Central Patricia Property Pickle Lake District of Kenora - Patricia Portion Ontario

Transcription

1 JAMES E. TILSLEY ft ASSATES LTD. v/.se DNA LAKE 00 GLDEN SHADW RESURCES INC. 8 EXPLRATIN PRGRAM Central Patricia Prperty Pickle Lake District f Kenra - Patricia Prtin ntari James E. Tilsley s Assciates Ltd. Cnsulting Gelgists and Engineers Aurra, ntari, Canada LG G8 Decemb

2 JAMES E. TILSLEY A ASSATES LTD. l l ' S008NE000 S0 nnna life DNA LAKE 00C TABLE F CNTENTS SUMMARY AND CNCLUSINS l INTRDUCTIN LCATIN AND ACCESS CLIMATE, TPGRAPHY, LCAL RESURCES PRPERTY... 8 HISTRY GELGY MINERALIZATIN PRDUCTIN 0 RESERVES 0 8 EXPLRATIN PRGRAM 0 GEPHYSICAL SURVEYS MAGNETIC SURVEYS Central Patricia Mine Grid Allan Creek Grid Pickle Crw Grid VLF-EM SURVEYS Central Patricia Mine Grid Allan Creek Grid Pickle Crw Grid GECHEMICAL SURVEY Central Patricia Mine Grid Pickle Crw Grid REFERENCES.

3 JAMES E. TILSLEY ft ASSATES LTD. Appendices (Appended) Appendix I List f Claims. (in accmpanying binder) Appendix II Appendix III Appendix IV Appendix V Gelgical Plans Magnetic Survey Plans VLF-EM Survey Plans Gechemical Survey Results Assay Certificates Maps Prperty Lcatin and Index Sheet Fllwing pg. Gephysical Surveys - Central Patricia Mine Grid Fllwing pg. Gephysical Surveys - Pickle Crw Grid Fllwing pg.

4 JAMES E. TILSLEY ft ASSATES LTD. SUMMARY AND CNCLUSINS During the past five years fur explratin prgrams have been cmpleted n the Central Patricia prperty f Glden Shadw Resurces Inc. at Pickle Lake, in the Patricia Mining Divisin, ntari. The first prgram was cmpleted in December f 8 and cnsisted f magnetic and VLF electrmagnetic surveying f apprximately km f lines, including prfiles and base lines, cut n the prperty. The prfile cntrl lines were riented nrth-suth and spaced at m intervals alng east-west base lines. Statin interval was nrmally m. Limited induced plarizatin surveying was als carried ut in claim PA. This wrk indicated eight first pririty and nine secnd pririty explratin targets. Diamnd drilling ttalling 00 feet (8m) in five hles was carried ut during January and February f 8. Results were generally less than ecnmically interesting. The best intersectin was 0.8 unces gld per tn fr a cre length f.0 feet btained frm ne f the hles drilled n claim PA. Gelgical mapping, gechemical surveys, trenching, and sampling were dne in September and ctber. Based n the results f the 8 prgram, further wrk was recmmended. Diamnd drilling f hles fr a ttal f. feet (m) began in mid-nvember, and was cmpleted in late December, 8. This drilling tested irn frmatins indicated by gephysical survey results btained in late 8, and was

5 JAMES E. TILSLEY ft ASSATES LTD. guided as well by results f previus diamnd drilling, gelgical mapping, sampling and gechemical surveying. Results shwed banded irn frmatins and ccasinal quartz veining, but values were generally lw. The best sectin assayed 0. unces f gld acrss a cre length f. feet. All available data were reviewed in early 8 and additinal detailed gephysical surveying recmmended t give the kind f detail that appears t be necessary t define gldbearing znes n the prperty. Lines were run at meter spacing between the existing prfiles and the existing lines brushed ut and re-chained. Determinatins f the vertical magnetic gradient, ttal magnetic field, real and quadrature cmpnents f the VLF-EM fields bradcast by navigatin statins lcated at Cutler, Maine and Annaplis, Maryland, USA, were made each 0m alng the prfiles. Gechemical surveys fr gld using frest mull (humus) as a sampling medium were dne in selected areas f the prperty. Results f this detailed investigatin indicate that the at least the magnetic prtins f the favrable irn frmatin hrizns are rather discntinuus alng strike and that there are frequent dislcatins f the ptentially gld-bearing hrizns due t faulting. VLF-EM results prvide infrmatin n the lcatin and rientatin f fault and shear znes cutting the areas f

6 JAMES E. TILSLEY ft ASSATES LTD. interest. Three 'sets' f faults/shears are identified. ne is essentially parallel t stratigraphy but shws lw-angle crss cutting tendencies. A 'set riented at abut 0 0 is well develped in the Pickle Crw Grid area. There is als a nrthsuth riented pattern. The latter is related t strng faults such as the Pickle Crw Fault, which enters the prperty in claim PA 0 then swings sharply suth and passes thrugh t the suthern brder f the prperty. The rle f these and ther faults in develpment and cntrl f gld-bearing quartz veins bears further investigatin/ particularly in thse areas where gechemical results shw elevated gld cntent in humus' cllected near such fault/shear znes. Results f gechemical studies frm the prperty suggest that there is a danger f cntaminatin f humus samples cllected within l t km frm tailings dispsal areas. Results f sampling in the western part f the prperty near the Central Patricia N.l mine shuld be interpreted cautiusly, at least until the pssible cntributin f wind-blwn tailings t the values reprted is established. Gechemical surveying results frm samples cllected in the eastern part f the prperty suggest there are sme areas adjacent t banded irn frmatins, and thers apparently under lain by metavlcanics and cut by fault r shear znes, where the distributin f gld in humus is indicative f mineralizatin in place. Further explratin is warranted in bth the eastern and western parts f the claim grup.

7 JAMES E. TILSLEY ft ASSATES LTD, INTRDUCTIN James E. Tilsley S Assciates Ltd. was retained t carry ut an explratin prgram n the Glden Shadw Resurces Inc. Central Patricia prperty, lcated at Pickle Lake, Patricia Mining Divisin in the Patricia Prtin f the District f Kenra, nrthwestern ntari. The prperty was first staked in the 0s and became part f the Central Patricia Gld Mines Ltd. hldings. The Central Patricia Mine was brught int prductin in and was an imprtant gld prducer thrugh the years t the end f when peratins ceased. 08,0. unces f gld and 8,. unces f silver were recvered frm,,8 tns milled. The Springer Mine als lies within the claims and perated frm t 0.,8. unces f gld were recvered frm 8,88 tns f quartz mined and milled. Renewed interest in gld explratin in the late 0s resulted in the prperty being re-examined and subjected t gephysical surveys and diamnd drilling beginning in 8. Data frm these prgrams in the files f Glden Shadw Resurces was received in early 8 and partial recrds frm the t peratins were btained frm the ffice f the Resident Gelgist in Siux Lkut. This infrmatin was studied and additinal gephysical and gechemical surveying carried ut. Several f the gelgical plans f the prperty were re-drafted frm salid prints that are believed t the nly

8 JAMES E. TILSLEY ft ASSATES LTD. existing cpies f the infrmatin. Ttal field magnetic and magnetic gradient infrmatin was cllected at statins lcated each ten meters alng nrth-suth lines spaced at m intervals. At the same time three cm pnents f the VLF-magnetic field bradcast by tw separate navigatin statins were recrded. The surveys emplyed a Scintrex IGS- system fr magnetic and VLF-EM data cllectin. The magnetic survey prtin f the instrument package was syncrnized with a recrding magnetic base statin.equipped with 8Kb internal slid state memry and pre-prgrammed micrprcessr crrectin rutine fr magnetic diurnal variatin. The VLF-EM data prvides infrmatin interpreted t relate t structural cnditins within the rcks f the prperty and the magnetic data serves t utline the limits f magnetic irn frmatins, sme f which are related t gld-bearing znes. Gechemical results indicate areas in which additinal detailed prspecting is warranted. Detailed discussin f results and interpretatins f data are presented in the bdy f the reprt.

9 JAMES E. TILSLEY ft ASSATES LTD. LCATIN AND ACCESS The prperty lies in the Patricia Mining Divisin in the Patricia Prtin f the District f Kenra, nrthwestern ntari. The main grup f claims extends t the east frm the Cnnell/Pnsfrd twnship line fr a distance f apprximately five miles, and ne half t three-quarters f a mile west f that line int Pnsfrd Twnship. There is ne additinal grup f six cntiguus claims in Pnsfrd/Twnship and tw individual claims that lie t the suth f the main grup and east f the village f Pickle Landing. A grup f fur claims lies n the Crw River n the east bundary f Cnnell Twnship. The Cnnell/Pnsfrd twnship line fllws lngitude 0 0 0' 00" West. Latitude 0 0' 00"W passes apprximately. miles nrth f the Central Patricia N. shaft. Highway and its extensin, Highway 808, run nrth thrugh the western part f the main claim grup. The Springer shaft can be reached by a rad that runs frm Highway east thrugh the claims and extends nrtheast t the bundary f Mccullagh Twnship abut n half mile suth f the Crw River. The claims area can be reached by Highway nrthnrtheast frm Ignace n the Trans Canada Highway, a distance f apprximately 80 miles (0km), r by daily air service frm Thunder Bay.

10 KEY MAP PRPERTY Scale = 0,000 l Albany River Shaft Pickle Crw N. Shaft )~ Central Patricia Shaft Springer Shaft.B.L.. ; CENTRAL PATRIA MINE GRID PICKLE CRW GRID GLDEN SHADW RESURCES INC. CENTRAL PATRIA PRPERTY Pickle Lake, ntari N S F R D PRPERTY LCATIN AND SHEET INDEX

11 JAMES E. TILSLEY ft ASSATES LTD. CLIMATE, TPGRAPHY, LCAL RESURCES The latitude f the prperty is apprximately 0 0 0"N and the climate is nrthern cntinental. Summer highs may reach 0 Celcius and winter lws apprach - 0 C. Frst is pssible thrughut the entire year and wet snw has been recrded in each f the summer mnths. The mean annual rainfall based n data cllected in the thirty year perid t is.mm and the mean annual snwfall fr the same perid is.8mm. Ttal average annual precipitatin is.mm r 8.8 inches. The elevatin f the regin is abut 00 feet (m) abve sea level. Lcal relief is generally less than 80 feet (0m) and mst hillcks rise less than 0 feet (m). There is ne cnspicuus hill just nrth f Pickle Lake twnsite that rises several hundred feet abve base level and serves as a lcal land mark. There is much prly drained grund. Swamps and meadws are develped extensively. The Kawingans (Crw) River flws nrtheast thrugh the prperty t Badesdawa Lake and the tskwin River which is part f the Attawapiskat River system that drains east-nrtheast t James Bay. Vegetatin cnsists f pplar and jackpine n the gravel ridges and ther higher grund, with black spruce in lwer wet areas. Lcally much f the merchantable timber has been harvested althugh recent highway cnstructin has prvided access t mre desirable stands nrth f Pickle Lake.

12 JAMES E. TILSLEY ft ASSATES LTD. There are general laburers available lcally, but skilled miners and supprt persnnel wuld have t be recruited else where. Pst ffices are lcated at Pickle Lake and Central Patricia. There are several general stres/ a mtel, and a htel in Pickle Lake. Charter air services are available in Pickle Lake and a Federal Ministry f Transprt airprt serves the lcal area with cnnectins n a scheduled basis t Thunder Bay. The clsest rail cnnectin t Pickle Lake is the Canadian Natinal Railway at Savant Lake, apprximately miles (0km) t the suth n Highway N.. PRPERTY The prperty cnsists f a ttal f 0 mining claims. Ninety-eight are in ne cntiguus blck which is made up f the Main and Springer grups. In additin, there is a six claim grup plus tw individual claims in Pnsfrd Twnship and a fur-claim blck in Cnnell Twnship n the Crw River. The latter grup extends acrss the Cnnell/McCullagh bundary with abut acres lying in Mccullagh Twnship. The claims are listed in Appendix I.

13 JAMES E. TILSLEY 8c ASSATES LTD. HISTRY Prspecting in the Pickle Lake area began in the early 0s. The discvery f the Central Patricia Mine is attributed t Gerge Simmns and Bill Seiger in. Assay results frm samples taken at their riginal shwing were lw and n claims were lcated. Hwever, the area was staked in by Alex and Murdch Msher fr a prspecting syndicate.frm Haileybury. The claims were ptined frm the syndicate in 8 by F. C. Cnnell wh financed a trenching and sampling prgram that was dne under the directin f Arthur Cckshutt. Results f this wrk were encuraging and undergrund wrk began in 0 but, due t the ecnmic cnditins prevailing at the time, start f prductin was delayed until. The Central Patricia Mine perated t the end f. The Springer Mine, which is lcated abut. miles t the east f the Central Patricia main shaft began peratin in and clsed in 0. Central Patricia Gld Mines Ltd. prduced,80 unces f gld frm the tw peratins, slightly mre than 08,00 unces f gld came frm the main mine. The balance was recvered frm abut,000 tns f mill feed extracted frm the Springer Mine. The Pickle Crw Mine lies t the east f the Springer Grup f the riginal Central Patricia Gld Mines Ltd. prperty. The Pickle Crw Mine was discvered in 8 by H. H. Hwell and Jck MacParlane. During the twenty-six year perid frm t this peratin prduced,, unces f gld frm,,

14 JAMES E. TILSLEY ft ASSATES LTD. tns f mill feed treated. Prir t Glden Shadw Resurces Inc. ptining the prperty in 80, there had been very little gephysical surveying and much f the verburden-cvered areas f the claims were relatively unexplred. The first prgram was cmpleted in December f 8 and cnsisted f magnetic and VLF electrmagnetic surveying f apprximately km f lines, including prfiles and base lines, cut n the prperty. The prfile cntrl lines were riented nrth-suth and spaced at m intervals alng east-west base lines. Statin interval was nrmally m. Limited induced plarizatin surveying was als carried ut in claim PA. This wrk indicated eight first pririty and nine secnd pririty explratin targets. Diamnd drilling ttalling 00 feet (8m) in five hles was carried ut during January and February f 8. Results were generally less than ecnmically interesting. The best intersectin was 0.8 unces gld per tn fr a cre length f.0 feet btained frm ne f the hles drilled n claim PA. Gelgical mapping, gechemical surveys, trenching, and sampling were dne in September and ctber. Based n the results f the 8 prgram, further wrk was recmmended. Diamnd drilling f hles fr a ttal f. feet (m) began in mid-nvember, and was cmpleted in late December, 8. This drilling tested irn frmatins indicated 0

15 JAMES E. TJLSLEY ft ASSATES LTD. by gephysical survey results btained in late 8, and was guided as well by results f previus diamnd drilling, gelgical mapping, sampling and gechemical surveying. Results shwed banded irn frmatins and ccasinal quartz veining, but values were generally lw. The best sectin assayed 0. unces f gld acrss a cre length f. feet. All available data were reviewed in early 8 and additinal detailed gephysical surveying recmmended t give the kind f detail that appears t be necessary t define gldbearing znes n the prperty. Lines were run at meter spacing between the existing prfiles and the existing lines brushed ut and re-chained. Determinatins f the vertical magnetic gradient, ttal magnetic field, real and quadrature cmpnents f the VLF-EM fields bradcast by navigatin statins lcated at Cutler, Maine and Annaplis, Maryland, USA, were made each 0m alng the prfiles. Gechemical surveys fr gld using frest mull (humus) as a sampling medium were dne in selected areas f the prperty.

