitic clasts ate the most predominant,Type 1, Type 2 ot Type 3.
Special featuressuch as veins, veinlets, tectonic bteccia zones,silica replacementzones and minetalization (pyrite and hematite) ate also recordedin the log that follows.
cont’d GO2 Page 2 L 5.55-90.53m Large Clast Talus Breccia 5.5%12.65m mixed large clasts (lo-15cm) of predominantly Type 1 andesite,but also Type 2 andesite;slight to moderatechlorite/calcite alteration, trace to 1% calcite/quartz veinlets, most are highly disrupted. 6.00-7.OOm 90% co*e recovery 8.68-12.16m disrupted and chlorite/calcite altered, slight hematite staining Samale 58341 = 8.68 to lO.OOm at lO.OOm 4 cm (true width) bandedquartz vein at 25” with l-2 mm band of pyrite at centre of vein Samale 58342 = 10.00 to 10.OSm quartz vein at 11.88m 1 cm brecciatedquartz vein at 40“ Sample 58343 = 10.08 to L12 16m 12.65-1956m mixed large clasts (lo-15 cm) of predominantly Type 1 andesite,minor type 2 andesite at 12.20m 2 cm quartz vein at 10” with 1 to 2 mm pyrite on edgesof vein at 13.95m 5 cm broken zone 15.00-15.97m disrupted and chlorite altered, 5% open space at 15.Wm 0.5 cm bandedquartz veinlet at 40” at 15.10111 1 cm banded quartz veinlet at 40” 15.97-18.30m much less disrupted, weakly chlorite altered, several textural changesin clasts, 1% calcite/quartz veinlets 18.30-19.56m highly disrupted,fme clast (0.1 to 2 cm) breccia ‘c, 18.40-18.70m 70% breccia, well altered, 2 to 5 cm clasts within breccia are less altered, 3% rusty blebs, highly disrupted at 19.06m 0.5 cm bandedquartz vein at 35”; with 0.5 mm pyrite selvages Sample 58344 = 18.30 to 19.56m 19.56-23.20m real mix of clasts, but predominantly Type 1 andesite,most is highly disrupted and well chlorite altered 19.56-21.65m brecciated to 0.5-2 cm cl&s, some 5 cm clasts, 2-3% pyrite mostly weathered to rust on fractures and within breccia matrix at 19.95m 1 cm quartz/calcite vein at 30” with hematite (after pyrite?) s&age Samole 58345 - 19.56 to 2165mI 21.65-23.20m as above, but some 5 to 15 cm clasts between zones with fme clasts, 2-3% calcite/quartz veins, 1% pyrite mostly weatheredto rust. at 22.03m 1 cm calcite/quartz vein at 25” at 23.03 and 23.10m 3 mm quartz veins with pyrite selvages Sample 58346 - 21.65 to 23.20m 23.20-25.80m large clast (lo-15 cm) breccia with mix of andesiteporphyries Types 1, 2 and others,highly chlorite/calcite altered, white, light grey and light green, 3% quartz/calciteveins at 23.65m 1 cm late bandedquartz vein at 35’ Sam& 58347 = 23.20 to 2420m some silica replacement at 24.65m 1 cm late bandedquartz vein at 35” at 24.97m 0.5 cm, banded quartz vein at 45”, disrupted at 25.02m 1 cm banded quartz vein, disrupted ti GO2 Page 3
25.66-25.76m three 1 cm bandedquartz veins at 45 to 50”) lowermost vein has very fme pyrite selvage 24.20-25.65m moderatesilica replacement SamDIe 58348 = 24.20 to 26.52m 25.80-26.52m highly chlorite altered and silica replaced,light grey and green, 10% quarts veins, black chlorite s&ages on most veins, 2 to 3% pyrite at 25.85m 5 cm multiphase, brecciatedquartz vein at 90” at 25.98m 2 cm bandedquarts vein at 50” at 26.18m 0.5 cm bandedquartz vein at 50” at 26.3Om 1.5 cm bandedquarts vein at 50”, highly disrupted 26.30-26.47m grey breccia zone mended with very fine quartz veinlets, 5% pyrite 26.52-27.46m breccia zone highly replaced with silica, 10% late quartz 90%/calcite 10% veinlets, 2-3% pyrite at 26.6Om 3.5 cm bandedand brecciatedquarts vein at 35” 26.7527.46m 10% of silica replacedzone is comprised of 10% disrupted quarts veins (1 cm) at 45 to 60”, lower contact of silicified zone is 45”, there is late brecciation of silicified zone and pyrite is late and lies betweenbreccia clasts Sample 58350 = 26.52 to 27.46m silica replacementzone 27.46-29.16m moderately altered and silica replaced,well brecciated,but also some larger unbroken clasts, hematite on tight fractures at 27.99m 1 cm bandedquartz vein at 60” 28.73-28.91m late breccia zone, well silicified with 10% late quarts and 5% pyrite, best w pyrite is with latest brecciation SamDIe 58351 = 27.46 to L29 16m 29.16-33.48m still large clast breccia of predominantly Type 1 andesite,slight to moderate chlorite alteration, local areasof high disruption, l-2% red hematite (after pyrite) blebs equal 70% hematite and 30% pyrite at 29.47m 2 cm multiphase, disrupted quarts SO%/calcite20% vein at 30” 29.16-30.27m fme clast breccia zone, upper contact approximately 55”) at 31.06 m 0.5 cm bandedquartz vein at 30” Samale 58352 = 29.16 to L3llOm 30.27-33.48m 10% fine clast breccia between large clasts 31.7531.85m 10% quartz mending breccia Samole 58353 = 31.10 to 33.48m 33.48-40.4Om large clast breccia, 50% Type 1 and 50% Type 2 andesite most of rock is altered to light green, moderatechlorite/calcite alteration, plagioclase phenocrystsare altered to light green minerals and augite phenoctystsare altered to dark green minerals 33.48-35.OOm very few fme calcite/quarts veinlets, 2-3%, blebs with 70% hematite and 30% residual pyrite at 34.19m 3 mm bandedquarts SO%/calcite50% veinlet at 35” at 34.34m 1 cm bandedquarts .5O%/calcite50% vein at 20” Sample 58354 = 33.48 to 35.OOm 35.00-38.40m l-2% blebs of hematite 70% and residual pyrite 30% at 35.28m 2 cm multiphase, brecciatedquartz 50%/calcite 50% vein bf at 35.70 m 8cm (ttue thickness)banded quartz 9O%/calcite 10% vein at 40” at 36.25m 1 cm bandedquartz vein at 37.02 and 37.08m two 1.5 cm bandedquarts 50%/calcite 50% veins at 60 & 50” G-02 w Page 4 at 38.2Om 2 cm multiphase, disruptedquartz 50%/calcite 50% vein Sam& 58355 = 35.00 to 38.40m 38.40-39.10m only trace of hematite and pyrite 38.49-38.62m breccia zone mended with 10% multiphase veinlets calcite 90%/quartz 10% 39.32-39.37m breccia zone mended with 50% multiphase veinlets quartz 50%/calcite 50% at 39.75m l-2 cm multiphase quartz 50%/calcite 50% vein, lower contact at 40’ 40.40-47.50m mixed large clast (5-15 cm) breccia predominantly Type 2, but 20% Type 1 andesite 40.40-42.30m moderatechlorite/calcite alteration 40.40-41.80m very broken core, 90% recovery at 40.80m 2 cm multiphase quartz 50/calcite 50% vein, disrupted at 40.88m 1 cm multiphase quartz 50%/calcite 50% vein, at 50” 41.20-41.35m 5% quartz/calciteveinlets, very disrupted,2% hematite/pyrite blebs at 41.54m 0.5 cm bandedquartz veinlet with calcite core at 80” 4 1H-4 1.74m 12 cm late breccia zone mended with 30% quartz veins to 2 cm, 2% pyrite 42.30-46.15m moderatechlorite/calcite alteration except for larger cl&s which are only slightly altered, trace to 1% calcite veinlets 0.2 to 4 mm. 42.71-42.78m 7 cm late breccia zone with 10% multiphase quartz 50%/calcite 50% mending breccia 46.15-47.23m late breccia, 0.5-3 cm clasts with gougy matrix which is strongly chlorite/ calcite altered, soft black chlorite(?) mending some of breccia 47.23-47.50m black chlorite(?) replacing groundmassminerals 47.50-54.50m mixed large clast breccia of several types of andesite w 47.50-48.75m non-typical fine grained white and black (salt and pepper)andesite 48.32-48.41m well silicified with 5% micro veinlets mending fractures 48.41-48.75m 5% highly disrupted quartz veinlets filling fractures 48.75-49.00m 5% pyrite blebs 48.75-54.50m large cast breccia of the more typical types of andesiteseen earlier in hole 48.75-49.OOm 2% quartz/calcite veinlets, 0.2-2 mm, disrupted 49.33-49.40m 5% quartz/calcite veinlets, 0.2-2 mm, disrupted 49.46-54.40m l-2% quartz/calcite veinlets, 0.2-2 mm, disrupted,some clasts of 5-10 cm 51.00-51.05,51.37-51.52 and at 51.80m banding at 7O”in fme grain filling between clasts 52.70-52.9Om 5 % calcite veinlets, disrupted 53.55-53.6Om 5 cm zone with 10% calcite veinlets highly disrupted. 54.50-61.61.52m mixed large clast breccia of predominantly Type 1 andesitegenerally only slight chlorite/calcite alteration at 54.62m 0.5cm quaa 50%/calcite 50% vein at 40” at 54.72m OScm quartz 50%/calcite 50% vein with a trace of fluorite at 50” 55.55-57.23m more disrupted than above 10% calcite 90%/quartz 10” veins most occur as blebs on edge of core (fillings betweenclasts?) at 55.55m 1 cm calcite 90%/quartz 10% vein at 40”) late disruption at 55.6Om 2 cm calcite 9O%/quartz10% vein at 20”, late disruption at 56.30-56.90m late breccia zone 56.37-56.65m 5% red hematite (after pyrite?) occurring as irregular smears (fillings between clasts?) 57.23~58.95m same large clast breccia as above, but only a trace to 1% calcite/quartz veinlets w of 0.1 to 1 mm, green, moderatechlorite/calcite alteration G-02 Page 5