16 JAMES E.TJLSLEY ft ASSATES LTD. GENERAL GELGY The Central Patricia prperty is lcated in the Pickle Lake Greenstne Belt. Basic vlcanic flws predminate but intermediate t acidic pyrclastic beds, metasediments and irn frmatin interbedded with the basalt flws are als present. The vlcanics and metasediments are intruded by gabbr, dirite, and feldspar prphyry. The greenstne belt lies within granitic basement which is expsed t the nrthwest and t the sutheast. The vlcanics and metasediments have been flded int a series f anticlines and synclines that strike parallel t the general nrtheasterly trend f the belt. The greenstne belt appears t have develped frm a basaltic vlcanic platfrm cmpsed f alternating Fe-thleiitic and Mg-thleiitic flws which were isclinally flded and subsequently verlain by a felsic vlcanic pile. The felsic rcks are largely erded, sme remnants being expsed in the sutheast part f the Pickle Lake area. The regin was defrmed subsequently and tilted t give a generally nrtheast t east-west strike and steep dips t the nrth. Cmplex flding, which is shwn by the banded irn frmatins, develped alng axial planes that strike N 0 0 E and dip 0 t 80 0 nrth in the area f the claims. The flding appears t plunge t the east thrughut the central part f the Pickle Lake gld area. Within the Central Patricia prperty, basaltic t andesitic

17 JAMES E. TILSLEY ft ASSATES LTD. vlcanic flws are the mst cmmn rck types. Minr felsic flws, pyrclastic and metasedimentary beds are present. Bands f magnetite/siderite/silica irn frmatin ten t thirty feet thick strike generally east-nrtheast parallel t the reginal trend f the vlcanics. Flding, which is mst well develped in the eastern part f the prperty, has resulted in prnunced lcal changes in strike and dip f all units, mst ntable in the case f the irn frmatins which are prbably the mst traceable members f the vlcanic-sedimentary sectin within the claims. Felsic intrusives, present as dykes and sills in the vlcanics, are mst cmmn near the Hker-Burkski stck between the Central Patricia shaft and the Springer Mine. These rcks are usually sheared quartz-feldspar prphyry, smetimes mapped as quartz-sericite schist. Gabbr dykes are nted near the Springer Vein, and ne Keeweenawan diabase dyke is fund striking nrth-nrthwest acrss the prperty abut ne-half mile east f the Central Patricia shaft. The axis f flding in the Central Patricia claims strikes 0 0 at the Main Mine and swings t abut 00 0 near the Hker- Berkski stck. East f the stck the fld axis swings back t east-west nly t assume the S 0 directin nrtheast f the Springer claim grup. The Central Patricia anticlinal axis passes apprximately 000 feet suth f the N. l shaft (Main

18 JAMES E. TILSLEY ft ASSATES LTD. Mine). Beds n bth limbs f this fld dip steeply t the nrth, the suth limb being verturned. The Pickle Crw synclinal axis parallels the anticline and lies abut 00 feet t the suth. A secnd synclinal axis lies abut 000 feet nrth f the N. l shaft. This fld appears t parallel the principal anticline but has nt been explred in detail. The majr faults in the area are the Dnna Creek, Pickle Crw, and the Chen-MacArthur. These strike abut S 0 and are essentially parallel t the fld axes. The Central Patricia Fault passes apprximately 0 feet suth f the N. l shaft. It strikes abut 0 0 t 0 0, is rughly parallel t the bedding n the nrth limb f the Central Patricia Anticline, but cuts the fld axis where the latter swings t the nrtheast in claim PA 8. A secnd set f faults lies at nearly 0 0 t the Pickle Crw and Dnna Creek faults. These faults are bserved t ffset the fld axes several tens t several hundreds f feet. Displacement is usually t the left in the Springer claims and t the right in the Main claim grup. Shearing is generally parallel t the fault structures, the mst well-develped being assciated with the Pickle Crw-Dnna Creek system. The mst usual secndary shearing strikes 0. The yungest rcks f the regin are diabase and lamprphyre dikes that are cnsidered t be f Keweenawan age.

19 JAMES E. TILSLEY 8e ASSATES LTD. MINERALIZATIN Thmsn classifies the types f gld depsits as:. Fissure r cmpsite quartz veins.. Stckwrks in irn frmatin.. Silicified shear znes.. Replacement bdies.. The fissure r cmpsite quartz veins ccupy fractures and fissures as cntinuus bands f quartz r the quartz may be present as irregularly intercnnected, mre r less parallel bands separated by cuntry rck. Bth varities are frequently strngly cntrted and drag flded. Thmsn and thers reprt turmaline, chlrite, seracite and native gld as the dminant mineralizatin in this type f structure. Sulphides are nted t be rare.. The Stckwrks in irn frmatin cntain ntable quantities f sulphides and the hst rcks are ften replaced by sulphides. These znes tend t be cnsiderably wider than the quartz vein mineralized znes but are mre discntinuus alng strike. Mining experience, hwever, has shwn that these znes are quite cntinuus dwn dip.. Silicified shear znes have develped in the metavlcanics and n the cntact f the greenstnes with irn frmatin. Silicificatin may be accmpanied by sulphide mineralizatin and quartz lenses and stringers.

20 JAMES E. TILSLEY 8t ASSATES LTD.. Replacement znes in which silica and carbnate accmpany sulphides are described in assciatin with stckwrks in irn frmatin and with silicified shear znes. ther siliceus carbnate replacement znes in greenstnes that are nt related t shearing usually cntain nly lw gld values. The spacial relatinship between the knwn mineralized znes and banded irn frmatin has influenced prspecting and develpment thrugh the years. Thmsn () cncluded that the irn frmatins were nt auriferus unless they had been fractured and pened up t permit migratin f mineralizing slutins. While there is prbably a genetic relatinship between the irn frmatins and assciated gld-bearing lenses and re bdies, as elabrated in fllwing paragraphs, results f recent gechemical studies d nt indicate the irn frmatin t be a surce-rck fr gld in either the quartz veins r the 'stckwrks' znes in the irn frmatins. ur review f data frm the area and ther gld-bearing greenstne belts in the Canadian Shield suggests alternate interpretatins f the rigin f the precius metal depsits in the Pickle Lake area in general, and the Central Patricia claims in particular. There appear t be tw distinct mineralizing mechanisms, ne syngenetic, the ther epigenetic. The syngenetic mineralizatin is typified by the rebdies mined at the Central

21 JAMES E. TILSLEY ft ASSATES LTD. Patricia N. l Mine. Gld was recvered frm material mined alng the hanging wall f a band f irn frmatin. The rebdies mined plunged t the nrtheast and were ntably cn tinuus alng plunge. Sme have been fllwed fr ver three thusand feet dwn the lng axis. Strike lengths f up t 8 feet have been recrded. The re shts respnsible fr 0* f prductin at the N. l Mine (Pye, ) lie alng the hanging wall (tp) f the irn frmatin and extend tward the ftwall thrugh the irn frmatin fr distances f up t frty feet. The lng axes f the re shts' fllw fracturing that extends stratigraphically belw the mineralized znes. The thickest sectins f the mineable znes were bserved t be develped in the irn frmatin ppsite strng fractures in the ftwall basic vlcanics. Apprximately ten percent f the re frm the Main Mine was recvered frm mineralized znes that crss-cut the irn frmatin. The latter is interpreted t be f epigenetic rigin and t be later than the bulk f the re mined at the Central Patricia N. l Mine. Available detailed mapping f mineralized znes at varius levels f the Main Mine suggests that the gld-bearing quartz veinlets and sulphide stringers tend t crss-cut the irn frmatin where the re is thickest and appear t becme parallel t the irn frmatin with increasing distance alng strike frm the thicker prtins f the re shts.

22 JAMES E. TILSLEY ft ASSATES LTD. These bservatins are interpreted as evidence that the majr znes f gld-bearing mineralizatin assciated with the irn frmatin were frmed by precipitatin frm slutins cir culating thrugh the basalts during pauses in extrusin f flws. Further, the cnduits fr the auriferus slutins are the same as thse thrugh which the cmpnents f the irn frmatin were brught t the lava/cean interface. It is als prbable that the irn frmatin was relatively uncnslidated at the time f syngenetic mineralizatin and many f the 'alter atin', 'small-scale flding', and 'replacement features can be best explained by assuming a sft-sediment envirnment during the primary intrductin f precius metals. The relatinship f the sulphide-quartz-chlrite-gld mineralizatin t the irn frmatin suggests that the mineralizing slutins were intr duced late in the submarine ht spring cycle, after depsitin f the bulk f the irn frmatin, prbably in respnse t energy (heat) increase preceding renewed intrusive/extrusive activity. Subsequent mvements during flding and hydrthermal effects related t later intrusive activity have mdified the riginal relatinships s that ver-printed fracturing f the irn frmatin and re-cementing with quartz and carbnate misleadingly suggests brecciatin f brittle irn frmatin as necessary t develpment f mineralized bdies. ur experience in the area indicated that there are many znes f fractured, 8

23 JAMES E. TILSLEY ft ASSATES LTD. brecciated, and quartz-cemented irn frmatin that are essentially devid f precius metals. The epigenetic gld depsits f the Pickle Lake area are typified by the quartz veins mined at the Pickle Crw, Albany, and Springer mines. These veins develped in dilatin znes usually alng minr faults cutting the stratigraphy at lw t mderate angles. Certain f the veins, fr example, in the Pickle Crw wrkings, cut the irn frmatin withut great change in nature and limited displacement f the strata. The quartz veins als cntain "re shts" in which values are cncentrated. In the Springer, r N. Vein, there were three znes frm which mill feed was extracted prfitably. These shts were generally in thicker sectins f the quartz vein, but gd values are nt necessarily present in, r cn fined t, the thicker sectins f any vein. These veins are interpreted t pst-date the irn frmatin and are related t pst-rgenic intrusins develping hydr thermal circulatin cells in an already flded sequence f flws and related chemical and clastic sediments. The mineralized silicified shear znes and replacement bdies in sheared lavas and within irn frmatin are inter preted t relate t epigenetic prcesses, sme f which are respnsible fr frmatin f the quartz veins mined in the eastern part f the area.

24 JAMES E. TJLSLEY ft ASSATES LTD. PRDUCTIN Central Patricia Gld Mines Ltd. prduced,80 unces f gld and 8, unces f silver frm within the claim grup. Slightly mre than 08,00 unces f gld came frm the N. l, r Main Mine. The balance was recvered frm abut,000 tns f mill feed extracted frm the Springer Mine. The Pickle Crw peratins lcated n claims adjining the Springer Grup at the east f the main prperty, during the twenty-six year perid frm t, prduced,, unces f gld and 8, unces f silver frm,, tns f mill feed treated. RESERVES There are insufficient data t permit reliable estimatin f re reserves within the claims. 8 EXPLRATIN PRGRAM Explratin during the prgram being reprted included cutting f additinal intermediate cntrl lines in selected areas f the prperty, detailed VLF-EM surveying using signals frm navigatin statins NAA (Cutler, Maine) and NSS (Annaplis, Maryland), determinatin f the ttal magnetic field and the vertical magnetic gradient, and recnnaissance gechemical sampling f frest mull (humus). 0

25 JAMES E, TILSLEY ft ASSATES LTD. Gelgical infrmatin n the prperty was gathered and maps cvering the surface f the main claim grup were re drafted frm salid cpies f the riginals which appear t have been lst in a warehuse fire. Data frm bth surface and undergrund were studied in detail t understand mineralized bdies n the prperty, and t develp a genetic mdel that wuld aid in further explratin. 0. kilmeters f cntrl grid and base lines were cut within the main claim grup. Determinatin f magnetic and VLFmagnetic parameters was dne alng the prfile lines at ten meter intervals, where pssible. Data were gathered at a ttal f,0 statins within the grid areas. humus samples were cllected frm areas f the prperty. The first area lies t the east f the Central Patricia Main Mine between 0m E and 0m E. Selected parts f the eastern prtin f the grid frm 00m E t 0m E were als cvered. Sample lcatins were spaced at 0m intervals alng picket lines 0m apart. GEPHYSICAL SURVEYS The gephysical surveys emplyed a Scintrex IGS- integrated Gephysical System fitted with sensrs and prcessing circuits t permit cllectin f ttal field magnetic and vertical magnetic gradient data (MP-), and measure three cm pnents f the VLF-magnetic field (VLF-). The system includes a slid state memry in which measurements are stred in ASI

26 JAMES E. TILSLEY ft ASSATES LTD. bit, n parity frmat. Data retrieval is by RS-C serial interface t digital printer, mdem, micrcmputer, r cassette tape recrder. The field magnetic data were micrprcessr crrected fr diurnal variatin using a pre-prgramed rutine resident in the memry f the IGS- field unit referenced t cntinuus magnetic recrds btained by a MP- prtn magnetmeter perating in base statin mde, time syncrnized with the IGS-/MP- field unit. At the end f each field day during the surveys, all data were recvered in hard cpy n a dt matrix digital printer. When hard cpy had been btained and verified, the slid state memries f the magnetic base statin and the field unit were erased in preparatin fr the next survey day. Gephysical data are pltted n a series f plans presented in Appendix II. Three areas, designated 'Central Patricia Mine Grid', 'Pickle Crw Grid, and Allan Creek Grid are cvered by the surveys. The Pickle Crw Grid is shwn n three sheets, the East, Center, and West sheets. There is ne set f plans fr the magnetic data, and ne set fr each f the tw VLF-EM transmitter statins used. MAGNETIC SURVEYS The magnetic base statin was set up in Pickle Lake with the sensr psitined in the back yard f the twnhuse used fr ffice and accmdatin f the field crew. The sensr was

27 ,, ptv: Magnetic anmaly VLF-EM anmaly GEPHYSICAL SURVEYS - CENTRAL PATRIA MINE Shwing X, v ' Lcatin f Anmalies f/'.s' Scale: " * 00' li] l

28 JAMES E. TILSLEY ft ASSATES LTD. remte frm vehicular traffic and in a lcatin unfrequented by children r pets. The base statin cnsle was placed in the huse and perated in an ideal climatic and secure envirnment. The assigned magnetic base level was nt (gammas), a value clse t the actual average magnetic intensity in the area. All field readings were adjusted t this reference level. The ttal field magnetic data were crrected fr diurnal variatin using the resident IGS- rutine as described abve. Crrected values adjusted t the selected base level have been pltted t the east f the survey lines. Vertical magnetic gradients are shwn t the west f the prfile lines. The ttal field determinatins have been cntured at an interval f 0 gammas. Magnetic respnse is mst prnunced at, and near, bands f irn frmatin. Details f magnetic relatinships appear n the plans, and can be cnsidered best by reference t the magnet meter survey maps. Central Patricia Mine Grid There are six magnetic anmalies within the limits f the Central Patricia Mine Grid. Anmaly (l). The largest anmaly, shwn as () n the accmpanying l'00' sketch, is lcated just suth f the base line in claims PA and PA 88. This anmaly reflects tw parallel bands f irn frmatin extending east frm the N. l Mine. These apparently are nt n the same stratigraphic

29 JAMES E. TILSLEY ft ASSATES LTD. hrizn as the main rebdies, but were tested by shallw drill hles during the perating perid f the Central Patricia Mine. Magnetic data suggest that the bands f irn frmatin are either smewhat discntinuus, r at least have variable cncen tratins f magnetic minerals alng strike. Anmaly () lies mstly in claim PA and crrelates well with a band f irn frmatin mapped t the nrtheast. The ' 00' gelgical plan f this part f the prperty shws six diamnd drill hles cutting parts f the structure. There are n data ther than the drill hle lcatins as shwn n the gelgical plan, and the ntatins shwn. Lgs f these hles were nt lcated during ur search f the recrds in the files f the Ministry f Nrthern Develpment and Mines. Anmaly () lies in the nrthwest crner f claim PA 80 and extends int the adjining claims PA and PA 8 fr a shrt distance in each case. An utcrp f irn frmatin is mapped n the claim line between PA and PA 80. Anmaly () lies n the mutual bundary f claims PA 8 and PA at the intersectin f the claim line and the Pickle Crw rad. This magnetic feature prbably indicates a mdestly magnetic irn frmatin, hwever the gelgical plan shws diamnd drill hle 0 passing thrugh the axis f the anmaly and des nt identify irn frmatin in the accmpanying ntatin. Anmaly () is a tw line {m t 0m lng) feature. The

30 JAMES E.TJLSLEY ft ASSATES LTD. cuntry rck is shwn as andesite and metasediments. Anmaly () is caused by the diabase dyke that cuts thrugh the eastern crner f the grid in claim PA 88. Allan Creek Grid ALLAN CREEK GRID l" = 00' There is little magnetic relief shwn by surveys f the Allan Creek grid. In the nrtheastern diagnal half f claim PA 0 {PA ) the ttal magnetic field is between 00 and 00nT

31 Magnetic anmaly VLF-EM anmaly GEPHYSICAL SURVEYS - PICKLE CRW GRID shwlng Anmalies and Lcatin f Sheets WEST SHEET CENTER SHEET EAST SHEE

32 JAMES E. TILSLEY Bc ASSATES LTD. (gammas) abve backgrund as established by determinatins in the suthern quarter f the grid. The suth edge f this gentle anmaly n the east claim bundary f PA 0 crrespnds clsely with the cntact between quartz prphyry t the suth and greywacke t the nrth. The cntact is reasnably well defined magnetically m t the west but becmes less bvius farther west where the cntact appears t swing t the nrthwest. The data als indicate that the quartz prphyry dips beneath the west end f the greywacke and reappears at surface nrth f Allan Creek. There is n general magnetic expressin f the zne n Allan Creek just nrth f the midpint f the suth bundary f claim PA 0 that was drilled extensively as indicated by the gelgical plan. Pickle Crw Grid The Pickle Crw Grid extends frm line 00m E t 000m E, frm statins 0m S t the nrthern claim bundary which lies 80m - 0m nrth f the base line in the western part f the area, and abut 00m nrth f the base line fr mst f the center and eastern prtin f the grid. Anmaly () lies mstly in claim PA and extends int claim PA 8 t the nrth. The anmaly is shwn n the West and Center sheets f the Pickle Crw Grid. The ttal magnetic relief appraches,nt, with,000 t,nt cmmn ver sectins f the irn frmatin. The magnetics indicate that

33 JAMES E. TILSLEY a ASSATES LTD. the magnetic sectins f the chemical sediment are nt cn tinuus alng strike, althugh mapping indicates that the hr izn is reasnably cnsistent alng strike. The cnturing cnventin creates a very chppy picture in the west part f the anmaly area. Detailed interpretatin must ignre the cnturs and accept a lw angle f intersectin f the irn frmatins with the survey lines. In the nrtheast crner f claim PA the lenses f irn frmatin appear t be less cntinuus, r at least less cnsistently magnetic. Pye has interpreted cmplex flding arund the synclinal axis in this area. The scale f the flding is indicated t be small, and smewhat mre clsely spaced statins and lines wuld be necessary t permit defin itin f these small-scale details. Anmaly (8) relates t a majr band f irn frmatin extending int claims PA and PA 0 frm the Pickle Crw claims t the nrtheast. Magnetic relief is usually less than lnt althugh there are several lcal areas which have ttal magnetic fields up t 000nT abve reginal backgrund f apprximately 0,nT. The magnetic respnse f the main irn frmatin in the suthern branch f Anmaly () is mdest, again indicating that magnetite is nt cnsistently distributed thrughut the sediment. There is n bvius explanatin fr the magnetic highs in the nrth branch f Anmaly (8). The respnses are similar t

34 ft JAMES E. TILSLEY ft ASSATES LTD. thse assciated with knwn irn frmatin and may indicate additinal lenses swinging t the nrthwest arund the Pickle Crw Syncline. Anmaly () reflects the suthwestern extensin f the irn frmatin cut by the Hwell Vein at the Pickle Crw N.l Shaft wrkings. The suth branch f the magnetic anmaly has magnetic relief in the rder f,00nt, while the nrth branch f the anmaly shws general magnetic relief f up t,nt, with maximum differences related t a discrtete magnetic bdy f slightly mre than,nt. Infrmatin frm diamnd drill hles indicates that the irn frmatin 'package' is 0m t 0m thick and can cnsist f 'lean irn frmatin, carbnate facie irn frmatin, sulphide facie irn frmatin, and magnetiterich passages. The irn frmatin appears t be mineralgically lensy, cnsistent with depsitin f a ht spring-related chemical sediment. Magnetic data d nt suggest the irn frmatin extends significantly beynd the area investigated by diamnd drilling. Anmaly (0) lies alng the nrth bundary f claim PA 8. Magnetic relief is generally less than lnt with lcal peaks reaching,000 t,nt. The higher values are believed t be related t small lenses f magnetite-bearing irn frmatin. There is n gelgical evidence f these lenses due t verburden cver and lack f diamnd drilling within the limits f the anmaly. 8

35 JAMES E. TILSLEY ft ASSATES LTD. Anmaly () is a small, islated, high relief, feature lying in the suthern quarter f claim PA, 0m t 0m nrth f the base line, centered n line 00m E. The anmaly is lcated in an area mapped as underlain by greenstne and is nt satisfactrily explained by infrmatin at hand. VLF-EM SURVEYS The VLF-EM surveys were dne using the IGS- unit fitted with the VLF- Sensr ptin. This cnfiguratin f the instru ment measures three parameters f VLF-magnetic field.. The hrizntal amplitude vectr in a directin perpendicular t a line jining the peratr t the signal surce used.. The amplitude f the cmpnent f the vertical field vectr which is in phase with the hrizntal vectr.. The amplitude f the cmpnent f the vertical field vectr which is 0 0 ut f phase with the hrizntal vectr. These three parameters are recrded simultaneusly fr each transmitter used in a survey. The vertical cmpnents are expressed as a percentage f the hrizntal vectr. The strength f the transmitted primary field is variable with time, therefre expressing the amplitudes as a percentage f the hrizntal vectr remves cyclical variatins due t changes the amplitude f the transmitted field. If the primary field strength is cnstant, changes in the amplitude f the hrizntal magnetic field mainly reflect variatins in the cnductivity f the earth. Nrmally there in

36 JAMES E. TILSLEY ft ASSATES LTD. will be n vertical magnetic field. Hwever, near a cnductr, a vertical field will be bserved. The relative amplitudes f the in-phase and quadrature cmpnents may be used t interpret the cnductivity-size characteristics f the cnductrs. The measurements f the vertical in-phase cmpnent can be interpreted t indicate the axes f cnductive bdies by a variety f methds. Since in mst survey areas there is a selectin f cnductrs f different rientatin, we have fund it useful t plt and cntur the vertical in-phase measurements t give a srt f 'tpgraphic' presentatin, particularly if the survey cntrl lines are nt parallel t the primary magnetic field being used. (i.e. perpendicular t the line jining the instrument and the transmitter). The lcatin and rientatin f cnductive axes is indicated by trend f clselyspaced cnturs. Values fr use in first difference (maximum slpe) interpretatins r filtering manipulatins that wrk best n traverses parallel t the primary magnetic field can be recvered frm pseud-traverses laid ut n the cntur presentatin. The surveys dne n the Central Patricia prperty used the primary magnetic field bradcast by tw navigatin statins, NAA at Cutler, Maine, and NSS at Annaplis, Maryland. The instrument tunes t the set frequencies f the transmitters used in the surveys and tests the signal t cnfirm a mmentarily stable state. In the event that the signal des 0

37 JAMES E. TILSLEY 8t ASSATES LTD. nt satisfy the instrument requirements, n measurements will be recrded even if the instrument is instructed t d s. A variety f cnditins can cause data rejectin. These include a weak r unstable signal frm the transmitter, strng electrical interference frm pwer lines, electric mtrs, et cetera. There are usually few prblems f this nature when using the signal bradcast by NAA. NSS, hwever, bradcasts with a pwer f 00kw as cmpared t lkw fr NAA. Therefre, it is nt uncmmn t experience primary signal difficulties when using statin NSS. When n measurements are accepted by the instrument the data utput recrds zers fr vertical in-phase and vertical quadrature. These data gaps are indicated n the plans by zers with lines drawn thrugh them. Central Patricia Mine Grid The lcatin and rientatin f the mre prnunced cn ductive features indicated by the VLF-EM surveys are shwn n the l' = 00" sketch. Vertical in-phase and vertical quadrature respnses as recrded by the IGS- system are pltted n the :0 scale plans f the grid and the psitin f interpreted cnductive axes relative t survey lines and statins are shwn alng with cnturs f the vertical in-phase measurements. The cnductive znes indicated by results f the VLF-EM surveys are interpreted t reflect znes f shearing within the vlcanics and metasediments f the prperty. There is a

38 JAMES E. TILSLEY ft ASSATES LTD. tendency fr shearing t develp alng the cntacts f the bands f irn frmatin and alng the cntacts with ther cntrasting rck types. These znes are generally cnfrmable with the strike f the vlcanics althugh sme appear t cut thrugh bands f irn frmatin at a lw angle. The cnductr assciated with magnetic anmaly () in claim PA is an example. A secnd set f cnductive features is riented at abut 0 0. These features are interpreted t indicate znes f shearing that is part f the system related t the failure ccupied by the diabase dyke that passes thrugh claims PA 88 and PA 8 at the east end f the grid. Allan Creek Grid There are n strng r cntinuus cnductive znes indicated by results f VLF-EM surveying n this grid. Hwever, there is ne feature that extends frm abut 0m N n line m E t m N n line 00m E. This crrelates with an interpreted cntact between metasediments and quartz prphyry. The cnductive feature becmes indistinct t the west, as des the magnetic expressin described earlier. Pickle Crw Grid The lcatin and rientatin f the strnger and mre cntinuus electrmagnetic features detected by the VLF-EM surveys are shwn n the accmpanying sketch f the area. The

39 JAMES E. TILSLEY ft ASSATES LTD. vertical in-phase and vertical quadrature measurements recrded by the instrument at each survey statin are presented n the :0 scale plans. The vertical in-phase values have been cntured and the axes f cnductive structures shwn by heavy brken lines. There are three principal rientatins f cnductive features in the survey area. There are cnductive znes essentially parallel t the axis f flding, abut S 0 t 00 0, a secnd set which strikes between 0 0 and 0 0, and a third riented generally nrth-suth. Nrtheast Striking Set: The znes that strike generally parallel t the axis f flding are ften best develped alng the margins f bands f irn frmatin, as in the nrtheast crner f claim PA 8. A feature which may have sme relatinship t develpment f auriferus quartz veins is lcated in the sutheast quarter f the grid in claims PA and PA (Pickle Crw Grid - East Sheet). The structure passes very clse t the cmmn crner f these tw claims and within abut 0 meters sutheast f the Springer shaft. The structure is ff-set t the nrth near the Springer shaft. It then cntinues nrtheast and swings eastsutheast at the east limit f the grid. The Springer Vein ccupies a dilatin zne that has an rientatin cmpatible with an rigin related t right hand mvement n an assumed fault fllwing the cnductive feature.

40 JAMES E.TJLSLEY ft ASSATES LTD. Sutheast-Striking Set This set includes sme f the mst cntinuus cnductive features in the survey area. Ntable examples are fund in claims PA 8 and PA, and in claims PA and PA. The amunt f mvement that may take place n these and related structures is nt evident frm infrmatin available. Hwever, they are likely lci fr dislcatins and indicate a mre suth easterly trend t ff-setting than previusly assumed. Nrth-Striking Sets The mst ntable f the nrth-striking cnductive features lies in claims PA 0, PA, and PA, This a relatively strng cnductr riented almst parallel t the survey prfile lines, particularly suth f the base line in claim PA. It becmes mst bvius n the cntured presentatin f the vertical in-phase measurements. This cnductr plts cincident with the suthern extensin f the Pickle Crw Fault which enters the Central Patricia Gld Mines Ltd. prperty in claim PA 0. Reference t the l = 00" sketch f the Pickle Crw Grid illustrates sme divergence between the expected lcatin f the fault frm gelgical bservatins and the interpreted lcatin based n VLF-EM data. The nrtheast cntinuatin f the Pickle Crw Fault thrugh claim PA 0 int the adjining prperty is nt clearly evident in the VLF-EM data due t the presence f a pwer line parallel t the fault zne.