58.30-58.40111 10 cm fracture zone mended with 10% multiphase quartz SO%/calcite50% veinlets at 58.85m 3 cm bandedcalcite vein at 60” 58.95-61.05m late breccia zone with 1-1Ocmclasts, 1% fine quartz/calcite veinlets 60.42~60.53m 10 cm banded,multiphase calcite 70%/quartz30% vein at 60” Sam& 58356 = 58.95 to 61.05m 60.53-61.32m strong chlorite/calcite alteration, soft, almost gouge, only 10% recognizable ande&e clasts 61.52-68.57m late breccia and highly shearedzone, dark olive green to grey, strong chlorite/calcite alteration, very soft, only a few of the larger clasts (5-10 cm) are unaltered and recognisableas Type 1 andesite at 61.70m 5 cm breccia zone on side of core with 50% calcite mending at 61.85m shearingat 40” at 61.95m 1.3 cm calcite vein highly disrupted 62.27-62.35m grey replacementzone 70% calcite/30% quartz at 63.30m shearingat 20” at 64.OOm shearingat 35” 65.54-65.71m brown moderately silicified zonesat 55” 66.04-68.57m small clast (O.l-lcm) late breccia zone, some clasts to 5 cm, most clasts in place, not much movement 68.57-90.53m mixed large clast (S-30 cm) bteccia of predominantly Type 1 andesite,zones of late fme clast breccia, strong chlorite/calcite alteration of fine breccia zones 68.87-69.20m fme clast (0. l- 1 cm) late breccia 69.20-70.78m large clasts, 2-3% calcite 90%/quartz lo%, l-10 mm, veinlets, highly disrupted 70.40-70.46m late breccia zone 70.78-72.75m late, fme clast breccia, 2% fine veinlets as above 72.75-73.78m large clasts, well fractured by late fracturing, 2% fine veinlets as above 73.78-74.18m late, fme clast breccia, 2% fine veinlets as above 74.18-74.90m large clasts well frachned by late fracturing, 2% fiie veinlets as above 74.90-76.80 m late, fine clast breccia, 2% fme veinlets as above, lower contact of fme breccia zone at 30” (all of the fine breccia zones are soft) 76.80-82.74m large clast breccia, dark grey to green, moderatechlorite/calcite alteration, 1% calcite/quartzveinlets, 0.2-S mm, disrupted 79.15-81.38m 10% chloritic, fine clast late breccia zone, upper contact at 35” 81.38-81.9Om late fine clast breccia, purple with hematite 8 1.90-82.74m large clasts, interval stained brick red with hematite at 81.90m contact at 75” 82.10-82.70m 1% calcite/quartz veinlets, O.l-2mm, highly disrupted 82.74-89.74m same large clast breccia with predominantly Type 1 andesite,generally slight chlorite alteration, 1% calcite/quartz veinlets, 0.2-3mm, most are highly disrupted at 85.66m 1 cm calcite/quartz vein at 85” 87.15-87.34m 10% quartz 9O%/calcite 10% veins to 1 cm, high disrupted 88.65-88.88m 10% of rock equals quartz 90%/calcite 10% mending small breccia zone at 89.10m 1 cm quartz 7O%/calcite30% vein at 15”) disrupted t 89.47-89.61m 10% quartz/calcite veinlets at 89.53m 1.5 cm quartz/calcitevein at 60” GO2 Page 6
Samole 58357 = 87.15-89.70m 89.74-90.53m same large clast breccia with predominantly Type 1 andesiteclasts, light green with slight to moderatechlorite/calcite alteration 89.74-89.8Sm 10% quartz/calcite veins, highly disrupted 90.05-90.10m 5 cm late breccia zone, mendedwith 30% quartz 70%/calcite 30% veins 90.30-90.40m 10 cm late breccia zone with 20% quartz 90%/calcite 10% veins 90.53m end of drill hole G-02 Simificant Values Obtained from SelectedDrill Core Iutervals of D.D.H. GO2
Wuple Interval Silver Gold Arsenic Antimony Molybdenum Mercury Thallium Sulphur Number (in metres) mm ti mm.-. ~llm wm mm-x- pm 56
58341 8.68-10.00 = 1.32m 2.8 61.1 286.5 4.8 0.68 58342 10.00-10.08 = 0.08m 18.9 889.9 1034.1 84.7 315.2 0.11 20.5 3.45 58343 10.08-12.16 = 2.08m 14.0 309.6 3.0 0.62 58344 18.30-19.56 = 1.26m 6.7 184.8 2.8 7.7 0.43 58345 19.56-21.65 = 2.09m 28.0 218.5 2.7 0.54 58346 21.65-23.20 = 1.55m 2.6 54.9 307.9 5.1 160.5 0.5 1.1 0.50 58347 23.20-24.20 = l.OOm 1.1 56.6 338.3 3.9 0.49 58348 24.20-26.52 = 2.32m 4.5 206.1 399.9 9.0 217.3 0.7 1.7 0.74 58350 26.52-27.46 = 0.94m 6.9 312.4 553.5 18.2 343.1 0.9 3.5 1.15 58351 27.46-29.16 = 1.7Om 63.0 398.9 6.2 87.5 0.6 1.1 0.96 58352 29.16-31.10 = 1.94m 125.4 89.0 2.1 6.0 58353 31.10-33.48 = 2.38m 29.9 72.9 1.4 13.6 58354 33.48-35.00 = 1.52m 146.2 61.6 1.3 58355 35.00-38.40 = 3.4Om 29.6
Please see the drill logs for a complete description of the samples.
Please also see Appendix D for the values obtained for all 35 elements that were analyzed. w DRILL HOLE D.D.H. GO3 k DOUBLESTAR RESOURCESLTD - GOLDEN RAINBOW CLAIM GROUP- DIAMOND DRILL RECORD
DRILL HOLE: D.D.H. GO3 SECTION: 3+30SE PAGE 1 of 9 PROPERTY LOCATION: 20 km southeastof OkanaganFalls, B.C. DRILL HOLE LOCATION: 251 m south and 398 m west of the L.C.P. of the Gold 1 Mineral Claim PROPERTY GRID: 10+21N, 3+30SE AZIMUTH: 225” DIP: -60” LENGTH: 222.59m DRILL TYPE: Longyear 38 CORE DIAMETER: BQWL DIP TESTS: none ELEVATION: 1437m DATE STARTED: October 16,202 DATE COMPLETED: October 21,2002 LOGGED BY: M.S. Morrisq!~ DRILLING CONTRACTOR: BeaupreDiamond Drilling Ltd., Princeton,B.C. /+A-- COMMENTS: 1. Casing to 6.71m; removed from drill hole at the completion of the job. 2. Core recoveriesare 100% unless otherwise recorded
DESCRIPTION: 0.00-O.1Sm drill collar O.lS-6.71m casing 6.71-139.72m EARLY EOCENE MARRON FORMATION
All of the Marron Formation encounteredin the drill hole is a talus breccia comprised of a mix of andesite clasts of which three types are predominant. Type 1 is a porphyritic plagioclaseandesite, Type 2 is a porphyritic plagioclase/augiteandeshe and Type 3 is a porphyritic au&e andesite. (These andesitesare more fully describedwith the log of D.D.H. G-01.)
The talus brecciasare well indurated and they contain very little interstitial material. Early tight fractures are Y mended with l-3% calcite veinlets, O.l-3mm, most of which are highly disrupted. All of the talus breccias have been subjectedto late tectonic movement and several tectonic breccia zones ranging from a few centimetres to a few metres are seen in the core. Only some of the breccia zonesare mended with calcite/quartz veinlets or silica
The andesitesexhibit several degreesof chlorite and calcite alteration ranging from slight to intense. The mote fractured rock is generally the most altered and some of the fmer later breccia zones are highly altered.
The andesitesare also cut by later banded calcite/quartzveins of a few centimetresin width. Pyrite occurs in trace amounts throughout the rock, but there is a notable increasein pyrite near the calcite/quartzveins. It is thought that the blebs of hematite which occur in some of the andesitesrepresent oxidized pyrite.
The talus brecciashave been separatedfrom one anotherin the log that follows basedon which andesitic clasts are the most predominant,Type 1, Type 2 or Type 3.
Special featuressuch as veins, veinlets, tectonic breccia zones,silica replacementzones and mineralisation (pyrite and hematite) are also recordedin the log that follows.