41 JAMES E. TILSLEY ft ASSATES LTD. A secnd cnductive feature having similar respnse and rientatin extends nrth frm claim PA 00 int the sutheast crner f claim PA frm where it swings easterly and passes frm the grid at abut the same pint as the nrtheast-trending anmaly that passes near the Springer Shaft. A third well-defined nrth-suth cnductr extends suth frm the irn frmatin in the nrtheast crner f claim PA 8 int the nrtheast crner f claim PA. This feature is truncated t the nrth by a cnductr f the nrtheast trending set, and n the suth by a feature f the west-nrthwest set. All these electrmagnetic anmalies appear t be related t shearing and faulting as ppsed t being caused by cnductive minerals with ecnmic ptential. The fracture systems which served as cnduits fr syngenetic mineralizatin assciated with banded irn frmatin d nt appear t have bvius electr magnetic expressin. GECHEMICAL SURVEY Studies f the surficial depsits within the claim grup has indicated that mst, if nt all, f the verburden is waterlain, and bears little surce relatinship with the underlying bedrck. The usual sil gechemistry is nt particularly effective under these cnditins. Frest mull (humus) develped frm leaves, needles, bark and wd frm trees grwing n the verburden will reflect the chemistry f the material penetrated by the rts. If the tree rts can traverse the verburden and

42 JAMES E. TILSLEY ft ASSATES LTD. reach bedrck, the metal cntent f the mull will be indicative f the gechemistry f the rck in place. Thse areas f the prperty where verburden cver is less than abut five t six meters, and where the water table is nt high in the verburden prfile, are favrable fr this type f investigatin. The humus material can be analized by a variety f methds. Neutrn activatin f pellets f humic material has prven t be an accurate, cst-effective prcedure particularly suited t the sampling medium. The element f mst interest in the prperty is, f curse, gld. Neutrn activatin analysis techniques are als suitable fr the determinatin f very small quantities f ther elements as well. The cst f 'additinal' elements, if dne at the same time as the gld analyses, are lw and may be useful in selectin f the mst favrable target areas in sme cases. Therefre, samples were analysed fr the full range f elements cmpatible with the neutrn activatin methd. Included are gld, chrmium, irn, cbalt, zinc, arsenic, selenium, brmine, mlybdenum, silver/ antimny, barium, tan talum, tungsten, thrium and uranium. Gld values are reprted in parts per billin (l ppb = 0.00 ppm r /0 f ne gram per tnne). Irn is reprted in percent. All ther elements are reprted in parts per millin (ppm). The metal f prime interest in this area is gld. Discussins are cnfined t the gld results btained. Data in

43 JAMES E. TILSLEY ft ASSATES LTD. respect t the ther elements is given n the assay certificates cpies f which are included in Appendix V. Central Patricia Mine Grid Results f sampling in this area are the highest btained n the prperty. Gld values range frm a lw f ppb t a high f 00ppb. The area sampled lies t the east f Fault Creek and within 00 t 00 feet f the main shaft, N.l Mine. Mst f this area is tpgraphically high and apparently well drained. Tailings have entered Fault Creek at sme time in the past, but there is n evidence f active depsitin f tailings east f the creek. While the values d have a likely range, and may relate t the mineralized znes mined, r t ther auriferus znes within the claims sampled, there is a strng pssibility f cntamin atin by wind-blwn tailings frm the dumps t the west f Fault Creek and frm the tailings dispsal area t the nrthwest acrss the Crw River frm the claims sampled. In general, there is a higher cncentratin f mst elements tested fr in this area than elsewhere n the prperty. There is a suggestin that higher values may be related t irn frmatins in the area sampled, but the data base cannt be accepted as reliable withut further cnfirmatin. Pickle Crw Grid Gld values range frm less than Ippb t highs f Slppb t

44 JAMES E. TILSLEY ft ASSATES LTD. ppb. The lwer values tend t cme frm areas where the grund is wet and, cnsequently, the vegetatin is less likely t have rts in cntact with bedrck. This is particularly ntable in results f samples taken n certain sectins f lines at the western end f the grid. Higher values are fund thrughut the prperty, smetimes they appear t be related t irn frmatin and in ther cases verlie areas mapped as underlain by basic metavlcanics. Slightly elevated values are als nted clse t intermediate t basic intrusive bdies (e.g. lines 00m E and 0m E at abut 00m N). Althugh anmalies are nt mre than abut five times backgrund in any instance, ne-statin 'spikes' are nt cmmn. The mst interesting anmalies are lcated in claims PA and PA 8. High values alng line 00m E between 00m N and 0m N are adjacent t a nrth-suth fault indicated by the VLF- EM survey. Further investigatinin this area is warranted. A secnd area warranting additinal attentin lies apprximately m t the west n lines 800m E and 80m E centered at abut 00m N. The higher values lie n the westward extensin f a fault r shear zne indicated by the VLF-EM data but there is n clear indicatin f a ntable shear underlying the anmaly, and there is n remarkable magnetic expressin. n lines 00m E and 0m E, again at between 0m t 0m nrth f the base line, there are elevated gld values in the 8

45 JAMES E. TILSLEY ft ASSATES LTD. humus. These values are frm samples taken ver and adjacent t a bdy f dirite. It is suspected that these results reflect a higher gld 'Clarke in the dirites and, pssibly, indicate that the dirite may prvide metal t the vegetatin mre easily than the ther rcks in the area. This relatinship has been bserved in ther gld camps in nrthern ntari. n lines 00m E t 0m E centering n abut 00m N, elevated values appear t be lcated ver the prjected psitin f the Pickle Crw Fault, and t the suth, rather than ver the irn frmatin which lies alng the nrth f the gechemical anmaly. Field studies in this area may prvide sme guidance fr further wrk. Gld values in humus in the western part f the grid nrth f the base line generally crrelate with areas f knwn irn frmatin where diamnd drilling has been dne during the time f peratin by Central Patricia Gld Mines Ltd. Hwever, there are several areas where elevated gld values are detected and there are n surface r diamnd drill gelgical data that serve t explain the values. ne such area lies alng the nrth bundary f claim PA between 0m E and m E. Recnnaissance prspecting in this area is suggested. Elevated gld values appear in the vicinity f the interpreted suthward extensin f the Pickle Crw Fault where it crsses the cmmn bundary f claims PA and PA. The number f samples frm this area is nt large. Therefre it can

46 JAMES E. TILSLEY A ASSATES LTD, nly be suggested that this area deserves mre sampling t develp a better data base fr further prspecting. There are tw 'pint' anmalies, ne at 0m E0m N, and 0m E/llm N. The frest mull is, in the general sense, rep resentative f the gechemical cnditins in a reasnably brad area. Hwever, small, discrete surces can cntribute enhanced quantities f metal t the mull in a relatively restricted area. Therefre, it is suggested that the area f these single pint anmalies shuld be checked in the field t determine, if pssible, whether they may indicate a vein type surce f gld. 0

47 JAMES E. TILSLEY 8c ASSATES LTD. REFERENCES Hurst, M.E. 0: Pickle Lake, Crw River Area, District f Kenra. ntari Dept. f Mines, Vl XXXIX, Part II, pp -. Thmsn, Jas. E. : The Crw River Area; ntari Dept. f Mines, Vl. XLVII, 8, Part III, pp. -. Fergusn, S. A., Gelgy f Pickle Crw Gld Mines Limited and Central Patricia Gld Mines Limited, N. peratin/ ntari Dept. f Mines, Miscellaneus Paper MP-, pp Sage, R.P. and Breaks, F.W. 8: Gelgy f the Cat Lake - Pickle Lake Area, Districts f Kenra and Thunder Bay; ntari Gelgical Survey, Reprt 0, Ministry f Natural Resurces, pp. 8. Pye, E.G. : Gelgy f the Crw River Area, District f Kenra; ntari Dept. f Mines pen File Reprt, pgs.. ntari Department f Mines Maps: P, Preliminary Map, Crw River Area, District f Kenra: Pye, E. G.,. 8, Cat Lake - Pickle Lake, Gelgical Cmpilatin Series, Districts f Kenra and Thunder Bay. : 0. Sage, R.P., Breaks, F.W., Trup, W. and Assistants, peratin Pickle Lake,. b, Crw River Area, District' f Kenra {Patricia Prtin), ntari. Scale 0 feet t the inch. Jas. E. Thmsn, 8. ther Infrmatin: Hdge, H.J. 8: Reprt n Crw River Prperty, Pickle Lake Area, ntari. Cnnell Twnship, Shegelski, R.J. 8: Assessment reprt n Gelgy and Gephysics f a Prtin f Cnnell Twnship, Pickle Lake Greenstne Belt.

48 JAMES E. TILSLEY A ASSATES LTD. Appendix I List f Claims

49 PARCEL NUMBER MINING CLAIM NUMBER APPRXIMATE ACREAGE LAND TITLES FFICE KENRA PA. PA PA PA 8 PA " PA 0 " PA " PA ". PA " PA PA " PA PA. PA " PA PA " PA PA 8 " PA " PA 0 " PA " PA " PA

50 PARCEL NUMBER MINING CLAIM NUMBER APPRXIMATE ACREAGE LAND TITLES FFICE KENRA 8 PA., " PA " PA PA PA " PA PA " PA PA PA 8 PA PA " PA PA " PA PA PA " PA " PA

51 PARCEL NUMBER MINING CLAIM NUMBER APPRXIMATE ACREAGE LAND TITLES FFICE KENRA PA " PA PA " PA " PA PA " PA PA ". PA PA PA " PA PA ". PA PA PA PA PA PA PA " PA PA PA

52 PARCEL NUMBER MINING CLAIM NUMBER APPRXIMATE ACREAGE LAND TITLES FFICE KENRA 0 H it n PA PA PA PA M II II II PA 'PA ea II PA 8.88 II PA 8.0 PA 8. II PA 8. II PA 8.8 II PA H PA 8. PA 88. PA. PA 8. PA 8.

53 PARCEL NUMBER MINING CLAIM NUMBER APPRXIMATE ACREAGE LAND TITLES FFICE KENRA PA 00 PA 00 PA 00 PA 00 PA 00 PA 008 PA 00 " PA 00 ". PA 0 " PA 0 PA 0 " PA 0 PA 0 PA 0 PA 08 PA 0 PA 00 Part f PA 0 " PA 0 PA 0 " PA 0 " PA 0 PA

54 JAMES E. TILSLEY ft ASSATES LTD. Appendix II GELGICAL PLANS Central Patricia Gld Mines Ltd. (circa - ) re-drafted frm zalid prints f riginals believed destryed in warehuse fire) GELGY - East Sheet (G -.0) l" = 00' GELGY - West Sheet (G -.) l" * 00' GELGY (G - 8-) l" = ' GELGY (G - 8-) l" = ' 'GELGY (G - -) l" * i' CMPSITE LEVEL PLAN - SPRINGER {N.) VEIN l" = 0' LNGITUDINAL SECTIN - SPRINGER (N.) VEIN l" * 0'

55 JAMES E. TILSLEY ft ASSATES LTD. Appendix III MAGNETIC SURVEY PLANS MAGNETIC SURVEY - CENTRAL PATRIA MINE GRID :0 MAGNETIC SURVEY - ALLAN CREEK GRID :0 MAGNETIC SURVEY - PICKLE CRW GRID East Sheet :0 MAGNETIC SURVEY - PICKLE CRW GRID Center Sheet :0 MAGNETIC SURVEY - PICKLE CRW GRID West Sheet :0

56 JAMES FvTILSLEY a ASSATES LTD. Appendix IV VLF-EM SURVEY PLANS VLF-EM SURVEY VLF-EM SURVEY CENTRAL PATRIA MINE GRID CENTRAL PATRIA MINE GRID (NSS) (NAA) :0 :0 VLF-EM SURVEY VLF-EM SURVEY VLF-EM SURVEY VLF-EM SURVEY VLF-EM SURVEY VLF-EM SURVEY VLF-EM SURVEY VLF-EM SURVEY ALLAN CREEK GRID {NSS) :0 ALLAN CREEK GRID {NAA) :0 PICKLE CRW GRID PICKLE CRW GRID East Sheet East Sheet PICKLE CRW GRID Center Sheet PICKLE CRW GRID Center Sheet PICKLE CRW GRID West Sheet PICKLE CRW GRID West Sheet (NSS) (NAA) (NSS) (NAA) (NSS) (NAA) :0 :0 :0 :0 :0 :0

57 JAMES E. TILSLEY ft ASSATES LTD. Appendix V GECHEMICAL SURVEY RESULTS Assay Certificates

58 X-RAY ASSAY LABRATRIES LIflJTCD 8 LESLIE STREET; DN WILLS* NTARI M J PHNE --Vi'- TELEX 0-8 CERTIFICATE F ANALYSIS T: JA'-'ES E. TILSLEY L ASSATES LTD ATTf!: J.E. TILSLEY GP PCX S STEEPLECHASE AVEMJE AURRA t NTARI L'tG G CUSTMER M. DATE SUBMITTED -MAY- REPRT 800 REF. FILE 0- ' HUMUS WERE ANALYSED AS FLLWS: AU PP C R P f f. FE y. C PPM ZN Pf! AS P P M SE P 0 M R PPM M PPM A G PPM SB PPM EA PPM T A PPM W PPM TH PPM U PPM METHD NA NA NA NA MA MA MA NA M A f!a MA NA MA M A M A MA DETECTIN LIMIT C X-RAY ASSAY LABRATRIES LIMITED DATE ls-juin- CERTIFIED"

59 NTE: DETECTIN LIMITS ARE VARIABLE DUE T THE NATURE F THE SAMPLE.

60 X-RAY ASSAY LABRATRIES -JUK-S REPRT 080 P.EF.FILE 0- PAGE i UF * SAMPLE AU PPC CR PPM FE Z C PPM L-S+0E-+0N L-+0E-+N L--E-+80N L-+E-+0N L-+E-+N L-+E-+0N -+E-+0N L-+E-+0N L-8+0E-+CN L-+0E-0N L-8* 0E-+0N L-8+QE-+0N L-8+0E-+0N L-8-HCE-*CN L-8+0E-+0N L-8+CE-+0N L-+CCE-+0N L-S+E-+0NA L-8+E-+CN L-8+E-+0N L-8+E-+CN L-S+E-+0N L-S+E-+CN L-+0E-+0N L-+0E-+0N L-+CE-+0N L-+0E-GM L-+0E-+CN L- + 0E-+0IM L-+CE-CN L-+0E-+0M L-CE-+0N L-+E-A+0N L--E-A+0N L-+E-+0N L--E- + 0N L-+E-+0M L-0E-+N L-+0E-+0N L-+0E-+N L-+0E-+0N L-+0E-+0N L-+0E-+SN L-t0E-'tN L-+0E-+N L-+0E-0N L-CE-*0.M L-+0E-+80N L-+0E-+AN L-+0E-+N ; 0 ---? 0 0 ' -j-- 0 -~. 8 C. ~* It) S 0.8- C. IB C C S C i x l,

61 X-RAY ASSAY LAbRATR lcs -juw- REPRT G REF.FILE 0- PAGt r SAMPLE AU PP GR PPM FE C PPM L-+E-+0N L-+QQE-+CN L-+GCE-+QN L-+CE-+0N L-+-JE- + 0N L-+E-+80M L-+S-+0N L-+CE-+CN L-&+E-+0N L-+CE-+0N L-*CE-*0,'J L-+L-+0N L-*00:i-*GCN L-+SE-+0N L-+E-+GGM L--E- + U.N L-G+0E-+GM L-+SE-+0N L-+0E-HCN L-CE-+0N L-+0E-+0N L-+0E-0+0M L-+0E-0+0U L--0E-0 + 0N L-+QE-M L-S+E-+80N L-+E-+0N L-+E-0N L-+E-+0N L-+E-+0N L-+E-+0N L-fE-t0N L-00E-0*0r\l L-*CE-0-*0N L-+CE-CN L-A*0E-t0N L-+CE-0+0N L-At0E-C0rj L- + CE-C-HN L-+0E-0+0S L-*0E-C-fCS L-A+0E-+0S L-+E-+CN L-i + CE-b-t-DN L-+E-+SM L-tE-0*0N L-'ifE-0*0M L-A+E-0+0N L-*-E-00S l-'**-cce-c*0s ' ? - A c 0 ~ T i- 0 0 A L/ 8 ' L ~t r, 0 c - T -* C. C C. 0, d C e B r i t. l 0 t l

62 X-RAY SAY LABRATRIES -Jin-S REPRT 00 R:F.FILE Z0- PAGE F SAMPLE AU P PS CR PPM FE Z C PPM L-+E-+CS L-+CE-C+CN L-+0E-0+CM L-& fce-c S L-+ 0E-C+0S L-+0E-+0S L-+0E-+0S L-+0E-+0S L-+CE-0+C L- + E-CS L-+CE-C+CS L-+E-+CS L-+E-+CS L-+CE-+0S L-+E-+0S L-+0E-+0S L-t,-*0C-l*0S L-+0E-+0S L-+0E-+0S L-+E-0+0S L--t CE-+0S L-+CE-+CS L-+CE-+GS L- + CE--CS L-+CE-+0S L--I- CG- + fjcs L-+0E-+N L-+0E-0+0N L- + 0E-J-0N L-H-CE-C+0S L-+0E-0+0S -H-CE-+S L-+0E-+CS L- tse-+0 L-+0E-+0S L-+0E-+0S L-+QE-0+0N L-+C-0+0S L- +E- + 0S L-+E-+0S L-+E-+0S L-+E-+0S L-+E-+0S L-+E-+0S L-+CE-+0S L-0-*-0E--f0N L-0*0E-*0N L-0tCE-0\' L-0+0E-+W L-0+0E-+0S P /. C ~~~i"?~ * w Q , S a ii i i ci ii ci ci j a i

63 X-RAY ASSAY LADRATJUtS -JUN- REPRT 800 RET.r RE 0- PAGi; -i Gf SAMPLE AU PPD GR PPM FE Z CD PPM L-0+0E-+CS L-0+GE-+0S L-C+0E-+0S L-0+E-+0N L-0+E-+80N L-0*CE-*0'J L-0+CE-+N L-0+CE-+0M L-0+CE-0N L-G+E-+0N L-0f CE-+0N L-CE-+N L-CtE--*Q,\' L-C+QG-+0M L-0+E-+N L-0+E-+0N L-0+CE-+0N L-0+E-0+0S L-0+E-+CS L-C+E-+lS L-&C+CCE-+0S L-0E- + CS L-0+E-+CS L-0+E-+0S L-+0E-+0N L-+GE-+0N L-+0E-+CM -+0E-+0N L-+0E-+CN L-*0E-**N L-+0E-+N L-t0E--0 L-+0E-CN L-f 0E-+0N L--t-0E-*0,\ L-+0E-00M L-+SE-+0N L-*0E-*0."J L-+GE-+8GN L-*E-*-'trj L--E--00,'J L-+E-+0N L-+E-+0N L-+E-+0N L-*E-*?0\ L-+E-+0N L-+E-+M L-+CE--+0N L-+E-+0N L--E-+0N ', r* S f. D iv -- 0 K 0 0 Q ~ a C G * C *J J* t C. C. C S C., <l l T L i g -* i

64 X-RAY ASSAY LABRATRIES -JUN-S RE PGRT 800 RE-r.flLE G- PAGc S GF SAMPLE AU PPD CR PPK F E C PPf, i r rt, A r "t * f rt * i t. -AyTL"~i.T-fy L-Si-CE-C'l J L-8*CE-C.'J L-C + 0E-+CM L-C + CE- + C'! L-S*0E-*0 N! L-+0E-+0N L-8 + 0E-+QN' L-8*0E-?*C\' 'L.-8+0E-+0N L-*UE- CN L-8+DE- + C"" L- + CE-+0''! L-8-t GE-+0 L-S+E-+0N L-8+CE-+0N L-8*E-*0M L-t'C-*00\' L-+CE-J-0M L-f CE-+0N L--*0E-*0;j L-.*0E-*0!k! L-S+0E-+N L-+CE-+0N L-*CC-*Crj L-+CE-+SM L-+0E-+0N L-+CE-+CW L-S+0E-+0N L-STE-S+ L--CE-*Crj L-+CE-+0N L-+E-+QN L-+-E-+N L-+E-+0N.--E-+0M L-+f.F-S+N L-+0E-+0M L-+0E-+0N L-t0E-t0-\' L-tCE-0rj L-S+0E-+N L-+&E '*! L-*0E-'t*0M L-S+0E-+0U L-S+SE-B+bQj'M L-+CE-+0N L-SG + SE-B + IJ L-S+CE-+CN * i. -J 0 ) 0 lr l* rt *U K T' 0. C 0 0 c 0 0 ' rt a ? G. r\ "" \s * c. * C. C. C n j i -) l l l l T -J t l l A

65 X-?.f,Y ASSAY LABRATRIES -JUM- REPRT C0 P.EF.FILE 0- PAGE DF SAMPLE A'j PP: C R PPM FE C PPM L-+0E-+0N L- + CE-S+fJ N L-f CE-+FJ L-+CE-+80N L-+E-+0N L-+E-+0N L-+E-+0N L-+E-+N L-+CQE-+CN L-+E-+0N L - - * 0 0 " - * 0 f i L--*-E-*-'i L-+E-+N L-+0E-S+0N L-+CE-8+0N L-+0E-+0N L-+0E-+0W L-*CE-*0 N : i -f'cj.rnn-.fqm L-*0E-*0N L-tGE--*-Gfv L- + 0E-0CN L-*0E-*C"J L-*CE-*lG k J L- + CE- *-0N L-+CE-+QN L-+0E- +0N L-+0E-+0N L-+0E-+0N L-+0E-0+0N L-+0E-0+0N L-+0E-0+0S L-+0E-0+0N L- + E M L-+CE-e+lN L- * E-0M L- + E- + C.N L-DE-*Crj L-+E-+0N L-+E-+0N L- + E- + 0N L- + CE- + 0IJ --C.Cj. t iqf' L * * \s \J. *W( L-+E-+0M L-+E--HN L-+E-+0N L-S-fE--*-0iNl L- + CE- -*QN L-+E-+0N?, 'r -... C) 0.'T T? J K C c b a i '""" ' c /, - 0 V C l i < i c. l l *ci ci ci

66 ASAY LADCRATCRIES -JU/- REPRT SC RCF.riLZ - PAGE F AU P P CR PPM C PPM L-*E-*0N L-+CE-0N L- + E-+0N L-+E-C0N L-00E-00N L-f 0E-GGN L-SS+CE-0+GS L-00E-GS i.-ge-l0s L-00E-l*vS L- t GE- +CS L-S+GCE-+0S L-CE-+CS L-S+CCE-+0S L-*0E--)CN L- GE-0.\ L-0E-+0N L-0E-+0N L- + 0E--CN L-CE-0*' L-+0E-+0N L--f 0E-+M L-S-0E-+CM L-*CE-0N L- t0e- +0N L- + SCE-+0.N L-CE-+0N L-0E-0+0N L-*0E-0*0.N L- frsge-+lcs L-+0E-CCS * ". f*sr)'-~-0'f i~"fs r)e' 'l ""0* i ff'p'sm L-+CE-B+0N, -A-E-QN L-QE-0N L- *-E-*0N L-+E-+0M L-+CE-+0N L-+E-+0N L-+GE-+0N L-CE-+0N L-0GE-Ci''l L- + E-+C.N L--V + CCE--H.M L - CE- + N L--tCE-l0N L-00E-00U L-A+E-0+0N i j. L- 0 c G i i. ** u -T 0 0? C 0 0 q 0 e -t r* R /, *T i. 8. -T t 0 g 0. 0, as c. -*... # vj * -J V * G. 0. C S 0.8 t t- f) i l A ci <l <l *. <l <l ci ci

67 X-RAY' ASSAY LAbRATDRlE S SAMPLE ~ L-JQE-0+DS L-+CE-0+0S L-+E-+0S L-+SE-B+0N L-+CE-8+0N L-+0E-S+0N L-+CE-+0N ! L-+QE-+0N L- + 0E--HN L + 0E 0.' L *" 0 E +0 \ L-+CE-0+0N L-+CE-0+0M L-+0E-0+0N L-+E-+CN L-+E-8+0N L-+CE-G+0N L- + CE-+N' L- + QCJE-CN- L-+0E-+0S L-+0E-+0S L-+0E-+0S L-+0E-+0S L-+0E-+0S L-+0E-+0S L-+0E-+0S L-+0E-+0S.L- + E-+0S L-+CE-CS L--+CE-+0S L-+CE-+0S L-+CE-CS L-+CE-+GS L-+CE-+0S L-+CE-H-CS L-+GE-+S L-l + 0E-+0S L-+0E-+80S L-l +0E- +0S L-+0E-+0S L-+0E-+S L-+E-0S L-+E-+S L-l + CE-+0S L-+E-+CS L-+CE-+CS L- + E--I-0S L-+E-+S E-JUIJ- AU P P S T _, ~".' <l 0 ; f H g ~t n S REPRT 00 CR PPM X RcF.MLE C C i t i- -0 C C B PACE C PPM a ii c l a i -a ii i \ l

68 X-RAY ASSAY LABRATRIES -JUN-8 REPRT 800 REF.FLE 0- PAGE F SAMPLE AU PPB CR PPM FE J C PPM L-+0E-0+0N L-+0E-0+0N L-+0E-0+CS L-+0E-0+0S L-+0E- *0S L-+CE-+CS L-+GE-0+0N L-+CE-0+CM L-+E-0+0S L-+CE-0+CS L-CE- + GS..L-+E-+0S L-t0E-C*C:r L-tCE-C-U C.'J L-+0C-0+DS L-+CE-0+CS L-+0E-+0S L-*0E-*QJ L- + E-0 + 0NT L-fQE-0-*-0M L-l +E-Q+CS L-+E-0+0S L-+E-+CS L-+CE-+0S L-+E-+S L-+E-+0S L-+E-+DS L-*E-*S L-+CE-+S L- + E-HS L- + CE-+S ~"" L-*0E-*S L-+-0E- + CS L-+0E-+0S L-+0E-+0S L-+CE-QS L-+E-+0S L-+E-+80S L-+CE-+0S L-+E-+CS L-l + CE- + S L-ll+SCE-Z+CS L-l + 0E- + 0S L-l * L-+CE-+0S NQ TAG S J ' 't ' G 0 -r c IB C r* y t- i l t; 0

69 ASSAY LABRATRY'S --Jjrj-0 REPRT 800 REF.FILE 0- PAGE C CF SAMPLE ZN PP"! AS PPM S PPM BR PPM L-+0E-+0N L-+0E-+N L-+E-+0N L-G+E-+0N L-+E-+N L-+QE-+0N L- + E-+0N.' L-*Qf-*80N -8+0E-+0N L-8*0E--*-0\' L L-S+0E-+CN L - * E- + N L-*0E-*0\ L-&+GE-+GN L-8+E-+CN L-8+E-+0N L-+E-+0NA L-G+QGE-+0N L-- + E-+0N L-bS + CE + SN L-+E-+0N L-8+E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+CN L-+0E-+0N L-+0E-+0M L-+0E-+0M L-+0E-+0N L-+F-+0N L-+E-+0N L-+E-+0N L-+CE-+0N L-t +CE-+0N L-+E-+0N L-+0E-+N L-+CE-+0N L-b*0E-ti L-+0E-+0N L-+0E-+0U L-+0E-+80N L-+0E-+CN L-+0E-+N L-+0E-+0K L-&+0E + 0N L-0E- 0,N L-+0E-+0N L-+0E-+N C /\ - U 0 "* i V S c g t i' *\ 8 8 8

70 X-AY ASAY LABRATRIES -JUN- REPRT 080 REF.FILE 0- PAGE DF SAMPLE ZN PPM AS PPM SE PPM BR PPM L-+E-+0N L-+E-0M L-+E-+N L-+E-+0N L-+E-+0N L-+CE-+CN L-+E-+0N L-+E-+N L-+E-+0N L-+E- + C.N L-+E-+BGN L- + E-+0N! L-+E-+CN L-+E-+0N L-*E-*e,N L-+0E-+0N L-+0E-+0N L-+0E-+0N L-*0E-*0N L-+0E-+CN L-+0E-+0N L-+0E-0+0N L-+E-0+CN L-+0E-0+0N L-*E-*n L-+E-+8CN L-+E-+0N L-+E-+0N L-+E-+0N L-+E-+0N L-+CE-+CN L-+E-+N L-00E-0+0N L-+E-0+0N L-+CE-+0N L- + 0E- + 0.N' L-+0E-0+0N L-*0E-0*0N L-A+0E-0+0N L-+0E-0+0S L-A-I-0E-0 + 0S L- + 0E-MCS L-tE-*0N L-+E-+N L-*GE--fSIS! L-fE-0*0!M L--tE-00M L-+E-0+0N L-+-CE-CCS L- + CE-0-0S C S 0 8 ~/ ( J 8 0 8

71 X-RAY ASSAY LABRATRIES -JUN- REPRT 8080 REF.FILE GF SAMPLE PPM AS PPM SE PPM 8R PPM L-+E-+0S L-+0E-0+0N L-+0E-0+0N L-+0E-Q+CS L-+0E-0+CS L-*0E-m0 L-+0E- +0S L-+0E-+0S L-+CE-0+00 L-+E-0+0S L-+CE-0+0S L-+E-+0S L-+CE-+CS L-+CE-+0S L-+CE-+CS L-*0E-U0S L-+0E-+0S L-+0C-+0S L-+0E-0S L-+E-0+0S L--fCCE-l + ls L-+CE-+0S L-+E-+0S L-+E-+0S L- + CE--HS L-*E--f0S L-+0E-+N L- + 0E N L-+0E-0+0N L-+0E-0+0S L-+0E-0+0S L--0E-+S L-+0E-+0S L-0E-+0S L-+0E-+0S L-*0E--fiS L-G+E-0+&N L-+E-0+80S L-+E-+0S L- + E- + 0S L-+E-+0S L- + E-+0S L-+E-+0S L-+E-+0S L-&+E-+0S L-0+0E-+0N L-0+0E-+SN L-0*0E-*0,N L-0+0E-+N L-0*0E-l0S C i -t ri \j "* t- *V C < 0 0 " C