Can’t GO3 w Page 2 6.71-139.72m Large Clad Talus Breccia 6.71-13.57m mixed large clasts (1.5-30cm) of predominantly Type 2 andesite,some chlorite/talc ite alteration of the groundmassminerals, less than 1% calcite/ quartz veinlets (excluding the large veins), l/4% very fine-grained disseminatedpyrite of which much is weatheredto red hematite. 6.71-8.70m limonite on fractures to 8.70m then fresh at 8.23m 4 mm calcite/quartzveinlet, disrupted 8.77~8.88m small silicified breccia zone mended with calcite/quartzveinlets 9.40-12.73m late chalky white bandedquartz 90%/calcite 10% veins 9.43-9.70m 9.5 cm late quartz 90%/calcite 10% vein at 25” Sample 58456 = 9.40-11.20m at 11.20m 2.5 cm vein, lower contact at 23” at 12.5Om 3 mm vein at 35’ at 12.73m 3 mm vein quartz 5O%/calcite50% at 25” 13.57-41.39m mixed large clasts (15-30 cm) of predominantly Type 1 andesite,light to moderatechlorite/calcite alteration of the groundmassminerals, 1% or less calcite/quartz veinlets highly disrupted 13.57-20.27m trace of very fine-grained disseminatedpyrite at 14.95m 5 mm bandedquartz vein at 20” at 15.5Om 2 mm quartz vein with 50% pyrite at 60” 15.80-16.20m light green with moderatechlorite/calcite alteration at 17.39m 3 mm qua*/pyrite vein at 45” at 17.6Om 3 mm quartz/pyrite vein 18.50-18.80m 5% pyrite filling late fractures at 10 to 15” 20.27-27.15m 1% brick red or purple hematite blebs (after pyrite) some zones with l/2% pyrite still unweathered at 21.75m 1.5 cm calcite 9O%/quartz10% vein at 15” 23.47-24.42m breccia zone, 0.1 to 1 cm clasts at 26.15m 5 cm (true thickness) multiphase bandedcalcite vein at 35” at 26.3 lm 2 cm (true thickness) multiphase banded calcite vein at 25” at 26.40m 0.5 cm (true thickness) multiphase bandedcalcite vein at 15” 27.15-29.35m several light green zones with moderatechlorite/calcite alteration 28.10-28SOm 2 to 15 mm calcite 9O%/quartz10% vein with 10% pyrite at 5” 28.77-28.80m 3 cm grey silicified zone at 65’ Sample 58457 = Z&10-28.80m 29.35-31.20m dark green chloritic; l-2% calcite/quartz.veinlets 0.2-3mm highly disrupted 31.20-34.17m 3% calcite/quartz veinlets 0.1 to 5 mm, many semi-parallel core axis, most highly disrupted, trace of very fine grain disseminatedpyrite throughout,but some 1 cm blebs near veinlets at 31.60m 4 mm calcite/quartz veinlet at 20” at 31.80m 4 mm calcite/quartz veinlet at lo”, pyrite adjacentvein 31.80-34.17m fine breccia with 0.1 to 1 cm clasts, good chlorite/calcite alteration 34.17-41.39m moderateto strong chlorite/calcite alteration, trace to 1% calcite/quartz veinlets 0.2 to 3 mm, disrupted; trace of very fme-grained pyrite, most associatedwith late veinlets at 36.30m 2 cm calcite 7O%/quartz30% multiphase vein with quartz core, lower contact at 30” 38.51-38.73m dark green with chlorite alteration G-03 Page 3
38.13-39.27m brecciatedzone 39.27-41.39m highly disrupted, moderateto strong chlorite/calcite alteration at 39.5lm 5 mm quartz/black chlorite veinlet, trace of pyrite, highly disrupted 39.55-41.39m 3% rusty orange and red hematitic zones (representingweathered pyrite?) now just a trace of pyrite, coloured zones are very disrupted 39.95-40.05m 10 cm zone, 10% black chlorite with quarts, also 1% pyrite SamDIe 58458 = 39.55-41.39m 40.05-40.63m brecciatedzone, 0.1 to 2 cm clasts 41.39-45.20m mixed large clasts (15-3Ocm)of predominantly Type 2 andesite,grey, green and light green,highly disrupted,moderate to strong chlorite/calcite alteration; 1% calcite/quartzveinlets, 0.2 to 3 mm, most are highly disrupted, 2-5% red hematite (weatheredpyrite?), zones are highly disrupted, trace of remnant pyrite with most zones 41.9442.21m 5% hematitic zones 42.96-43.04m black chlorite/quattz/hematte zone, disrupted upper contact at 30” 44.96-45.20m 5% hematitic zones with a trace of remnant pyrite Sample 58459 = 41.39-45.20m 45.20-55.44m mixed large clasts (15-30 cm) of predominantly Type 2 andesite,darker green, moderateto strong chlorite/calcite alteration; 1% calcite/quartzveinlets, 0.2 to 1 INU, diSrUpted 46.52-48.37m highly brecciated,0.1 to 1 cm clasts strong chlorite/talcite alteration 48.37-49.OOm green,brecciatcd, moderatechlorite/calcite alteration, 1% red hematitic zones to 1 cm 49.00-51.25m 5% red and purple hematitic blebs, could be weatheredpyrite 49.50-49.90mand 50.70-50.85m brecciatedzones 5 1.25-55.OOm much fewer hematite blebs than above, less than 1% 51.75-52.OOmand 53.15-53.30m brecciatedzones at 53.96m 3 mm calcite/quarts veinlet at 35” at 55.05m 2 mm calcite/quarts veinlet at 60” .55.44-62.55m large clast breccia of predominantly Type 3 andesite,much (80%) is re- brecciatedto finer clasts, moderateto strong chlorite/calcite alteration; alteration is strongestin finer breccia, 1 to 2% calcite/quarts vein& throughout 62.55-69.51m large clast breccia of predominantly Type 2 andesite,many zones of finer breccia. moderatechlorite/calcite alteration, 1% calcite90%/quattz lo%, 0.1 to 3 mm, highly disrupted veinlets 62.55-63.53m late brecciatedzone, coarse 64.fKM4.18, 64.40-64.46,64.70-64.80, 65.15-65.25 & 65.55-65.87m several small brecciatedzones at 65.65m banding at 80’ 68.00-68.15m broken core 68.50-69.37m brecciatedzone upper contact at 60”, lower contact at 30” 69.51-83.69m green to grey augite andesite,Type 3, could be a coarseclast breccia, several late breccia zones with moderatechlorite/calcite alteration, augite phenocrysts are altered to a light green mineral, 2% calcite/quarts,0.1 to 10 mm, highly w disrupted veinlets, only a trace of pyrite 69.51-69.81,70.48-70.64, 71.14-73.58 & 74.95-75.55m late breccia zones at 73.59m 1 cm late calcite 9O%/quartz 10% vein at 40” G-03 Page 4
at 75.65m 1.5 cm late calcite 9O%/quartz10% vein at 40” 76.22-76.41m clast of Type 1 andesite at 78.80 and 78.98m 1 cm bandedquarts 90%/calcite 10% veins at 30” and 45” at 79.87m 1 cm quartz vein at 60” 79.87-80.95m lam brecciatedzone 80.95-81.3lm purple fine gram shear zone, banding at 60 to 65” 81.31-81.54m andesiteis less altered 81.54-83.69m brecciated,moderately chlorite/calcite altered 81.70-81.75m 1.5 cm highly disrupted quarts vein with a black chlotitic rim less than 1 mm 82.40-82.52m soft, clayey, banding at 60” 82.52-83.69m well brecciated 83.69-97.75m mixed large clast breccia (15-30 cm clasts) of predominantly Type 2 andesite, moderatechlorite/calcite alteration, 1% calcite/quartzveinlets, 0.1-2 mm, highly disrupted, 2-5% red and orange hematite blebs with residual pyrite less than 1% Samule 58460 = 83.69 to 84.95m at 83.75m banding at 60” 88.95-89.05m small brecciatedzone 89.3590.67m some clasts to 50 cm, 2% red hematit.eblebs 91.80-93.57m 2% calcite/quartz veinlets 91.80-93.57m less altered, less than 1% veinlets 94.75-95.6om brecciated zone, strong chlorite/calcite alteration, 0.25% very fine-granted v diiminated pyrite, tmce of veinlets 95.60-97.75m less altered 96.62-96.87m late breccia zone 97.75104.90m mixed large clast breccia (15-30 cm cl&s) of predominantly Type 2 andesite, mixed textures, 1% calcite/quartz veinlets, 0.1-4 mm, most are highly disrupted, 2% red hematite blebs 97.75-100.15m less altered 100.15-104.25m more altered and disrupted 104.41-100.46m 5 cm zone of silica replacementon side of core, trace of very fine-granted PYrhe at 101.85m banding at 60 to 70” 104.25-104.90m less altered 104.90-119.30m mixed large clast breccia Type 1, 2 & 3 andesitesand other andesites;light to moderatechlorite/calcite alteration; 1% calcite/quartz veinlets, 0.1 to 10 mm highly disrupted, rare pyrite. at 112.80m late 0.5 cm fracture zone with 2% calcite/quarts mendmg at 114.OOm late 1 cm fracture zone with 10% calcite/quartz mending at 116.88m late 2 cm fracture zone mended with calcite/quartz at 118.25m late 5 cm fracture zone mended with 30% calcite/quartzveining at 119.05m late 5 cm fracture zone mended with 30% calcite/quartzveining 119.30-126.57m mixed large clast breccia (10-15 cm clasts) predominantly Type 1 andesite, light alteration except in disrupted zones,strong to moderatesilica replacement from 122.50-126.57m b at 119.55m 5 cm disrupted zone with 1 cm calcite/quarts vein at 50” at 121.05m 1 cm calcite/quartzvein at 80” 119.30-121.30m 2% calcite/quarts veinlets, 0.1 to 4 mm, disrupted G-03 Page 5
121.30-122.05m highly fractured with 5% calcite/quartz veinlets, 0.1 to 15 mm 122.05-122.5Om light green, highly brecciated,soft, some gouge,strong chlorite/calcite alteration 122.50-123.OOm light grey, 90% silica and 10% grey clay replacement,brecciated and remendedwith silica, 4% pyrite, upper contact at 65” Sam& 58374 = 122.50-123.OOm 123.00-125.3Om light grey, 80% silica and 20% grey clay replacement,highly disrupted, 0.5% diiminated pyrite SamDIe 58375 = 123.~125.30m 125.30-126.57m silica replacementdecreases down hole from 80% to 30%, highly disrupted, 0.5% very fine disseminatedpyrite at 126.3Om banding at 60” Samole 58376 = 125.30-126.57m 126.57-133.85m mixed large clast breccia, several types of andesite,but predominantly Type 2; light to moderatechlorite/calcite alteration 126.57-127.53m well altered highly disrupted, brecciatedand sheared at 127.28m blebs of pyrite to 1 cm 127.31-127.53m banding (shearing)at 70 to 80” 127.53-128.3Om lest; altered 128.30-130.7Om moderately altered, highly disrupted 128.40-128.60m 10% quartz veinlets at 5 to 15”, but highly dismpted, 0.2 mm black chlorite adjacent veinlets cv 129.02-129.10m 8 cm zone of light grey silica replacedbreccia 129.S130.70m brecciated at 130.5Om banding (shearing)at 60 to 70” 130.70-131.97m brick red, hematitic, minor green zones,highly disrupted and banded (sheared), 1% calcite/quartz veinlets, 0.1 to 3 mm, highly disrupted at 131.30m banding at 50” at 131.97m banding at 75”, 3 mm shear plane 131.97-132.30m highly fractured 132.06-132.22m 10% calcite/quartz veinlets, 0.1-3 mm, mending fractures 132.22-133.85m highly disrupted, moderatechlorite/calcite alteration, 1% calcite/quartz veinlets, O.l-2mm disrupted 133.85-136.50m mixed large clast breccia, mixed andesites,but predominantly Type 2 & 3 andesites 133.85-134.16m well chlorite/calcite altered, highly disrupted and brecciated 133.88-134.05m 20% grey highly silicified c&s in late brecciatedzone 134.05-134.16m chloritic, gougy, lower contact at 25” 