72 X-RAY ASSAY LABRATRIES -JUN-8 REPRT 0S REF.FILE 0- PACE CF S Z.N PPM AS PPM SE PPM ZR PPM L-0+CE-+0S L-G+0E-+CS L-0+0E-+0S L-C+CE-+0N L-000E-0N' L-C+E-+0N L-0+E-+K L-0+E-+CN L-0+QE-+0N L-0+E-+80N L N L-0+DE-+QN L-0 + CE-+0.N L-0+CCE-+0N L-0+E-+IM L-C.+E-+0N L-0+QGE-+GN L-0+QE-0+0S L-0+GE-+CS L-0+E-+GS L-0+E-+0S L-0+E-+0 L-Q+CE-+0S L-0+E-+0S L-+0E-+CN L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+80N L-.+0E- + 0N L-+0E-+N L-+0E-+0M L-+0E-+0N L-+0E-+80N L-+0E-+0N L-CE-+CN L-+CE-+CN L-+0E-+0N L-+0E-+80N L-+E-+0N L-+E-+M L-+E-+0N L-+E-+CM L-+CE-+0N L-+E-+0N L- + E- + 0-M L-+E-+N L-+E-+CM L-*CE--*0N L-+E-+0N C D BC y t 8 C li C 0

73 RAY ASSAY L AD" ATR IE S G-JU.\-D REPRT 080 REF.FIL 0- PAGE GF SAMPLE PP.", AS PPM SE PPM IR PPM L-E- + GU L-+CE-+N L-8*0E-*N L-8+0E-+0N I E- + 0N L-8+CE-+CN L-8+CE-+0N L-8+0E-+0M L-8+0E-+0N L-B*CE-*N L-8+E-+0N ', L-+E-+0M L-+E-+DN L-+E-+80N L-Gfr0E-*',CN L-8+E-+N L-+CE-+0M L-+0E-+0N L-+0E-+CN L-+CE-+CN L-+0E-+N L-+0E- + 0N! L-+0E-+0N L-+0E-+80N L- + f;e- + -'t! L-+0E-+N L-+0E-+0M L-+E-+N L-+E-A+0N L-+CE-+CN L- + E- + Q.M L-+E-+AN L-+E-+N L-+CE-+0!': L-00E-+0N L-+0E-G+N. L-+0E-+0M L-+0E-+0N L-+0E-+80K L-*0E-tN L-+0E-+N L- + CE-+N L-+ 0E-+0N L-+0E-A+0N L-+0E- + BN L-+0E-+DN L-*f.E-*N L-+0E-+0N A C C IC t i c C V c-* 0 Q

74 ASSAY LABRATRIES -JIW-8 REPRT 00 REP.FILE 0- PAGE CF SAMPLE ZN PPM AS PPM SE PPM GR PPK L-+0E-+0N L-tCE-*-N L-+E-0N L-*E-*0 KJ L-+DE-+N L-*CE-*0N L-+CCE-+0N L- + E-+C.M L-+E-+N L-+E-+0N L-+E-0N' L-+E-+UN L-+E-+0K L-+QE-+N L-*CE-e*G.\' L-0E-C+0M L-+0E-+0N L-f +0E-+0N L-+0E-+0N L-+0E-0N L-+0E-+CM L-+0E-+0U L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+QN L-+0E-+0N L-+0E-+0N L-f0E-llN L-S-H0E-0 + 0N L-S+0E-0+0N L-+0E-C+0S L-+0E-0CN L-+E-8+CN L- + E-S-i-lN L-+CE-+CN L-+E-+0N L--E-+0N L-E- + 0N L-00E-+0N L-*E--t-0N L-00E--t-0N L-+E-+0N L-+E-A+0N L-+E-+lN L-+E-+0N L-+E-+0N L-+QE-+0N L-+E-+0N "y r\ i- U j ~* 't. A B S 8 8

75 X-RAY ASSAY LABRATRIES -JUN-8 REPRT 808G RE?.FILE 0- PAGE F SAMPLE ZN PPM AS PPM SE PPM R PPM L-+E-+0N L-00E-l0fJ L-+E-0M L-+CE-00N L- CE-0CN L-+CE-00N L-F* 00E-00S L-00F-0S t -00E-0S L-00E-0S L-00E-0S L-QE-0S L-QCE-+0S L-tE--t0S L--0E-0N L-+0E-0N L-0E-liM L-+0E-GN L- + 0E-0.M L- + 0E--I-0N L-0E-0N L-0c-lCu L-+0E-0N L-0E-0N L-+0E- +0N L - 0 E - D N L-0E-0N L-0E-00N L-0E-00N L-t-CE-0lS L - 0 E S L- + 0E-0+0S L-+0E-+CS L--*-E-S0r\l L-.00E-8 + 0N L-+E-CN L-S00E-0-N L--CE-CN L- 00E- +CN L-*-E-.0N L -QE- N L-00E-CM L-0CE-0N L-+E-CN L--CE-0N L-+E-0N L-00E-0N L-tE-l0 l'j L-00E-00M L-CCE-00M ( ( <t * S 0 R e; Q Q

76 X-RAY ASSAY LABRATRIES -JUN-8 REPRT 00 REF.FILE 0- PAGE DF SAKPLE Zr-J PPM AS PPM SE PPM R PPM L-E-0 + 0N L-+E-0+0S L-+CE-0+0S L-A+E-+0S L- + CE-00N L-+0C-C+CN L-+GE-8+0N L-:*GE-*0N L-+0E-+0N L- + GE- + G;*! L-*Gc-*iGN L- + 0C-H-0.M L-+0E- CM L-i*0tI-C*0N L-+CE-C+GN L-+CE-0+CN L-+E-+0N L-+E-S+0N L--t E-8N L-+E-+0N L-+E-+CN L-l +CE-+0S L-l L-+0E-+0S L-+0E-+0S L-+QE-+QS L-l +CE-+GS L-+0E-+0S L-l +CE-+0S L-+CE-+0S L-+E-+CS L-+E-+CS L-+E-+CS L-+E-+0S L-+CE-+0S L-l t+e-+0 L--*CE- +0S L-+0E-+S L-+0E-+0S L-+0E-+80S L-+0E-+0S L-+0E-+CS L-+CE-+S L-+E-+0S L-+E-+S L-+E-+AS L-+E-+0S L-+E-+0S L-+E-+0S L-+E-+S 0 0 C 0 0 Q C C -* t <l e; L < < * l 0 r\ D j,

77 X-RAY ASAY LABRATRIES REPRT 080 REF.FILE 0- PACE F SAMPLE ZN PPM AS PPM SE PPM B!l PPM L-+0E-0+0N L-+CE-0+0N L-+0E-0+0S L-+0E-0CS L-+CE-+0S L-+0E-+0S L-+E-0+0N L-+E-0+0M L-+CE-+S L-+CE-0+0S L-+E-+0S L-f E-0S L-*0E-0*CJ L-+0E-0+0N L-+SE-0+0S L-+0E-0+CS L-+0E-+0S L-+0E-+0S L-+E-0+N L-+0E-C+0N L-+CE-0+0S L-+E-00S L-+E-+0S L-+E-+0S L-+-E-+0S L-+E-+0S L-+CE-+0S L-+0E-+S L-+E-+S L-+0E-+S L-+0E-+0S L-+0E-+SS L-+0E-+CS L - 0iT-*0S L-+E-+S L-+CE-+0S L-l + E- + 0S L-+CE-+0S L-+E-+0S L-+0E-+S L-+0E-+0S L-+0E-+80S L-l +0E- + 0S L-l + CE- + 0S N TAG C *? f p f\ , 0 < < ' Q 0 8 P B 8 q 8 0 S - 0 0

78 X-RAY ASSAY LABRATRIES n-jl'n-s REPRT E080 REF.FILE 0- PAGE Q D? S SAMPLE M P P M A G D P M S P P M? A ' P P w L **! "! L-+CCE-+0K' L-+CE-+N L-+CCE-+i.N !-, *: l-s+sce-s + PCfJ i!ic:ap c:af:rim k. v ~..J v* C ' * J \J - * L-8 + CE- + C"! L N L- S *; L-8t0c--'s'! *0 L-P N L-8+CE-+0M* L N L-S+00-+CN L-C+E-+0N L-+E-+0N L-C*CE-*0\' L-+CE-+0N L-+CE-+0N L M L-+0E-+0N L-+0E-+0N L-+0E-+CN L-+C-+0N ! L M L-+E-A+0N L N L N.- + CE- + 0N L-+0E-+N L L-+0-+N L-+0E-+0N L-+0E-+CN L-+0E-A+0M L-+0-+0N L-+0E-+0N L-+0E-+0N L-+0E-+SDN L-t0-*'tN L-+0E-+N 0. 0,. <0. 0, f c ~s * <C. *CC < C.? < <0. *C0. <0. < C. CC. < ? <? L..'t 0. D.t C. D. S 0. C t 0, C , C.I , IC C C C 00 C *a

79 X-RAY ASSAY LA0RATRIES -JU/J- RE PRT 00 REF.FILE 0- PAGE 0 GF SAMPLE M PPM AG PPM S PPM A PPM L-+E-+CN L-+E-+0N L-+E-+N L-+CE-+CN L-+CE-+0N L-+E-+CN L-+E-+0N L-+E-+N L-+E-+CN L-+E-+0N L E- +8 N L-Se + E-Z+'tCN L-+E-+N L-+E-+0N L-+E-+0N L-+0E-+0N L-+CE-+0N L-*fiCE-*0.N L-t0E-*0N L-+0E-+0N L-CE-+CN L- + 0E-0+0.N L-+0E M L-+0E-0+0N L-+E-+N L-+E-+0N L-+E-+0N L-*E-0 N! -+CE-+0M L-+E- *CN L-+CE- +0N L-+E-C+0N L-+E-0+0N L-+E-C+0N L-0E-0N L-A+0E-+80M L-t*0E-0*0N L-+0E-0+0N L-+0E-C+0N L-+0E-0+0S L-+0E-0+0S L-+0E-+0S L-&A+E-+0N L-00E-*00?J L-'t+CE-S+SN L-A+CE-0+0M L-+E-0+0N L-e'V+E- + lm L-A+E-0+0S L-+E-0+0S <0. <0. <0. <0. <0. <. 0. <0. <0. <0. <C. < <0. < CC. C. fi C. S C ? 0.' C. 0. C. S J C , ci ci ci ci

80 X-RAY SAY LABRATRIES -JUN-8 REPRT SSC REF.FILE 0- PACE F SAMPLE ne PPM AG PPf PPM EA PPM L-G*CE-H-0S L-+0F-0+0N L-+0E-0+CN L-+SE-0+0S L-+0E-0+0S -+0E-+0S L-+0E-+0S L-+0E-+0S L-+CE-0+D L-+E-+CS L-+E-0+0S L--E-lH-lS L-+E-+0S L-+CE-+0S L-+CE-+CS L-+0E-+CS L-+0E-+0S L-+0E-+0S L-+0E-+GS L-+E-0+QS l- + GE-mCS L-*CE-l-fCS L-+E-+CS L-+CCE-+0S L-+CE-+CS L-+CE-+0S L-+0E-00N L-+CE-0+0N L-+0E-0+0N L-+0E-0+0S L-+0E-0+0S L-fcl+SCE-+S L-0E-+0S L-+0E-+0S L--0E-+0S L-+CC-0S - IfCE- + SfJ L-fcUE-0 + SS L-+E-+0S L-+E-+0S L- + E-H-QS L-H-CE-+0S L-+E-+0S L-+E-+0S L-+E-+0S L-0+&E-+0N L-0+0E-+0N L-0+CE-+0N L-0+0E-+N L-0+0E-H-0S. <C... <0. <0. < <0. C0. <0. crj CC. CC c""* r, \ \s *.C 0. C C.I 0. C C C , C C C C C IC C a C C IC 00 C C C C C C 00 C 00 C C

81 X-RAY SAY LABRATRIES - J UN- 8 REPRT 8080 REF.FILf 0- PAGE TF SAMPLF M PPM AG PPM SB PPM FU PPM L-0+0E-+0S L-0+0E-+0S L-0+E-+0N L-0+E-+80N L-0+E-+0N L-0+E-+N L-b-E-*0rj L-0+E-+0N L-0+E-+0N L-C*-CE-0N L-0+E-+N L-0+GE-+0N L-C+E-+0N L-C+CCE-+N L-0+E-+0N L-0+E-+0N L-0+QE-0+0S L-0+E-+0S L-0+E-+CS L-0+E-+0S L-0+E-+CS L-0I-E- + 0S L-+0E-+CN L-+CE-+N L-+CE-+0N -+CE-+0N L-+0E-+80M L-+0E-+0N L-+0E-+N L-+0E-+0N L-t0E-0\' L-+0E-+0N L-+0E-+0N L-+0E-+M L-+CE-+0N L-+CE-+CN L-f0E-l*8CN L- + E- + 'tj L-+CE-+N L-+E-+0N L-+E-+0N L-+E-+0N L-+E-A+0M L-Sg+E-A+SCN L-+E-+N L-+CE-+0N L-+E-+0N L-+E-+80N. <0. <0.. <0. <0. <0. <0. r\ U * <C/. <0. <u.. s r* r S. w * <0. <C... <0. <C. <a < r. I; 0... <0. C. f C, CC. CC. CG e r\ t v * D C. A *t.A C & C C C C C C C C C C C C C

82 X-RAY ASSAY LABRATRIES SAMPLE PPM REPRT 080 REF.FILE 0- PAGE GF A PPM SB PPM A PPM L-+CE-+0M L-+E-+N L-C+0E-+N L-8+0E-+0N L-B+0E-+0N L-8+0E-+SQN L-+0E-+0N L-8+0E-+N L-8+0E-+0N L-+0E-+CN L-+E-+N L-8+E-+0N L-S+CE-+0N L-+E-+0N L-8+E-+0N L-8+E-+0N L-+E-+CN L-8+E-+CN L-+0E-+0N L-+0E-+0N L-+0E-+80N L-* 0E- +0N l-f 0E-+N L-+0E-+0N L- + 0E--J-0N L-+CE-+80N L-+0E-+0N L- + 0E--I.N L-+0E-+0N L-+E-+N L-+E-+0N L-+E-+0N L-*E-*SN L-+CCE-+CN L-+E-+N L-+E-+0N L-+CE-+C" L-+0E-S+CN L-+0E-+0M L-+0E-+0N L-S+0E-+80N L-+0E-+0N L-+0E-+N L-+0E-+N L-+0E-+0N L-+0E-+0N L-+0E-+80N L-+0E-+0N L-+0E-+N L-+0E-+SN CC '? C. 0. C. CC. CC. CC. 0. CC. CC. CC. A C CC. 0. C f C. C C C L 00 C C IC C 00 C 00 C C 00