134.16-135.OOm moderatechlorite/chlorite alteration, moderately disrupted 135.00-135.53m green chloritic and red her&tic, highly disrupted,upper and lower contacts at 70” 135.53-13650m moderately disrupted, 1% disrupted calcite/quartz veinlets, O. l-2mm at 136.75m banding at 65” 135.00-136.OOm 92% core recovery 136.50-139.72m mixed large clast breccia, predominantly Type 1 andesite t 136.50-137.10m trace of veinlets 137.10-139.10m rock gets more disrupted and altered down hole, 3% calcite/quartz veinlets, 0.1-3 mm, most disrupted GO3 w Page 6 at 138.66m 1.5 cm calcite/quartz vein at 50”) disrupted 139.10-139.40m very chloritic, highly disrupted,upper contact at 85” at 139.31m 3 cm bleb of hematite and quartz on side of core at 139.72m contact with porphyritic felsic intrusive at 55” 139.72-202.37m Porphvritic Rhvodacite Sill Very homogeneous,porphyritic rhyodacite with 20% rounded pink or orange orthoclasephenocrysts, 2 to 5 mm, and 3% fine-grained mafics in a very fme- grained groundmass,slight to moderatechlorite alteration (alteration is most intense where the rock is well fractured) weak hematite colours the intrusive pink locally , l-2% micro calcite/quartzveinlets 0.1-l mm, most are highly disrupted, late calcite/quartzveins and pyrite are rare. Special features within the sill are listed below. Sample 58461 = 139.80-141.19m 141,19-148.44m common veinlet anitudesat 30, 60 & 80” at 142.59m 1 cm gouge zone at 45” at 144.83m 2 cm gouge zone at 70’ 148.44-155.70m common veinlet altitudes at 45, 60, 70 & SO”, joints at 15, 35, 45” 154.00-155.70m well fractured, weatheringin fractures, calcite veinlets are 50% weatheredout at 155.24m and 155.27m 2 cm & O&m gouge zones at 60” 155.70-162.96m same rhyodacite as above, late veinlets at 50, 45 & 35”, some disrupted veinlets at 50 to lo’, trace of very fine-grainedpyrite in narrow gouge zones 155.80-156.33m well fractured, 30% of calcite veinlets are weatheredout w at 156.32m 1 cm gouge zone at 40” 161.00-162.00 90% core recovery 161.95-162.09m well fractured, 50% of calcite veinlets are weatheredout at 162.46m 3 cm green clay gouge at 60” 162.83-162.9Om 2 cm late brecciatedzone mended with 50% quartz and 50% calcite 162.96-169.77m same rhyodacite as above, late veinlets at 50 & 60” at 165.48m 1 cm late calcite 9O%/quartz10% vein at 70” 163.00-164.10m well fractured, minor gouge on fractures 167.50-168.05m highly brecciatedzones over 1-5 cm 168.00- 168.05m 1.5 cm green gouge zones at 40” Sample 58462 = 168.00 to 168.55m 169.77-176.95m same rhyodacite as above, late veinlets at 40, 50 & 70” at 170.41mand 170.46m joints at 20 & 60” with 0.5 cm fracture zones at 170&m and 170.78m joints at 50 & 60” with 0.5 cm fracture zones at 172.00-172.50m joints at 5 to 20”, broken core, 90% core recovery Sample 58463 = 173.62 to 175.72m 175.72-176.1Om late breccia zone 176.10-176.95m well fractured (recent) 176.95-183.79m same rhyodacite as above, late veinlets at 70 to 80” at 177.40-177.75m,178.76-179.2Om and 179X0-180.02m well fractured and mended with very fme veinlets at 178.76m 0.5 cm chlorite/calcite gouge at 75” at 179.44m 0.5 cm chlorite/calcite gouge at 35” b 180.16-180.55m 2 to 15 mm light greencalcitic gouge at 70” at 181.33 1 cm calcite veinlet with trace of fluorite at 45” at 182.24-182.30m late well fractured zone at 183.70m 2 cm well brecciatedzone at 20” GO3 Page 7 L 183.64-183.72m 5% calcite mending brecciatedzone Samole 58464 = 181.33 to 183.79m 183.79-190.86m same rhyodacite as above, common joints at 25, 35, 55 & 60” 183.79-183.90m 5% calcite filling fractures 184.40-184.50m 2% calcite filling fractures at 184.7lm and 184.83m small fractured zonesmended with micro veinlets at 185.56m 0.5 cm calcite veinlet at 40” at 186.9Omand 187.71m light green gougetilliig joints at 70” 189.05-189.27m light green gouge between micro breccia zones at 190.38m and 190.56m 0.5 cm calcite veinlets and green gouge at 50” at 190.78m 1 cm light green gouge at 45” Sample 58465 = 189.00to 190.86m limo&e on fractures (after pyrite?) 190.86-197.9Om same rhyodacite as above, common joints at 25, 35, 50, 60 & 70” at 192.OOmand 192.22m 1 cm green gouge and calcite in joints at 50” Samale 58466 = 190.86 to 192.70m limo&e on fractures (after pyrite?) at 193.50m 1 cm calcite and green gouge filling joint at 50” at 194.23m 1.5 cm calcite and green gouge filling joint at 50” SamDIe 58467 = 192.70 to 195.30m trace of limo&e on fractures at 196.72m two, 1 cm gouge zones filliig fractures at 197.45m 1 cm fractured zone with green gouge at 35” at 197Slm 3 cm well fractured zone Samole 58468 = 195.30 to 19790m many tight fractures with limonitefiematite staining (after v pyrite?) 197.90-202.37m same rhyodacite as above 198.40-202.37m rock gets darker grey or green towards the fault 202.37-222.59m Fort Knox Basement Fault Zone 202.37.210.66m EARLY EOCENE MARRON FORMATION 202.37-210.66m Large Clast Talus Breccia Predominantly Type 1 andesitic clasts? The rock is highly disrupted and altered in the fault zone, and only an occasionalType 1 clast can be recognized. 202.37m top of fault zone, upper contact at 80” 202.37-202.54m gouge zone with grey clay and rock chips 202.54-204.28m green (chloritic) and black (chloritic) highly disrupted, brecciated,mended, brecciatedand mended (was andesiteporphyry?) 5% pyrite blebs, streaks and fillings betweenclasts at 202.82m shearingat 50 & 60” Samole 58469 = 202.37 to 204.2Sm very chloritic, 5% pyrite 204.28-204.84m much less disrupted at 204.66m 1 cm calcite with pyrite filling joint at 60” 204.84-205.35m only moderately altered Type 1 andesite at 205.22m 2 mm band of pyrite at 50” 205.35-206.13m highly disrupted zone, brecciated,mended, re-brecciatedgreen and grey chloritic, 2% pyrite, l-2 cm gouge along fractures at various angles, lower contact at 70” L 205.81-205.88m 7 cm brecciatedzone mended with 20% quartz, 10% calcite and 10% pyrite 206.13-206.72m well disrupted andesite,good cbloritic alteration, 5% quartz in circular blebs, 2-10 mm, with minor pyrite GO3 Page 8
at 206.6Om 1 cm quartz vein with 50% pyrite at 40” 206.42-206.72m 5% pyrite, some associatedwith quartz blebs Sam& 58470 = 204.28 to 206.72m 206.72-210.66m highly disrupted,brecciated, mended and brecciatedandesite porphyry, good chlorite alternation, 5% quarts 50%/calcite 50% veinlets and blebs, highly disrupted, pyrite l-3% at 207.1Om 2 cm vein, at 207.18m 2.5 cm vein, at 207.22m 2 cm vein, at 207.34m 2 cm vein and at 207.57m 1 cm vein all veins are multiphase,banded quartz 50%/calcite 40% with 5 to 10% pyrite on outer edges,all are highly disrupted by late brecciation at 208.40m 3 cm multiphase vein quartz SO%/calcite40%/pyrite 5% at 209.OOm shearing at 60 to 70” 206.72-208.40m 2% pyrite 208.40-21O.OOm 3% pyrite usually associatedwith quartz veins and blebs Samale 58471 = 206.72 to 210.OOm 210.66-222.59m Pm-Permian Monashee Gneiss 210.66-211.85m green highly disrupted (gneiss?),brecciated and mended several times, 30% green and black chlorite replacementand 20% quarts replacement,late 1 mm calcite veinlets at 70” 211.85-218.89m small zonesof relatively fresh gneiss between zones of highly disrupted and replacedgneiss 211.85-212.45m highly disrupted, white, pink and green from 212.09-212.40m70% white and pink silica replacement,elsewhere 10% silica and 20% chlorite replacement Samole 58472 = 210.66 to 212.45m 212.45-212.80m much less disrupted and altered black gneiss, S % quarts replacement,5% chlorite filling fractures .l-lmm 212.80-213.24m highly disrupted,brecciated and mended several times, 10% quarts and 10% green chlorite replacement 213.24-214.30m highly disrupted,pink, white and green with 20% quartz and 5% epidote and chlorite replacement,many cycles of brecciation and mending, but 20% relatively unalteredgneiss within zone, lower contact at 45”; 1 cm late brecciatedzones at 80” 214.30-215.67m moderately disrupted unaltered gneiss includes some disrupted zonesover a few centimetres;5% disrupted quartz replacementzones, 3% chlorite filling fractures and joints at 50 & 70”; lower contact at 45” 215.67-218.33m black gneiss with 20% small zones of highly disrupted and replaced rock 215.67-216.08m 10% quartz and 10% chlorite replacement 217.21-217.31m 10 cm zone with 80% quartz and 20% chlorite replacementat 70 to 75” 217.70-217.9Om three l-3 cm pegmatitedykes at 80” 217.23-217.80m 50% quartz and 30% chlorite replacement 217.80-218.33m highly fractured gneiss, 10% chlorite mending fractures 218.89-219.42m 95% highly disrupted gneiss, brecciatedand mended several times, 80% silica and 10% chlorite replacement,trace of very fine-grained pyrite, very tight late fractures throughout Samole 58473 = 218.33 to 219.42m u 219.42-221.21m highly fractured and disrupted gneiss, generally 10% quarts and 10% chlorite replacement 220.10-220.2Om 10 cm zone at 60” with 70% quartz and 30% chlorite replacement G-03 Page 9
221.00-221.21m 40% quartz and 20% chlorite replacement,lower contact at 60” 221.21-222Slm fresh gneiss, but foliation distorted (several attitudes) 222.51-222.59m highly disrupted gneiss, 80% quartz and 20% chlorite replacement,upper contact at 40” (network of very fine late fractures in all of the highly replaced zones noted above) 222.59m end of drill hole G-03
W ‘gaitkant Values Obtained from SelectedDrill Core Intervals of D.D.H. G-03
Sample Iut erId Silver Gold Arsenic Antimony Molybdenum Mercury Thallium Sulphur Number (in metres) am mb mmk ~nm pm mm..- mm %
58456 9.40-11.20 = 1.80111 36.0 58457 28.10-28.80 = 0.7Om 3.1 170.6 993.8 45.1 235.1 0.17 3.5 3.47 58458 39.55-41.39 = 1.84m 1.7 68.0 266.4 4.6 118.7 0.9 0.78 58459 41.39-45.20 = 3.81m 39.6 183.9 3.3 108.0 0.6 0.56 58460 83.69-84.95 = 1.26m 22.2 232.9 2.3 58374 122.50-123.00 = 0.5Om 3.1 94.1 784.8 7.6 28.9 1.59 58375 123.00-125.30 = 2.3Om 1.8 161.7 1651.4 17.9 7.7 1.33 58376 125.30-126.57 = 127m 32.7 498.6 4.7 1.08 58462 168.00-168.55 = 0.55m 16.9 10.0 58469 202.37-204.28 = 1.91m 5.1 787.0 30.6 0.37 5.4 3.59 58470 204.28-206.72 = 2.44m 3.3 381.3 15.1 0.24 2.7 2.28 58471 206.72-210.00 = 3.28m 3.9 917.3 41.8 0.43 8.0 3.55 58472 210.66-212.45 = 1.79m 10.9 58473 218.33-219.42 = 1.09m 15.6
Please see drill logs for a complete description of the samples.
Please also see Appendix D for the values obtained for all 35 elements that were analyzed. L DRILL HOLE D.D.H. G-04 w DOUBLESTAR RESOURCESLTD - GOLDEN RAINROW CLAIM GROUP- DIAMOND DRILL RECORD
DRILL HOLE: D.D.H. GO4 SECTION: 3+OOSE PAGE 1 of 7 PROPERTY LOCATION: 20 km southeastof OkanaganFalls, B.C. DRILL HOLE LOCATION: 100 m south and 274 m west of the L.C.P. of the Gold 1 Mineral Claim PROPERTY GRID: 12+lON, 3+OOSE AZIMUTH: 225” DIP: -70” LENGTH: 84.43m DRILL TYPE: Longyear 38 CORE DIAMETER: BQWL DIP TESTS: none ELEVATION: 1450m DATE STARTED: October 21,2002 DATE COMPLETED: October 23,200Z LOGGED BY: M.S. Morrisoq DRILLING CONTRACTOR: Beaupre Diamond Drilling Ltd., Princeton, B.C. b+L=%v COMMENTS: 1. Casing to 4.27m; removed from drill hole at the completion of the job. 2. Core recoveriesare 100% unless otherwise recorded
DESCRIPTION: O.OO-0.15m drill collar 0.15-4.27m casing in broken rock 4.27-84.43m EARLY EOCENE MARRON FORMATION
All of the Marron Formation encounteredin the drill hole is a talus breccia comprised of a mix of andesite clasts, the majority of which are comprised of Type I porphyritic plagioclaseandesite. (The Type 1 andesite is describedin more detail with the log of D.D.H. G-01.)
The talus breccia is well indurated and it contains very little interstitial material. Early tight fractures are mended with l-3% calcite veinlets, 0.1-3 mm, most of which are highly disrupted. v The talus breccia has been subjectedto considerabletectonic movement and much of it has been broken into finer clasts. Only some of the later breccia zonesare mended with calcite/quartz veinlets or silica.
The andesiteexhibits several degreesof chlorite and calcite alteration ranging from slight to intense. The more fractured rock is generally the most altered and some of the late finer breccia zonesare highly altered.
The andesitesare also cut by severalbanded calcite/quartz veins of a few centimetres in width. Pyrite occurs in trace amounts throughoutthe rock, but there is a notable increasein pyrite near the late calcite/quartz veins. It is thought that the blebs of hematite which occur in some of the andesiterepresent oxidized pyrite
Special featuressuch as veins, veinlets, tectonic breccia zones, silica replacementzones and mineralization (pyrite and hematite) are recordedin the log that follows.
Con’t G-04 Page 2
4.27~84.43m Large Clad Talus Breccia 4.27-25.26m mixed large clasts (S-1.5cm) of predominantly Type 1 andesite,with intervals of fine breccia (l-3 cm clasts), slight to moderate chlorite/calcite alteration with the finer clast brecciasbeing more altered, 1% calcite/quartzveinlets 0.1 to 2 mm, disrupted 4.31-5.85m well fractured 4.79-4.9Om 1.5 cm quartz vein at 15”,bandedclear, white and grey 5.00-6.OOm 95 % core recovery at 5.85m 1 cm calcite vein at 40” 6.15-6.32m 15% calcite 9O%/quartz 10% filliig between c&s at 6.40 m 3 cm late microbreccia zone widi”breccia, late minor calcite menclmg breccia 6.50-6.58m 15% calcite 90%/quartz 10% m&ding breccia at 6.7Om 3 cm bandedquartz 50%/calcite 50% mending breccia Samale 34404 = 4.31 to 6.76m at 7.20m 2 cm calcite vein at 25” 7.90-7.98m 8 cm late breccia zone, 5% calcite SO%/quartz20% menclingbreccia 8.20-8.95m fme breccia, 1 cm clasts, strong chlorite/calcite alteration 8.95-9.35m strong chlorite/calcite alteration 9.35-9.45m recent broken weatheredzone 9.45-10.88m clasts 2 to 10 cm lO.OO-lO.lOm 5% quartz matrix at lO.lOm 1 cm calcite vein at SO” at 10.54m 1 cm calcite vein at 40” 10.54-10.88m 0.5% pyrite Sample 34405 = 10.00 to 10.88m 10X8-18.10m same Type 1 andesitebreccia as above, 0.5 to 10 cm clasts, trace of disseminatedpyrite, usually near veinlets ll.OO-12.OOm 85% core recovery at 12.23m 3 cm (true width) banded calcite vein at 65” 12.45-16.46m 30% green clasts in 70% grey to brown very fme-grained matrix, 1% calcite/quartz veinlets, 0.1-5 mm at 13.42m 3 mm calcite 9O%/quartz10% veinlet at 60” SamDIe 34406 = 13.25 to 13.93m 20% silica replacement 15.00-16.OOm 90% core recovery at 15.80m 5 mm calcite 9O%/qua* 10% vein at 40” 15.82-15.88m soft gouge 15.80-18.1Om 0.25% pyrite disseminated,but most is close to veins 16.46-17.45m large clasts (to 1.5cm), 2% calcite/quartz veinlets, highly disrupted 17.45-18.10m late brecciated zone (2 to 5 cm clasts) 5% calcite/quartz filling betweenclasts Sam& 34407 = 15.97 to lS.lOm l&10-1932m large clast breccia, slight alteration 18.00-19.OOm 90% core recovery 19.32-20.7Om 3 to 5 cm clasts, moderatealteration, 1% calcite/quartz veinlets, disrupted, trace of pyrite associatedwith veining 19.59-19.63m 10% calcite 9O%/quartz10% mending late breccia zone, trace pyrite 19.90-20.OOm 10% calcite 9O%/quartz10% mending late breccia zone, trace pyrite 20.45-20.55m 15% calcite 9O%/quartz10% mending late breccia zone G-04 Page 3
Samole 34408 = 19.32 to 20.70m 20.70-22.17m clasts to 15 cm, slight alteration, trace of disseminatedpyrite, most near veinlets at 21.5Om 0.5 cm calcite 90%/quartz 10% vein at 5”, disrupted 21.80-21.84m 5% calcite 9O%/quartz 10% mending late breccia zone 22.10-22.17m 5 cm (true width) bandedcalcite CO%/quartz40% vein, lower portion of vein is quartz, upper contact at 40”, lower contact at 35” 22.17-22.45m 30% fiie (0.5-2 cm) green and grey clasts set in 70% fiie grain soft grey matrix, moderatechlorite/calcite alteration Samole 34409 = 22.10 to 24.1Sm 22.45-24.18111 clasts up to 15 cm, slight alteration, trace of disseminatedpyrite, most of pyrite is near veining 23.24-23.28m 10% calcite 9O%/quartz10% mending late breccia 23.54-23.57m 10% calcite 9O%/quartz10% mending late breccia 23.86-24.18111 20% calcite 90%/quartz 10% mending late breccia 24.18-24.44m 14 cm (true thickness) brecciated,composite calcite 90%/quartz 10% vein, centre of vein is bandedcalcite/quartz , upper contact 30”) lower contact 20” Sam& 34410 = 24.18 to 24.44m composite vein 24.44-24.90m large cl&s, slight alteration, trace of pyrite 24.90-25.26m 3-10 cm clasts slight alteration, trace of pyrite 25.26-32.25m same large clast (S-15 cm) breccia with predominantly Type 1 andesiteclasts, but some clasts are dark grey to black and the crystal textures are different, moderateto strong chlorite/calcite alteration, 0.5% disseminatedpyrite, most is closely associatedwith veining 25.26-25.84m 15% calcite 90%/quartz 10% mending late breccia 25.84-25.96m 10 cm (tme width) calcite 95%/quartz 5% vein at 60”, late quattz band near centre of vein at 50” at 26.18m 2 cm calcite 95%/qnati 5% vein at 70”, late quartz near centre of vein 25.96-26.30m 10% calcite 95%/quartz 5% mending late breccia Samole 34411 = 25.26 to 26.38m 26.38-28.65m fme clast breccia with minor larger (S-10 cm) clasts, 2% small brick red bematitic clasts, micro veinlets between clasts, strong waxy green chlorite alteration, 0.25% very fme pyrite throughout,locally near veins 1% pyrite at 26.88111 1 cm calcite 95%/quartz5% vein at 40” 27.90-28.20m 10 % calcite 95%/quartz 5% mending late breccia Sam& 34412 = 26.38 to 28.65m 28.65-29.16m mix of large and fine clasts, 1% pyrite 28.80-28.85m grey clay gouge 29.16 - 29.4Sm fine clast late breccia strong chlorite/calcite/clay alteration 29.45-30.80m large clast breccia (some clasts to 5 cm), less than 0.5% pyrite overall, but up to 1% near veining at 30.OOm 1 cm calcite 90%/quartz 10% vein 30.45-30.55m 10% calcite 9O%/quartz10% mending late breccia zone 30.65-30.80111 10% calcite 9O%/quartz10% mending late breccia zone 30.80-31.23m dark grey, slight alteration, trace of pyrite only 31.23-32.25m large clast breccia, highly fractured, S-10% calcite/quartz filling fractures, G-04 Page 4