83 X-RAY ASSAY LABRATRIES -JU.*J-0 REPRT 00 REF.FILE 0- PAGE DF SAMPLE MD PPM AG PPM S 0 PM BA PP L-+0E-+QN L-+QE-8+N L-+E-+0N L-+E-+0N L-+E-+0M L-+E-+CN L-+E-+0M L-+E-+0N L-+E-+N L-+E-+0N L-+E-+0M L-+E-+0M L-+E-+0M L- + CE- *-Crj L-0E-8+0N L-+0E-8+0N L-+0E-+CM L-0E-0 N L-+CE-+0N L-*CE-f0N L-+0E-QN L-0E-*0rj L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E--CN L-+0E--HN L-+0E-0+0N L-+CE-0+0N L-t0E-00S L-+0E-0+0N L CN L-+CE-S+CN L-+CE-+CN L-+CE-+0N L-+E-+0N L-+CE-+0N L-00E-+CN L-+E-+0N L-+E-+0N L-+E-0N L-+E-+0N L---CE- + 0N L-+E-+0N L- + E- + 0.N L-+E-+0N L-+E-+0N 0. C.? C 0. C0. C0. C. CC. C. f, CC. 0. CC. CC. CC. CC. C? S X. L C.I C C 00 c l cic C C < ci < < < ci ci ci <

84 X-RAY ASSAY LABRATRIES -JUN- PRT 080 RcF.FILE 0- PAGE F SAMPLE M PPM AG PPM S PPM BA PPK L-00E-0N L-00E-0N L-00E-0N L-00E-00N L-00E-00N L-00E-0CN L-00E-00S L- + E-H-0S L-00E-0S L-00E-0S L-0CE-0S L-00E-+0S L-00E-0S L-00E-0S L-+0E-+CN L-SCE-+0N L-S0E-0N L-0E-0N L-tSE:-fJ L-+0E-+0N L-0E J-0N L-0E-0N L-0E-0M L-+0E-+0N L--0E-+0N L-0E-0N L-0E-+0N L-0E-00N L-0E-0+0N L-0E-00S L-0E-0+0S L-0E-00S L-+0E-0S L-00E-80N L-00E-8-0N L-+E-+0U L-00E-+0M L-0CE-+0N L--E-0N L-+CE-0N L- tce-l N L-00E-0N L-+E-+0M L-*-E-0N L-00E-+0N L-00E-0N L-+E-+0M L-00E-+0N L-00E-0+0N L-00E-0CN <0. <0. <0. <0. *CC. <.J <0. <0. < <0. <0. * C *. <.... <0. <0. <0.. < <0. <0.. <0.. C. C. ( G. C. rr "t J * -* C * G. C C C IC C C r\r\ J. xy 00 CCC C C C C C C C < C C C C C CCC C C C

85 X-RAY AS SAY LABRATRIES -JUN-8 REPRT 080 REF.FILE 0- PAGE SAViPLE " r* P M AG PPM SE PPM EA P 0 M L-+CE-C+QN L--E-0+0S L-+E-0+0S L-+E--HS L-+0E-+0N L-+0E-8H0N L-+-0E-G + 0N L-f 0E-+0N L- + 0E-N L- + 0E- + 0.N L-+0E-+0N L--C!:- t0,v L-+0E-+0N L-0E-0*')tt L-0E-00N L-0E-00N L- + E--HN L-00E-S-0N L-0CE-0\ L-I-E-C.N L-CE-0N L-0E-0S L-0E-CS L-+0E-+0S L-+0E-0S L-l 0E-0S L-l +0E-+CS L-0E-QS L-0E-0S L-PE-+0S L-QE-+CS L-+CE-+0S L-+E-+0S L-+CE-+0S L- + E--+0S L-+E-+CS L-+CE-+CS L-+0E-+S L-l +0G-+0S L-+0E- t0s L-+SE-+CS L-+0E-+CS L-+0E-+S L-*-E-*0S L-+E-+S L- + E--KS L-+E-+0S L-+E-+CS L-+E-+0S L-+CE-+S <0.. <0. <G.S <0. <C.. C. <0. <C CD.. -C0... s r* c S*-/ <0. <0. <0.. f <0. <0. <C.. 0. <0. <Q. < ff\ C \.. <0. <0. <0. <0. < ( - - < <? * C ri i,j f ~ vr ~ C B IC *:i 000 -a - C 00 a a a a ct ~~ DD

86 X-RAY ASSAY LABRATRIES ls-j'jn-8 REPRT 00 acf.fre 0- PAGE F SAMPLE H PPM AG PPM SB PPM A PPM L-+0E-0+CN L-l + CE-Q + 0N: L-+CE-0+CS L-+0E-0+0S L-'. + SE-l + ls L -+0 E- + S L-*QE-0*0,V J L-+E-0+0N L-+E-0+0S L-+E-0+0S L-00E-+GS L-+GE-+0S L-+GB-0-KM L- + 0E-0-UN L-+CE-0+CS L-+CE-C+0S L-+0E-+0S L-+0E-+0S L-+E-0CN L-+E-0+0N L-+E-0+0S L-+E-0+0S L-l +-E-+0S L-+E-+0S L-+E-+S L-+E-+0S L-+E-+0S L-+E-+0S L-+E-+S L-+E-+S L-+0E-+S L-+CE-+0 L-+0E-+80S L-+0E-+0S L-+0E-+0S L-+E-+CS L-CCE-*'*S.-CC-+0S L-+E-+0S L-+CE-+0S L-l 0E-00S L-l +0E-+0S L-ll r,e-*0s L-l + 0E- + 0S L-l + 0E-+0S N TAG <0.. <0. <.S <C. C. S 0.. <0. <0..0 j <0... < S <.s <0.. <0. <0.. C. C. C. CC. CC. CD. C. S CC. C. C C C C C C C C C C C. 0. Q ? f\ l u * C C.I C.l C.l C C

87 X-RAY ASSAY LABRATRIES -JUN-8.E PRT 080 REFFRE 0- PACE?.8 F SAMPLE TA ptf '-J PPM T H P PH U PPM L-+0E-+0M L-+0E-+N L-00E-+0N L-S+E-+0N L-+E-S + 'J L-+CGE-+&N L- + CE- + C;,! L-*CCc-0?J L-S+0E-+0N L-+CE-+0N L-C + 0E--UN L-+0E-+CN L-*-0E-*0rj L-8-0E--0\' L-t S0E-+0M L-8+E-+0N L-8 + E- + 0N' L-S+-E- + MA L-8*-E--HN L-8+CE-+0N L-8+E-+0N L-8+E-+QN L-80CE--0r; L-+0E-+0N L-CE-0\' L-CE-+0N L--0E-0N L-+CE-+0N L-+0E--0N L-+0E-+0N L-+0E-+0N L-+E-+0N L--fE-0N L-00E-A+0N L--f E- + 0N L--CE-0\' L-+-E- + 0N L-+SGE-+N L-+0E-+0N L-*0E-tN L-+0E-+0N L-+CE-+0N L-+0E-+0N L-te+SE-A+N L-*CE-'tt0N L-*0E-*0N L-+0E-0N L-*-DE-0N L-+CE-+ACM L-+0E--I-CN 0. <C. <0. C a 00. CD. c. p C*? en. CC. CD. CC. CC... "t t- t, - 0 t- ci? ci ci y t ī T C ci T t- l l B S C. 0.

88 ASSAY LABRATRIES * SAMP L E ~ L-QE-CN L--i 00-00M L-&CCE-0N L-&00E-0N' L-S0CE-S*,' L-E-0.N L-DE-0CN L-+ E-CN L-&00E-0N L-+C--0.N L-*E-CN L-0CE-0PN L-+E-+0N L-E-80M L-0E-0M L-0E-0N L-0E-0N L-CE-0M L-CE- f0n L-0E-GN L-+CE-CCM L - * 0 E- 0 N L-0E-0GN L-QCE-M L-CE-0N L-0CE-CN L-00E-0M L-00E-0N L-QE-0N L-00E-0.N L-00E-00N L-00E-00N L-00E-00N L-0E-&0M L-0E-+QN L-0E-00, L-0E-0CN L-0E-00K L-*-0E-00S L-0E-00S L-0E-0S L-QE-0N L-00E-0CN L-QE-0N L-00E-00N L-0CE-0CN L-0CE-00V L-00E-00S L-00E-00S - JUiJ-E T A P P ;V C.? C. C. f C.. C C. C. f C.? C0. r) c.. s C * f C. C. S <C * CC. C 0. CC. C. C. CC. C. f. CC..IE PRT 800 \i PPM i ci ci <l REP. F ILE TH PPM CC s C. CC. 0.. C. 0.. CC PAGE y P p H ,.i.S C.l C.l C. 0. C. F

89 X-RAY ASSAY LABRATRIES -JUU-0 REPRT 80G REF.FILE 0- PAGE F SAMPLE L-tE-llS L-CE-00N L-+0E-00N L-0E-C0S irjic". /ic i.c L J'-JwiCw *" f W J L-00E- tls L-0E-0S L-0E-0S L--t E-000 L-CE-0CS L-+E-00S L-+CCE-+CS L-+E-CS L-+E-0S L-00E-CS L-0E-0S L-0E- + CS L-+CE- +CS L-+CE-+0S L-0CE-00S L-CCE-LS L-CCE-+CS L-00E-+0S L-CE-0S L-00E-0S L-CE-0S L-H-0E-00N L-0E-0SM L-0E-00N L-l0E-0?S L-0E-00S L-0E-00S L-H-CE-+CS L-0E-+0S L-0E-0S L-0E-CS L-00E-0+0N L- 00E-0CS L-00E-0S L-+E-+CS L-0CE-0S L- 00E-CS L-00E-+0S L-00E-0S L-0CE-CS L-00E-0N L-0CE-?, 0\' L-0 t 0E- 0N L-0+0E-+CN L-00E-0S TA PPf C. c. r C. f. C.? CC. CC. S f\ C C. *S C. f r\ \./. c, C. C. CC. C. f. C.? C.? C.? '.l ci <l.l PPM ci A. T H PPM. CC CC CC CC. CC C U PPM C.l. C.l 0. C. 0. CC. C.l C.! C.l C.l C.I 0. C

90 X-RAY ASSAY LADRATRIES S-JU.N-S RcPDRT S REF.FILE 0- PACc CF SAMPLE TA?PH W PPK TH PPM U PPM L-0 + I.E-+0S L-0+0E-+0S L -0 f0e-*0s L- -i-e- tcn L-0+QCE-MSCN L-0+E-+0N L-0+E-+N L-0*E-*0\' L-0+E-+CN L-0+CE-+! L-0-* E-+0N L-0+ QE-+M L-C+E-+0N L-0+ E-*'tCN L-fc+E--tN L-0+E-+CN L-C+E-+CM L-C + E-CM0S L-0+CE-+CS L-0+E-+CS L-0+E-+0S L-0+E-+0S L-0E--HCS L-0+E-+S L-+0E-+0N L-+0E-+0N L-+0E- + 0N' L-+0E-+0N L-+0E-+80N L-+0F-+0N L-+0E-+N L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+DN L-+0E-+0N L-+0E-+CN L-+0E-+80N L-+E-+0N L-+E-+N L-+E--I-0N L-00E-+0N L-?*E-*SN L-+E-+0N L-+E-+0N L- + E--I-N L-+E-+0N L-fE-*0N L-+CE-+0N CC. C, C.?. s C.S C. C. C. C. f r* C C. CC. C. C. CC. 0. CC. < < ci ci ci ci ci ci ci ci ci ci ci c i ci ci ci c i ci c i ci ci c i C. CC CC CC C' c... CC C.l C C.I 0. D. 0. C.I C.l

91 X-RAY ASSAY LABRATRIES B-JUM- REPRT 800 REF.FILE 0- PAGE r SAMPLE TA?P" l! PPM TH PPM U PPM L-+E--KN L-+E-+N L-8+0E-00N L-8+0E-0N -8+0E-+0N L-+0E-+PN L-8+CE-+AN L-+-0E- + N L C E- + N L- + 0E-+C:; L-SS-i-GE-+CrM L-80G!I-u;M L-S+GE-+CM L-8+CCE-+CN L- + CE- + 0?, L-SetE-*0rj L--0CE-Z0N L-+-CE-+N L-+0E- + 0.N L-0E- R CN L-+0E-+SN L-+0E-+0N L-+0E-N L- 0E-+0M L-+0E-+0N L-+0E-+0M L-+0E-+0N L-+CE-+N L-0E-l*GfJ L-S'(-E-*G.kJ L-+CE-A+CN L-*CCE-At0N L-00E-+CN L-+E-+CN L-+E-00N L-00E-0J L-+0E-+0M L-+0E-B+N L-+0E- + 0N L-+0E-+0N L--0E-+SN L-+CE-+0N L-+CE-+N L-+CE-+CN L-+0E-0N L-+0E-A+0N L-+0E-+BN L-+0E-+AN L--0E-+N L-+CE-+SN <0. <0...s <0. l? <0.f <0. CC.. S <C. c. <a.. <0. <0. <G.... <0. *CC. <0. <0. <0. <0.. s r\ c S. xy t,j <G. <0.!i <0. 0. <C. <0. < f. *:e,s <0. <0. <0. <C. 0*.. <0. <0. *C0. <0. <0, <0. a *a <l i ti <l a <l ii i i *a i <l <l i <l <l <l i ci i <l <l <l <l <l 0.? r\ q w * Q. L C. 0. CD C S.S C , C.l 0. 0.