highly disrupted, and multiphase veining, but only a trace of pyrite, small brecciatedzones over 2-5 cm between larger clasts, strong, waxy chlorite alteration Sam& 34413 = 31.23 to 32.25m 32.2553.47m large clast .breccia,predominantly Type 1 andesiteclasts, but some mixed andesiteclasts, 1% calcite veinlets, 0.1-2 mm, highly disrupted, 0.1% pyrite 32.2532.78m late brecciatedzone with 2-4 cm clasts at 32.43m 2 cm late calcite 9O%/quartz10% vein at 60” with a 3 mm bleb of fluorite 32.78-33.17m fme clast (0.5-1.5 cm) late breccia, matrix of chlorite and clay gouge, 5% calcite clasts (broken veins?) strong chlorite alteration 33.17-34.OOm fine clast breccia as above, but less gouge, strong chlorite alteration 33.62-33.74m l-2 cm zonesof late brecciation, minor gouge 34.00-35.04m large clast (5-15 cm) breccia, moderatechlorite alteration 34.70-34.96m 5% silica mending lam breccia at 35.03m 1 cm calcite 70%/quartz 30% vein at 50” banded,late quartz in centre of vein Sam& 34414 = 34.00 to 35.04m 35.04-39.10m fme clast (0.25-3 cm) breccia, occasional 5-10 cm clasts, moderatechlorite alteration 35.04.35.78m 30% grey and brown very fime matrix minerals mending breccia 35.78-38.01m same as above, more chloritic 36.90-37.15m late chloritic breccia zones 37.50-38.01m late breccia zones,chlorite and clay, almost gouge w at 37.75m 2 cm calcite vein in gouge zone 38.01-39.10m fme clasts (0.5-2 cm) in 30% grey fme-grained matrix 38.15-38.23m 6 cm (true width) banded calcite vein at 40” at 39.10m 3 mm calcite 8O%/fluorite20% vein at 80” 39.10-46.39m large clast breccia which has been re-brecciated,trace to l/4% pyrite, best pyrite with small red hematitic zones,often near veining and late fine brecciatedzones 39.10-39.77m small clasts (0.5-2 cm) some to 5 cm, 5% grey and brown fine-grained matrix at 39.85m 2 cm calcite 90%/quartz 10% zone on side of core 39.77-40.70m late breccia and gouge, strong clay/chlorite alteration, 85% core recovery 40.70-46.39m dark grey to green medium clast (5 cm) breccia with minor fme breccia and late breccia zones,moderate to strong chlorite alteration at 40.80m 1 cm calcite vein at 40”, offset 4 cm by late fracture at 25” 41.01-41.07m late breccia zone 41.25-41.28m 40% calcite mending breccia zone 41.34-41.40m 20% calcite, 5% quarts mending breccia zone 41.87-41.93m 25% calcite 8O%/quarta20% mending breccia zone 42.50-42.55m 50% calcite 95%/quartz 5% mending breccia zone, 5 mm bleb of fluorite at 42.62m 1 cm calcite vein at 65” 42.82-42.9Om calcite 80%/quartz20% mending breccia at 43.08m 1 cm calcite vein at 70 43.14-43.2Om one half of a 4 cm calcite 80%/quartz2O%vein on the side of the core, highly disrupted, 1 cm band of quartz in centre of vein u 43.2543.28m 30% calcite 95%/quarts 5% mending breccia 43.38-43.55m 20% grey/brown very fme grain matrix G-04 w Page 5 Sam& 34415 = 41.24 to 43.56m 44.64-44.68m 20% calcite mending breccia 44.75-44.81m late breccia zone 44.81-45.52m 5% fragments of highly disrupted calcite veins 45.52-45.55m 2.5 cm late calcite vein at 80” at 45.90m 1 cm late calcite vein at 60” 45.94-45.98m 3 cm calcite 7O%/quartz30% disrupted vein 45.98-46.39m 5% highly disrupted calcite veins Sam& 34416 = 43.56 to 46.39m 46.39-S1.60m small clast (1-2 cm) breccia some clasts to 5 cm, 5% calcite mending breccia, 10 to 30% very fme-grained grey/brown matrix minerals, 0.5-l % very fme- grained disseminatedpyrite, strong chlorite alteration at 48.10m 1.5 cm late calcite vein at 30” at 48.6Om 4 cm (true width) calcite vein at 70” Sample 34417 = 46.39 to 49.OOm at 49.70m 1 cm zone of calcite veinlets at 60” 50.05-50.12m quartz 20%/calcite lO%/hematite 3% mending breccia, l-2% pyrite 50.20-50.26m quartz lO%/calcite 2O%/hematite3% mending breccia, l-2% pyrite 50.65-50.73m quartz 20%/calcite lO%/hematite 3% mending breccia, l-2% pyrite all of the pyrite is very fine grained SamDIe 34418 = 49.00 to 51.OOm 51.60-51.78m late fine clast breccia zone, strong chlorite/calcite alteration v 51.78-53.47m coarser clasts (up to 10 cm) 10% very fine-grainedbrown matrix minerals, 0.25-0.5% pyrite disseminated at 51.90m 0.5 cm late calcite 70%/quartz 30% vein at 85”; quartz bands in centre of vein at 52.95m 1 cm late calcite vein at 70” at 53.25m 1 cm broken calcite vein at 60” at 53.35m 0.5 cm calcite vein at 60” SamDIe 34419 - 51.00 to 53.47m 53.47-67.56m mixed large clast (5-15 cm) breccia of predominantly Type 1 andesiteclasts, slight to strong chlorite alteration, several late zones of tectonic brecciation 53.47-55.20m 5 cm clasts among fmer clast (0.1-2 cm) breccia 53.77-55.48m 2% calcite (portions of highly disrupted veins?) at 54.48m 2 cm calcite SS%/quartzlO%/fluorite 5% vein at 80” 54.48-55.20m 10% calcite (portions of highly disrupted veins?) Samole 34420 = 54.48 to 55.20m 55.20-55.38m 80% rock chips 20% clay and chlorite gouge, upper contact 55”, lower contact 45” (opposite) 55.38-55.84m highly disrupted brecciatedzone with 20% vein material, bandedquartz 50%/calcite SO%,2% disseminatedpyrite, strong chlorite alteration 55.52-55.62m 4 cm (true width) bandedquartz/calcite vein, upper contact at 30”) lower contact is highly disrupted 55.72-55.84 5 cm (true width) bandedquartz/calcite vein, upper contact is highly disrupted, lower contact at 30” Samrde 34421 = 55.38 to 55.84m 55.84-58.84m 80% fine clast (0.1 to 2 cm) 20% with 3-5 cm clasts, 3-S% calcite filling u matrix (could be portions of highly disrupted veins?), trace to 0.5% pyrite, strong chlorite alteration G-04 Page 6 Lr at 57.95 and 57.97m two 1 cm late calcite veins at 70” 58.84~60.49m generally large clasts (5-15 cm) separatedby small zonesof small clast (0.1-2 cm) breccia, dark olive green, strong chlorite alteration of finer breccia zones, 3-5% calcite filling matrix (could be portions of highly disrupted veins) 60.49-63.08m generally large clasts (5-10 cm) separatedby small zones of small clasts (O.l- 2cm) breccia, 5% calcite filling matrix (could be broken veins?), 0.5% disseminatedpyrite, strong chloritic alteration SamDIe 34422 = 60.49 to 63.OSm 62.34-62.48m highly disrupted vein (possible 5 cm true width) calcite 9O%/quartz10% 63.08~64.98m highly disrupted fme clast late breccia, 8% calcite filling matrix (could be broken veins?), strong chlorite alterat& 64.62-65.40m 5% silica replacementin matrix of breccia Sample 34423 = 63.08 to 65.40m 64.98-67.56m large clast breccia separatedby 20% small clast breccia zones, moderate chlorite/calcite alteration, 0.25-0.5% disseminatedpyrite, 7% calcite filling matrix (Could be broken veins?) also late veins at 65.80m 1 cm late calcite vein at 45” at 66.43m 1 cm late calcite vein at 40” at 66.55m 0.5 cm late calcite vein at 60” 67.56-74.66m mixed large clast breccia of predominantly Type 1 andesiteclasts, but some mixed types of andesite with different textures, all plagioclase phenocrystsare moderately altered to light green minerals, moderateto strong chlorite/calcite alteration, 0.25% pyrite showing a close associationwith veins 67.56-69.6Om local highly fractured zones, 3% calcite veinlets, 0.1-5 mm, most are highly disrupted 69.60-70.17m brecciated0. l-l cm clasts 70.17-70.65m large Type I andesiteclast 70.65-71.50m fme breccia 0.1-2 cm clasts, 5% calcite matrix 71.50.74SOm large (5-10 cm) Type 1 andesiteclasts, 2% calcite veinlets 0.1-5 mm 71.70-71.73m late breccia zone with 5% calcite matrix at 72.24m 3 cm (tie width) banded, white and clear quartz vein, lower contact at 30” at 72.6Om 4 cm (true width) banded,quartz 6O%/calcite40% vein with calcite in the centre, upper contact at 30”) lower contact at 50” at 72.83m 4.5 cm (true width) banded,quartz SO%/calcite20% vein with calcite in the centre at 30” SamDIe 34424 = 72.24 to 72.93m at 73.14m 1 cm (true width) banded,quartz 50%/calcite 50% vein at 60” at 73.60-73.64m 4 cm gouge zone at 70” 74.66-81.74m dark grey and green large clast breccia of predominantly Type 1 andesite, plagioclasealtered to light green minerals, moderateto strong chlorite/calcite alteration, only a trace of very fine-grained pyrite 74.66-75.00m clasts lo-15 cm 75.00-75.29m small clast zone, 3% calcite veinlets, 0.1-2 mm, with trace of fluorite 75.29-76.95m medium clast breccia, 2-5 cm, some 0.1 cm at 75.38m 0.5 cm calcite vein at 45” at 75.90m 1 cm calcite vein at 60” at 76.68m 0.5 cm calcite 6o%/quartz 40%/fluorite (trace) vein at 60” 76.95-81.74m large cfast breccia with local fine brecciatedzones GO4 Page I
at 77.07m 1 cm calcite vein at 55” 77.79-77.87m 10% calcite/quartz mending small breccia zone at 78.55m 3 cm green clay and rock chips, gouge zone at 30” 78.84-79.06m green siltstone at 60” 79.60-80.10m brecciatedzone, 3% calcite veinlets 0.1-2 mm, highly disrupted 80.47-S1.04m brecciatedzone, 5% calcite tilling matix 81.23-81.74m moderately brecciated,fine and medium clasts 81.74.84.43m dark grey large clast breccia of predominantly Type 1 andesite,much late brecciation to 0.1-3 cm clasts, plagioclasealtered to light green minerals, moderateto strong chkwite/calcite alteration, l-2% calcite veinlets, 0.1-5 mm, most are highly disrupted, trace of very fine-grainedpyrite at 82.72m 0.5 cm late calcite 9O%/quartz10% vein at 40” at 82.88 and 83.02m two 3 mm late calcite 9O%/quartz 10% veins at 45” 84.43m end of drill hole G-04 L Significant Values Obtained from SelectedDrill Core Intervals of D.D.H. G-04 Sample Interval Gold Arsenic Antimony Molybdenum Sulphur Special Number fin metres) lll!!L - PDm DDrn % Features
34404 4.31-6.76 = 2.45m 186.9 129.3 1.9 32.3 0.32 small calcite/quartz veins 34405 10.00-10.88 = 0.88m 13.1 0.47 small calcite veins 34406 13.25-13.93= 0.68m 8.8 20% silica replacement 34407 15.97-18.10= 2.13m 11.1 0.89 minor pyrite 34411 25.26-26.38= 1.12m 345.9 0.48 calcite/quartzveins 34421 55.38-55.84 = 0.46m 408.3 69.5 0.8 0.64 calcite/quartzveins 34422 60.56-63.08 = 2.52m 10.0 62.1 0.74 calcite/quartzveins
Pleasesee the drill hole logs for a completedescription of the samples.
Pleasealso seeAppendix D for the valuesobtained for all 35 elementsthat were analyzed. APPENDIX D
CERTIFICATES OF ANALYSES .I 2.6 10.6 20 .l .I .1 4 .06 .5 c.1 .9 c.1 1 ;I .l G.1 1 .07c.o01 Cl 2.1 co1 2<.001 4 .a1 ,290 .Ol .I s.01 <.I <.I c.Q6 .4 1.9 1.5 2 .I 1.1 .3 759 .lB 3.7 2 190.0‘ .5 2910 r.1 .2 c.1 2 17.59 ,004 4 5.1 .04 L&=.001 2 .05 ,006 .03 1.7 g.01 2 4 .a9 .E L4.E 19.3 46 .I l3.4 8.9 374 2.06 42.7 1.3 2Q.9 L2.3 255 .L .a <.I 27 1.49 .l% 60 33.4 .69 57 .QO2 1 .95 .015 .23 2.0 TO1 2.4 .I .37 14.7 14.3 18.9 42 .I W.6 9.0 r)l 2.40 76.0 2.0 23.4 II.,? 2(18 c.1 1.1 <.I 19. 1.17 ,110 54 35.9 .49 50 .OQ3 1 .69 .QO7 .24 1.E .Ql 2.2 .11.52 2.4 16.0 12.4 49 .l 14.0 8.9 52Q2.33 .58.5 3.1 10.6 14.7 295 .l 1.4 c.1 3, 2.10 ,108 69 34.0 .7Q 46 .Offi cl l.M .Q30 .23 1.3 .Ol 2.1 .L 20 5B306 2.0 15.9 L4.9 41 ,112.G 9.3 700 2151 15.6 3.4 4.9 19.8 3W .l .6 .L 40 2.63 .L13 73 38.7 .X3 57 .OlS Cl .% ,035 .23 Z.Q<.OL 2.2 .l c.05 58306 1.7 16.0 22.9 46 .2 12.3 9.4 4% 2.39 114.4 3.2 13.4 17.8 2% .1 2.4 .L 28 1.64 .117 85 30.1 .65 46 .QOS Cl 1.11 ,033 .26 1.4 .OL 2.1 .2 .44 58307 L7.4 11.6 9.8 32 .5 9.6 6.1 465 1.76 311.0 .B 76.9 8.1 310 <.I 3.5 <.I ~18 3.66 .071 36 24.1 .61 56 .OlQ 4 .7l .OU .I8 3.9 c.01 1.1 .2 .6Q 58x4 .E L3.2 13.3 47 <.I 11.0 7.5 611 2.07 77.4 2.1 8.1 16.3 202 c.1 1.5 c.1 37 2.46 ,112 69 32.4 .6Q 87 .Q44 I 2.3 .a89 .n 1.4 c.01 2.4 .I .I4 53309 .9 14.0 14.9 50 .2 ti.6 8.9 510 2.56 708.9 1.7 64.7 11.9 222 .I 7.9 <.I 26 1.77 .lLL 63 26,9 .a2 66 .ol5 11.16 .057 .29 1.7 .Q3 1.9 .3 .75
6e310 .7 11.3 14.1 43 z.1 1l.E 7.3 61Q2.09 5.3 2.3 4.7 17.1 l87 .l .4 c.1 32 2.28 ,106 76 34.8 .b6 112 ,057 2 .GL ,069 .26 1.6 '.OL 1.9 .I co5 68311 2.5 13.6 21.2 50 .2 14.7 9.0 447 2.06 242.5 2.7 10.3 17.4 147 <.I 3.2 cl 29 1.23 .I21 73 23.0 .63 206 .Q49 2 .59 .QEQ 3 2.5 c.01 2.0 .l .37 58312 1.2 14.1X.9 47 <.I 12.5 9.7 572 2.36 1.6 2.4 3.1 19.5 159 .L .8 s.1 40 2.57 .113 82 33.7 ..90 U7 .!I33 1 1.23 .068 .38 :7 a.01 2.1 .1 c.05 58313 1.6 15.3 14.5 51 .l 14.2 6.8 669 2.23 12.5 3.9 7.6 18.3 614 .2 .4 .I 38 2.50 .112 72 36.0 33 511 326 ~1 1.10 .062 .24 2.3 .Ol 2.1 .1 .W 59314 1.0 9.3 12.4 3-3 .I 9.2 6.1 657 1.63 6.7 24.5 49.5 11.1 3159 .I ~.2 4 2.3 6.07 .c65 46 22.6 x.0 na .a23 2 .81 .a41 .19 2.0 -COI 1.7 <.I .Q3
.9 W.5 16.8 50 c.1 13.6 LO.0 763 2.51 3.0 2.4 2.1 17.6 210 .I .5 cl 46 3.37 ,117 61 34.9 1.01 297 ,033 11.37 ,069 31 1.0 c.01 2.3 .l c.05 1.0 2.9 6.8 13 c.1 7.8 1.7 1366 .96 2.7 1.2 7.4 4.4 476 .2 .2 .3 ,1215.54 ,026 10 15.1 .33 16 ,001 ,cl .45 ,032 .L4 2.6~01 1.0 <.I c.05 1.9 3.6 5.1 17 c.1 4.6 2.8 479 .94 4.1 3.4 I.2 2.9 2x72 .I .I .5 12 4.17 .a49 22 13.4 .36 26 ,003 2 .E ,078 .I9 3.4 q.01 1.5 c.3 co5 1.6 24.6 14.9 36 .l 2.8 3.5 431 1.43 2.3 .5 2.7 2.6 309 2 .I .1 I6 3.12 .Q44 21 9.2 .29 124 .006 ~1 .6l.Q% .2a 1.3 ~01 1.3 .L .Ll 1.6 25.1 14.2 34 .I 2.5 3.7 442 1.45 2.5 .5 1.1 2.9 ,301 .2 .l .I .L6 2.96 .a43 22 3.5 .30 131 .aL% =I SB ,058 .20 1.2 c.01 1.3 .L<.(H
RBE SE318 1.7 26.3 33.2 34 .L 1.9 3.8 442 1.44 2.3 .5 1.E 2.9 247 .l .l .L 15 2.66 .043 2.2 9.7 .3L 126 ,006 ~1. .6Q ,057 .L9 2.5 s.01 1.3 .lc.Q5 58319 5.3 m.2 9.6 34 .l -2.7 3.9 393 1.41 3.4 .6 1.6 2.9 116 .I .I .I 14 2.28 ,045 21 e.9 .23 218 ,007 3 .59 .056 .2l 1.3 c.01 1.3 c.1 .I1 2.2 17.3 7.5 31 <.I 2.2 3.1 363 1.36 1.9 ,6 1.4 2;7 117 c.1 .L c.1 11 1.41 ,037 19 8.7 .26 165 445 1 .59 .c59 .2l 3.0 co1 1.2 ,I~.05 iE 1.8 18.9 6.6 27 .I 2.6 3.1 321 1.33 4.4 .6 1.8 3.4 112 .1 .2 c.1 17 1.37 .04U 20 9.4 23 .73 ,062
.1.9 19.4 8.8 30 .l 2,s 3.3 3611.46 4.7 .E 1.4 4.2 119 .I .h c.1 20 1.84 ,041 20 10.0 -24 219 ,003 E 58374 28.9 19.5 18.9 42 3.1 12.6 9.4 276 2.89 764.8 1.3 94.1 8.9 71 r.1 7.6 c.1 38 .7Q ,115 52. 34.6 .62 49 .014 cl .85 .Q26 .P .7 .Q2 2.1 .5 1.59 ,g &a375 7.7 14.6 13.6 47 LB 11.7 8.9 347 2.49 1651.4 1.2 161.7 8.0 31E .l 17.9 c.1 38 1.81 ,116 54 31.6 .56 43 .OU L .n ,023 .20 .3 .02 2.4 .3 1.33 mm76 2.6 15.5 21.2 56 .4 L3.7 11.1 3% 2.93 498.6 1.0 32.7 8.9 193 <.I 4.7 .l 35 49 .I37 66 32.5 1.02 44 ,008 1‘1:40 ,045 .29 .5 .Q2 2.2 .3 1.08 STANGAFXI LE4 6.5 129.6 30.0 161 .3 33.5 11.8 790 3.19 22.5 6.6 24.6 3.8 213 5.2 4.8 5.2 74 .54 .a&( 15 1~38.4 .57 137 ,066 3 1.70 ,029 .LS 3.8 .27 3.5 1.2 c.05 E . . G- IDA - lo.0 rW SAMPLE LEACHED UITH 60 ML 2-2-2 WCL-k&N20 Al 95 DEG. C F(R ONE H,XAI, DlL"TFI) TO.200 M., AMUSED BILCP-MS. UPPER LINllS - AG, W, HG, Y D 1W PAI; HI, Co, CD, Wr GI; lH, "LB 2 = 2.000 PPN; Cu. PE, ZN. III, NMIY. AS. V. LA. CR = 10,000 PCII. - SANPLEIWE: a4lE RlSObDC Ai' muAt* we -ideMd the mfidential prqmrty 01 the cl/eat. km Gsum the liGbil{ties fir actual east bf the analysis only. S.wPLE# Ma Cu Pb Zn &I 111 Co Iin Fe te U Au Th Sr Cd Sb Bi 'I Cd P La Cr Kg ea Ti 8 Al Il.3 K u t@ SC ll 5 Pm Ppm PP PW Ppn Ppn PW PW s PP FW wb FP PW IW w m PP X 1 Ppln PFm x PP XPpln 1 g g W FFm PP PPR x P 51 .1 1.9 4.9 10 .1 .6 c.1 72 .D3 .7 c.1 q.5 c.1 1 .I .2 <.I Cl .06<.aal ~1 1.4 <.a1 4~.001 2 c.01 ,343 c.01 .I .a2 .l <.I c.65 w4 32.3 28.9 19.9 69 1.7 27.9 15.4 693 3.36 129.3 1.1 186.9 3.9 111 c.1 1.9 .2 67 2.71 ,163 69 49.6 1.59 41 ,120 d 1.82 ,009 .20 1.2 .G2 4.3 .3 32 34415 1.2 B.6 20.7 66 .4 26.1 16.1 708,. 