92 X-RAY ASSAY LABRATRIES -JUM-S REPRT 080 REF.FILE 0- PAGE GF SAMPLE TA PPM H PPM TH PPM U PPM L-CE-0N L-+E-800N L-+E-+0N L-+E-+0N L-+CE-SN L-+E-+0N L-+E-+0N L-00E-*r.\ L-00E-0CN L-+E-+0N L-+E-+CN L-&0CE-0N! L-0E-.',N L-QE-0CN L-0E-80N L-+0E-+0N L-+CE-0N L-+0E-+0N L-SE-0N L-+0E-+0N L-+0E-0N L-+0E-+0N L-CE-+0N L-+0E-0N L-+0E-+0N L-+0E-+0N L-0E-+0N L-+0E-0M L-+0E-+0N L-S+CE-+0N L-+0E-0+0N L-+0E-00N L-+0E-00S L-+0E-0+0N L-00E-8CN L-CE-8CN L-f E-+0M L-+E-+0N L-00E-0N L-00E-0N L-00E-QN L-00E-0N L-+E-0N L-0CE-0N L-00E-0N L-+E-A+0N L-QE-0N L-+E-+0N L-00E-0N L-00E-0N i"* t ** -i * CC. C. f* C.? c. s CC. CD. en. C. f CC. CC. ci '* <.. t* * T ,.0 0. C, C. 0. (C.I C 0. C.l CD C

93 X-RAY ASSAY LABRATRIES S-JUN-S REPRT 800 REF.FILE 0- PAGE F SAMPLE TA PPM W PPM T.H PPM 'J P 0 M L-+E-+0N -+E-+0N L-+E-+0N L-+E-0+0N L-+E-0+0N L-+DE-+lN L-+CE-0+0S L-+E-+0S L-+E-+0S L-+E-+0S L-+E-+0S L-+QE-+0S L-+E-+0S L-+E-+0S L-+0E-+0M L-A+0E-0N L-+-0E-+0N L-A+0E-+0N L-+0E-A+CN L-+0E-+0N L-+0E-+0N L-+0E-+0N L-A+0E-+CN L-A+0E-+0N L-+0E-+0N L- A+0E- + 0N L-+0E-+CN L-A+0E-0+0N L-+0E-0+0N L-A-f0E-0-i-0S L-A+0E-C+0S L-A+0E-0+0S L-A+0E-+0S L-A+E-8+0N L-+E-+0N L-A+E-+0N L-A+E-+0N L-A-i-E-fcf0N L-A+CE-A+CN L-A+E-A+0N L-A+E-A+0N L-A+E-+0N L-A+E-+0N L-+E-+0N L-A+E-+0N L-A+E-+0N L-A*E-l*0r-, L-A-E-0N L-A+E-0+0N L-A+E-C+CN <0. <0. <0. *:.s <0. <0. <0. <0.. <0. <0. <0. <C. *C0. <0. <C. CC. <0.. <0.. <0, <C.. <0. <0. <0. <0.. <0.. <0. <0. *C0. <0. <0. <0.. <0. <0. <0. <0.. *C0. <0. <0... <0. <l <l <l <l <l <l ci ci l , C.l C.l 0. ' C.l C.l 0. C.l

94 X-RAY ASSAY LABRATRIES 8-JUN-S REPRT 8080 REF.FILE 0- PAGE F SAMPLE TA PPM W PPM TH PPM U PPM L-+E-0+0N L-tE-0-i-0S L-+CE-0+0S L-+E-+0S L-+0E-8+DN L-+0E-8+0N L-+0E-+0N L-+0E-+0M L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-+0N L-+0E-0+0N L-+0E-0+0N L-+0E-0+0N L-+E-+0N L-+QE-+0N L-+E-8+0N L-+E-+0N L-+E-+0N L-+0E-+0S L-l +0E-+CS L-+0E-+CS L-+0E-+CS L-+0E-+0S L-+0E-+CS L-+0E-+0S L-+0E-+0S L-+E-+0S L-+E-+0S L- + E---0S L-+CE-+0S L-+E-+0S L-+CE-+0S L-+CE-+0S L- + 0E-H0S L-+0E-+S L-*0E-*'*S L-+0E-+0S L-+0E-+0S L-S+0E-+0S L-0E-+S L- + E-H-0S L-+E-+S L-+CE-+0S L-+E-+0S L-+E-+0S L-+E-+0S L-+E-+S <0. <C. <0.. <0.. <0. <0.. <0. <0. <0. <0.. s <0. <0. <0.? <C.. <C. <0. <0., <0. <G,. <C. (0. (0. (0. (0. (0. (. (0. (0. (0. (0. (0. (0. (0. (0. (0. (0. (0. (0. (0. (0. (0. (0. ( ( ( ( ( ( A. ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( 0.8 (0. 0. (0. (0. (0. ( ( (0. (0. (0. ( A (0. ( C.I , 0,

95 X-P.AY ASSAY LABRATRIES -JUN-S EPP.T 0S REF.FILE 0- PAGE S F SAMPLE TA P W PPM TH PPM u PPM L-+0E-0+0N L-+0E-0+ N L-l +0F-0+0S L-+0E-0+0S L-+0E-+0S L-+0E-+0S L-+E-0+0K L-+CE-0+0N L-0CE-0+0S L-+E-0+0S L-+CE-+0S L-fE-lCS L-+0E-0+0N L-l +0E-0+0N L-+GE-0+CS L-+CE-0+CS L-+0E-+CS L-+0E-+0S L-+E-0+0N L-+E-C+0N L-l f CE-0+0S L-+E-0+0S L-+E-+0S L-+E-+0S L-+E-+S L-+E-+0S L-+E-+0S L-+CE-+0S L-+E-S L-+E-+S L-+0E-+CS L-+0E-+0S L-+0E-+0S L-+0E-+GS L-+0E-+0S L-+CE-+S L-+CE-+0S L-+CE-+0S L-+CCE-+0S L-+E-+0S L-+0E-+S L-IUSE-Z + 'S L-+0E-+80S L-+0E-+0S L-+CE-0S, N TAG C. C. C0. r- 0. C. S u. r C r ' r~ C.. C C. C. C. c C. C.? CC. C. C. CD. L C. CC. CG. CC. CC. 0 ci ci ci ci -a i ci ci ci ci ci ci ci i ci l ci CC.. 0. G l.l C.l C.l

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102 GLDEN SHADW RESURCES INC. SURFACE CENTRAL PATRIA PRPERTRY PICKLE LAKE, DISTRICT F KENRA. (PATRIA PRTIN) NTARI Lngitudinal Sectin SPRINGER ( N.) VEIN Scale ; l inch t 0 feet -0. 0, 0 l ),,0 ) (0-,, -) 0-, 0, 0-0-,, ,, - ) (0-80, 0, - 0-, 8, - ) 0, 0, (0-, 0, - J -8 ( 0-, 8!, - LEGEND 0, 0, 80. STPE GRADE IN UNCES/TN, TNS MILLED, UNCES F GLD RECVERED..0 l ' ( ) QUARTZ VEIN GRADE VER WIDTH IN INCHES FEET -8 STPE NUMBER EG0

103 008 C cr UJ CL cr CL r CL i cr UJ Q LlJ Q ffi UJ C > w C : H CL V C LL) c/) tn UJ l C l p UJ C I in LJ v 00 0 K W

104 UJ r UJ in r UJ C\J r UJ in 00 r UJ r r UJ m r r UJ tf r UJ in sjt UJ in r 00 N i -z 0 0 N 080 \ N -G00\ S N LEGEND GRADIMETER MAGNETMETER - 00 N Gradimeter Determinatins Gammas per meters 0 Ttal Field in Gammas L Q?L' Cntur interval ez - se Instrument: IGS- System (008. Z-?,. 0 Q-& E GLDEN SHADW RESURCES INC CENTRAL PATR IA PRPERTY CNNELL TWP., DISTRICT F KENRA, PATRIA PRTIN - 0 b ALLAN CREEK GRID 0-08 n. Magnetic Surveys BASELINE JAMES E. TILSLEY a ASSATES LIMITED 0 m SCALE l: 0.0 DNA LAKE 80 (DM JUNE, 8

105 GLDEN SHADW RESURCES INC. LEGEND CENTRAL PAT R l A PRPERTY CNNELL TWP., DISTRICT F KE NRA, PATRIA PRTIN PICKLE CRW GRID - EAST SHEET GRADIMETER MAGNETMETER Magnetic Surveys Gradimeter Determinatins Gammas per meters S Ttal Field in Gammas JAMES E. TILSLEY a ASSATES LIMITED 0 m Cntur interval 0* SCALE l : 0 Instrument : IGS- System 00 N t 0 A j Alder Swamp 0? f fic(s f G\#) f 0 0 N f 0 A*a\ SW 00 N 0 0 f W l? 0 N h ' h? Q, S?8 C " ' l-. t 0 ( f CZ 0- l i ** 0 0 h *. "S f S- l- W? 0 BASELINE (00 0 BASELINE G 8 00 l G l 00 S 00 0 S LU r t LU in r t UJ *- t LU in t LU l t LU in m c UJ (D t LU l t U) LU N t LU If) N t LU 00 t LU If) 00 t LU 0 ( LU If) ) t LU N.0 DNA LAKE 0 JUNE IE

106 K 8 LEGEND 80 N '.A GRADIMETER Gradimeter Determinatins Gammas per meters MAGNETMETER Ttal Field in Gammas GLDEN SHADW RESURCES INC. CENTRAL PATRIA PRPERTY CNNELL TWP., DISTRICT F KENRA, PATRIA PRTIN PICKLE CRW GRID - CENTER SHEET JAMES E. TILSLEY S ASSATES LIMITED SN \qi -G\tqG \ l nstrument : IGS System 0 m SCALE l: 0 0 N 00 N 0-0 h \ 0 N (V S* *0 V - J N 0 0N f -- ill - \ Ml l \. 0 X \ 00 t,* 8 SN [ "0J - j- (.(0 -f-j IGS VI Y -Z-cni Z0 V L? lemfsz fcc- l- l IG 00 l 0 0 h f G G X V Q-I 0 l ' - i! h (0 0 0 ///' h GI V IR. (0*?-Z- BASELINE G0 II. - G 0 - -? 0G 0S l l j- -I b - 00 if - p?- 0 S G L Stf?i. ' G - G\t? 0e8NE00.0 DNA LAKE 00 JUNE,l

107 ( - GLDEN SHADW RESURCES INC. CENTRAL PAT R l ClA PRPERTY CNNELL TWP, DISTRICT F KENRA, PATRIA PRTIN PICKLE CRW GRID - WEST SHEET Magnetic Surveys JAMES E. TILSLEY 8 ASSATES LIMITED 0 m SCALE l : S? l*? LEGEND GRADIMETER MAGNETMETER Gradimeter Determinatins Gammas per meters # Ttal Field in Gammas f 00 ' Instrument: IGS- System 0 S UJ J in UJ in 00 in UJ/ r in UJ mr m UJ If) ST in UJ in in.0 DNA LAKE 0 JUNE, 8

108 C UJ C cr UJ Q- cr CL u cr Q : LU Z c C " C UJ t in 8 UJ C Q. cr UJ < Q. N I UJ -J C/) en UJ 008 0Z It*- l'** 0- = ir- 'S 'K -g NM HlMd G cu C

109 \ 8 fctlr Q UJ E C : UJ Q. a cc a. < v r r~ CL Q E LU GC ) c N I t UJ C C 0 UJ l C. z e, UJ : <. CJ UJ C LU (B *A LP 'S *. in - J- \s y w t(\- - T} C * tfi ) VS-?v IIP i i i- l- '-H J c* Hi!- i LL!! l \ 000 UJ UJ -J 0 W C '8.i

110 LJ r LU l r \JJ CM r LU in CVJ r LJ r r LU L r r LiJ SJr LJ L r UJ in r - 00 N 0 N 00 N 0 N LEGEND - KHz- Annaplis, Maryland In Phase Cntur interval 0 ' n ' Quadrature S Cnductr axis \0 t A -z-i- l t 0 )0I GLDEN SHADW RESURCES INC. CENTRAL PAIR l C l A PR P E R T Y CNNELL TWP, DISTRICT F KENRA, PATRIA" PRTIN" BASELINE ALLEN CREEK GRID VLF-EM Survey - KHz - Annaplis, Maryland JAMES E. TILSLEY S ASSATES LIMITED 0 m iff SCALE l. 0.sei DNA LAKE 0 UNE, 8

111 LJ r UJ in f LU CM r UJ m 00 r LJ r r UJ in r r UJ tf r LU mtr UJ in P 00 N 0 N 00 N LEGEND -0 KHz - Cutler, Maine. 0 N In Phase Quadrature Cntur interval 0 0X 00 N Cnductr axis 0 N GLDEN SHADW RESURCES INC CENTRAL PATRIA PRPERTY CNNELL TWP., DISTRICT F KENRA, PATRIA PRTIN ALLEN CREEK GRID BASELINE VLF-EM Survey -0 KHz - Cutler, Maine ' JAMES E- TILSLEY a ASSATES LIMITED m Si A. f l ; 0.seis DNA LAKE 0 H JUNE, 8

112 GLDEN SHADW RESURCES JNC. CENTRAL PATRIA PRPERTY LEGEND - KHz- Annaplis, Maryland PICKLE CRW GRID - EAST SHEET VLF- EM Survey - KHz - Annaplis, Maryland Jn JAMES E TILSLEY 8 ASSATES LIMITED In Phase Cntured at intervals Quadrature Cnductr axis c t- 00 N 0 N 00 N 0 N r C 8 V SN 0N 00 N BASELINE 00 S 00 0S 08NE008.8 DNA LAKE 0 JUNE

113 GLDEN SHADW RESURCES INC. CENTRAL PATRIA PRPERTY LEGEND -0 KHz - Cutler, Maine. PICKLE CRW GRID - EAST SHEET VLF-EIVI Survey -0 KHz - Cutler, Maine JAMES E. TILSLEY S ASSATES LIMITED In Phase Cntured at 0 Quadrature SCALE t : 0 m intervals Cnductr axis - 00 N 0 N 00 N 0 N 00 N 0N 00 N BASELINE { 00 BASELINE 00 S 00 0 S UJ r CD LU in r ID UJ ST C LU l d- C LJ m UJ C LLJ C CD UJ \n t LLJ N CD UJ in i CD LU 00 C LLJ m a CD LU en CD LU in ) CD LU 008NE000.0 DNA LAKE 0 JUNE 8

114 /S' 80 N In Phase Cntured at intervals LEGEND I- KHz - Annaplis, Maryland GLDEN SHADW RESURCES l N C. C E N TR AJ. PATRIA P R C P EJR TY CNNELL TWP, DISTRICT F K!' NRA, PATRIA PRTIN PICKLE CRW GRID - CENTER VLF-EM Survey I- KHz - Annaplis, Maryland SHEET JAMES E TILSLEY B. ASSATES LIMITED 800 N 0 N 00 N 0 N 00 N 0 N SN 0 N 00 N 0 N BASELINE 0 S.sais DNA LAKE 80 JL

115 LEGEND GLDEN SHADW RESURCES INC 80 N -0 KHz - Cutler, Maine. In Phase Cntured dt 0 'ntervals L TRW GPii - - CFNTIT.R SH'T JAMES E VLF-EM Survey -0 KHz - Cutler, Maine TILSLEY 8 ASSATES LIMITED SN CAL t 0 N r 00 N 0 N 00 N 0 N SN 0 N 00 N 0 N 00 N BASELINE 0 S.seis DNA LAKE 0 JUIS