3.43 3.2 1.4 13.1 3.8 Ia4 .L .3 C.L 61 3.7a.L74 57 51.7 1.79 33 ,197 <12.05 ,016 .L7 1.4 .02 5.0 .2 .47 34406 .8 23.7 19.2 61 .I 23.3 13.5 758 3.15 2.8 1.1 8.8 3.9 207 .l .3 c.1 61 2.80 -161 56 47.11.44 36 ,143 11.77 ,007 .I4 .7 .Ol 4.5 .1 .I1 34407 1.2 29.2 19.8 68 .2 27.2 16.2 764 3.65 5.5 1.1 11.1 3.8 191 .l .4 c.1 68 3.27.175 62 5521.59 38 ,132 11.80 ,024 .14 2.1 .04 4.4 .2 .89 34408 .7 259 19.9 6J .4 24.6 15.0 787 3.48 3.0 1.2 9.3 4.0 200 ., .3 ~.l 64 X69.167 67 48.01.63 36 ,179 Il.83 ,027 .16 .9 .02 4.9 .2 .67 34409 .6 24.619.3 58 .522.213.7 6533.05 2.9 1.1 7.9 4.0 199 .2 .2 .I 56 3.57 X8 57 46.61.48 35 .L56 ~1 1.56 .a32 .14 2.3 .04 4.6 .2 .47 34410 -2 4.8 7.1 16 .3 5.2 4.2 598 .80 .6 .3 5.5 1.1 1222 .3 .l c.1 1424.10 .041 16 11.5 ~41 10 .a53 3441 1.3 38.5 18.3 63 .I 28.1 17.4 721 3.49 4.5 .9 5.6 3.9 272 .l .3 .l 46 3.07 .L68 78 54.51.57 36 ,035 2 1.80 .049 .20 1.2 .02 3.2 .2 .57 34419 I.1 29.4 17.3 66 .3 25.7 L5.6 7323.51 .3.9 1.0 6.9 4.1 314 .I .2 C.1 48 3.61 ,169 78 51.E 1.70 42 ,072 -=l 1.93 ,047 .22 2.1 CO1 4.0 .l .b3 34420 .P 23.2 17.6 61 .3 22.1 14.0 744 3.18 3.6 .9 7.1 4.2 325 c,L .2 c.1 41 4.10 ,166 78 41.11.61 42.030 2 1.83 ,052 .22 1.0 .Ol 3.4 .l .66 RE 34420 .9 22.2 17.1 61 ,322,s 13.9 7653.15 3.4 .a 7.8 4.3 317 .I .2 c.1 41 4.03 .I59 73 4L.0 1.57 41 ,030 2 1.76 ,050 .22 .9 A1 3.4 .2 .64 API 34420 .P 23.6 18.4 63 .3 21.4 14.2 758 3.23 3.6 .9 7.3 4.3 320 .I .3 c.1 43 4.U .170 78 40.51.62 W ,028 11.83 ,052 .21 1.7 ~01 3.4 .2 .66 34421 1.7 15.7 16.3 34 .7 22.3 9.2 787 1.78 69.5 .5 408.3 2.1 576 .l .8 c-1 2011.01 .092 41 39.9 .87 41 ,003 ~1 .91.024 .l3 1.3 .Ol 1.4 .L .64 34.m 1.1 27.6 19.3 63 .324.5 14.9 7303.45 62.1 .9 10.0 4.0 323 c-1 .7 s.1 45 3.89 .175 79 45.3 1.77 41 ,031 Il.96 .M9 22 1.7 .Ol 3.5 .2 .74 34423 1.0 27.221.0 M .123.615.1 8723.41 3.3 .9 7.1 4.1 300 c.1 .2 s-1 4.3 5.13 .I71 75 45.2 1.65 53 .069 2 1.84 ,049 22 1.0 s.01 3.5 .2 .b'l 34424 1.0 23.3 13.6 46 .6 19.1 11.1 7E822.66 17.8 .6 15.1 3.2 356 <.I .4 c.1 34 5.58 ,122 4 36.3 1.33 27 ,003 3 1.38 ,029 .17 1.7c.01 2.1 .1 .eo El!341 28.2 13.3 20.1 51 2.8 13.5 8.9 253 2.25 286.5 1.6 61.1 12.2 43 <.I 4.8 x.1 30 .EO ,106 67 35.6 .I4 33 .I37 4 1.01 ,007 .20 1.9 .03 2.9 .8 .Ea 52342 315.2 18.8 26.7 39 18.9 12.8 8.1 220 4.03 1034.1 1.5 889.9 7.3 66 <.I E4.7 .I 21 .92 ,076 34 31.5 .42 25 .060 2 .59 .a05 .I5 6.9 .lL 2.0 20.5 3.45 58343 L.3 13.0 X6 50 .9 13.9 9.4 260 2.13 303.6 1.5 14.0 12.5 40 <.I 3.0 <.I 25 .51 ,110 63 34.9 .73 37 .a83 2 34 .oas .20 2.0 .G2 2.5 .4 .62 58344 7.7 14.3 L7.2 56 .714.7 8.1 247 2.11 184.8 1.7 6.7 13.6 38 .l 2.8 c.1 4G3 .U ,111 67 38.4 -72 45 .I15 3 1.06 .OOE .24 3.9 .02 2.8 .4 .43 58315 2.3 16.914.8 61 .? 14.7 8.1 2292.23 218.5 1.8 28.013.8 35 CL 2.7 <.L 51 .39 .112 67 39.7 -86 48 ,114 3 1.11 .007 .24 2.0 a.01 3.2 .2 .54 582.46 1M.5 13.8 16.8 51 2.6 15.4 9.1 186 1.67 307.9 2.2 54.9 13.9 53 c.1 5.1 <.I Z?8 .50 ,101 58 32.0 .5b 65 ,056 1 .76 ,009 .25 4.3 .05 2.1 1.1 .50- 58347 30.9 11.4 9.0 33 1.1 10.2 5.7 103 1.25 338.3 1.6 56.612.7 37 c.1 3.9 <.I 25 .33 .O89 53 25.2 .37 ~59 ,042 3 -55 ,008 -25 1.9 .a3 1.4 .4 .49 5rw3 217.3 14.3 11.0 30 4.510.1 5.2 1981.62 -WA.9 L.87J6.110.7 90 r.1 9.0 c.L 25 .b3 ,082 45 30.3 .41 55 .G18 2 .5b .OOb .21 5.3 .07 1.5 1.7 .74 58350 343.1 14.6 8.9 22 6.9 8.4 4.5 212 1.87 553.5 2.0312.4 9.9 88 <.118.2 c.1 32 .87 ,074 36 27.9 .45 35 ,010 5 .54 ,006 .I6 2.6 .09 1.6 3.5 1.15 58351 87.5 L5.0 15.9 49 1.5 12.6 8.2 349 2.37 356.9 2.5 63.0 14.2 137 c.1 6.2 x.1 47 1.65 .W 54 35.6 .I1 51 ,082 2 .87 ,007 .20 5.0 .06 2.8 1.1 .96 58352 6.0 16.5 12.6 55 .5 11.2 7.2 312 2.00 09.0 3.7 125.4 15.5 88 .L 2.1 c., 35 .85 .I06 66 38.2 .GO 67 .C82 11.06 ,009 .26 2.5 .03 3.0 .4 .23 STAlwAnrJ OS4 6.4 126.6 30.6 153 J33.4 11.7 75533.19 22.4 6.3 28.8 3.6 27 5.4 5.3 5.2 72 .% .OE5 15 158.4 .57 139 ,081 2 1.68 ,028 .15 4.4 .28 3.7 1.2 c.05. GR(UP 1DA - 10.0 01 SAMPLE LEACHED "IT" 60 HL 2-2-2 "CL-"HO%"2G AT S'S DEG. C FOR OHE HOUR. DILUYED TO 200 ML, ANALYSED GY ICP-MS. UPPEG LIYITG - AGO. AU, HE. " = 100 PPM: "0, W, CD, 58, 81, T", " A S - 2.000 PPW; CU. PG, Z,,, NI, MH, AS, V, LA, CFi = 10,OW PPW. - SAMPLE TYPE: CGRS R150 MC Smr., es beainninq 'RE' we Reruna end 'RRE' apa Reiect Rerun*. DATB RECErVgD, OEC 4 2002 DATE REPORT MAILBD: p& ,&. SIGNED W.C. D. TOYE, C.LECMG, J. UAWG; CERTIFIED 8-C. ASUYERS ALL results arc considered the confidential property of the client. Acme assums the liabilities far a f the analysis only. 3 ‘I!+ Doublestar Resources Ltd. PROJECT GOLD FILE # A205317 Page 2 s .I"I*ILvnw rm /.vLwo[IL WPLE% b C" Pb 2n R-J Ni Co Hh Fe ds U A" nl *r Cd Sb Bi V Ca P La Cr Hg Ea Ti B Al tia K ld lig SC 11 5 Gi d PPn FPn Ppil PP PPn FP PPn PP s FW PP~ PPb PP F@ YW PP~ PW m x 1. FP Fw x PP fPpn x x x Ppn Ppn Fpn Pm x PP .5e35458353 13.61.6 13.911.016.8 11.5 4649 .7.712.4 12.5 8.68.3 4282.1661.62% 2.23 72.9 2.314b.215.52.1 299.9 15.2 Mb114 c.1.1 1.41.3 c.1 4241 1.501.02 .095,099 5963 38.339.5 .BB.92 61 .W4 1 1.14 ,004 .23 4.7 .lV 2.9 .2 .36 ; 68355 1.2 14.0 11.0 42 .2 12.1 7.7 62 .D93 1 1.07 ,008 .23 2.6 .Ol 2.8 .L .34 I 58356 .3 IL.4 12.5 16 .l 7.0 5812.02 LB.5 1.5 29.6 14.2 332 .L .6 cl 31 2.07 ,094 58 36.7 .B5 43 ,051 *I 1.07 ,009 .23 4.5 .OL 2.5 .L .09 ; 4.21378 .76 18.7 .2 7.7 1.12094 .L .3 <.I 9 25.65 ,045 20 10.7 .43 45 .a04 58357 .4 20.0 I4.8 77 .146.9 18.8 1632 3.87 5.9 2.2 7.9 5.5 231 .I .5 c.L 80 3.25 ,182 65 93.9 2.38 146 ,352 CL1 2.32.48 ,056,013 .I8.09 2.4.7 c.01TO1 6.4.a C.Lc.1~05 .oa Li STPJIDPXI 041 6.7 124.8 30.6 165 .334.8 12.7 816 3.34 23.1 6.1 28.2 3.8 26 5.3 4.7 4.9 77 .55 .O83 17 166.8 .M) 159 .aB2 ~1 1.74 .a32 .L5 4.1 29 3.5 1.1 .06 I SXple tame: COG RIEAI 6OC.