E.W. Bazinet, P. Eng. Designated Consulting Engineer Dated At Toronto, Ontario September JO, 1988

Transcription

1 s DUFFELL LAKE 010 RK ON DIAMOND DRILLING PROGRAM ON PROPERTY OF NAPOLEON EXPLORATION CORPORATION MILNER CONSOLIDATED SILVER MINES LTD. AMOCO CANADA PETROLEUM COMPANY LTD. DUFFELL LAKE AREA SIOUX LOOKOUT MINING DIVISION ONTARIO E.W. Bazinet, P. Eng. Designated Consulting Engineer Dated At Toronto, Ontario September JO, 1988

2 TABLE ( in mini mi DUFFELL LAKE 0 10C 1. Summary 2. Introduction 3. Property and Location 4. History of Work Done Previously 5. Geology 6. Diamond Drilling Program and Results Diamond Drill Hole No. l Diamond Drill Hole No. 2 Diamond Drill Hole No. 3 Diamond Drill Hole No. 4 Diamond Drill Hole No. 5 Diamond Drill Hole No. 6 Diamond Drill Hole No. 7 Diamond Drill Hole No. 8 Diamond Drill Hole No Conclusions and Reconroendations 8. Appendix Diamond drill hole records complete with sampling and assaying records. Diamond drill hole numbers l to Maps Claim Location Map Drill Hole Location Maps General Geology Plan Location Map

3 REPORT ON DIAMOND DRILLING PROGRAM ON PROPERTY OF NAPOLEON EXPLORATION CORPORATION MILNER CONSOLIDATED SILVER MINES LTD. AMOCO CANADA PETROLEUM COMPANY LTD. DUFFELL LAKE AREA SIOUX LOOKOUT MINING DIVISION ONTARIO SUMMARY During June and July 1988, carried out a diamond drilling program on a claim group held under ^option from Airoco Canada tetroleum *53fl^wny ^f^ 'gi.ivemlts^j^ The property is located near Duffell Lake in the Sioux Lookout Mining Division approximately 13 miles southeast of the Golden Patricia gold deposit and is underlain by the same favourable greenstone belt that hosts the Golden Patricia. Napoleon can earn a 491 interest in the property by funding exploration programs on the property. This report contains an outline of the geology, the history of exploration carried out to - date on the property and the results of the diamond drilling program carried out on the property during the summer of Nine diamonded?!!! holes were completed on the property in the 1988 program totalling' 3435 feet. In total 121 drill core sections were sampled and assayed. In,general, these holes intersected well mineralized silicified porphyrys, shear zones and fault zones and in one hole sulfidic chert and iron formation. Encouraging gold values ware encountered in two of the drill holes (D.D.H. No. 9 and D.D.H. No. 4). It is recommended that limited additional geophysical programs be carried out in the immediate areas around D.D.H. No. 9 followed by additional diamond drilling to determine the extent and persistence of the gold values encountered in D.D.H. No. 9.

4 - 2 - During the months of June and July, 1988, a diamond drilling program was carried out by Napoleon Exploration Corporation on a claim group under option from Amoco Canada Petroleum Company Ltd. by Milner Consolidated Silver Mines Ltd. Milner can earn 1001 interest in the property, subject to a 2.51 net smelter return royalty. Napoleon entered into an agreement with Milner whereby it can earn a 49% interest in the property by funding exploration programs on the property. The purpose of the diamond drilling program was firstly to explore the overburden covered area "up - ice" from a spectacular basal till gold anomaly which had previously been outlined by Amoco, and secondly to explore anomalous features defined by ground geophysical surveys carried out in 1987, for economic concentrations of gold.

5 - 3- PROPERTY AND LOCATION The claim group consists of fourty-four claims totalling approximately 1,760 acres, situated on the Meen Lake - Kasagiminnis Lake greenstone belt. This belt is the westerly extension of the Pickle Lake greenstone belt. The claims are approximately 35 air miles west of the town of Pickle Lake. Access is by float or ski equipped charter aircraft or by winter road from Pickel Lake. The claims are shown on the Duffell Lake Area Claim map and are more precisely described as follows: Claim No Total: claims

6 - 4 - ESTORY OF WORK DONE PREVIOUSLY During the period between 1935 and 1938, the Pickle Crow Gold Mine and the Central Patricia Mine, both of which are located at the eastern end of the Pickle Lake - Meen - Dempster greenstone belt, were brought into production. More than 2 million ounces of gold were produced from these two mines before they closed in 1966 due to a static gold price and rising costs. Rising gold prices in the early 1980's caused a revival of exploration interest in the area and in the past several years at least 5 new deposits have been discovered along the belt, including Placer - Dome's Donna Lake Deposit, St. Joe Canada's Golden Patricia and Dobie Deposits, Umex's Dobie River Area Deposit and Lac Mineral's Hasaga Deposit. The Donna Lake deposit and the Golden Patricia are currently being prepared for production and work is proceeding towards expanding tonnage on the other above mentioned deposits, as well as on the former Central Patricia Mine and Pickle Crow Mine. The 44 claim Amoco group upon which the 1988 drill program was carried out was staked by Anoco in 1982 and 1983, after the Latter Company uncovered anomalous concentrations of gold in the Eskers in the area. Early in 1983, Amoco conducted a reverse circulation drilling program to test the basal till of the claim group for anomalous gold content. This work resulted in defining highly anomalous basal till in the east central sector of the property. The gold grains in the anomalous till are of extreme delicacy indicating a nearby bedrock source for the gold. Subsequently, Anoco bored seven diamond drill holes totalling 2400 feet which explored a 1400 feet section of bedrock up - ice from the centre of the anomalous till area. These holes did not intersect significant gold values and work was suspended but the claims were maintained in good standing. In 1986, Milner acquired an option from Anoco to earn a 100% interest in the claim group subject to a 2.51 net smelter royalty reserved to Amoco. Milner subsequently entered into an agreement with Napoleon whereby the latter company can earn a 491 interest in the claim group subject to the 2.5*1 royalty. In 1987, Napoleon funded line cutting, prospecting, geophysical and geological programs on the claim group. This work resulted in outlining of anomalous zones which were deemed to indicate geological features with the potential of hosting concentrations of gold. The 1988 diamond drilling program was carried out to explore the anomalous features outlined by the geophysical surveys and to extend Amoco's drilling cross section further up - ice in an attempt to locate the bedrock source of the gold in the basal till.

7 - 5 - The property is located along the Meen - Denpster Lake greenstone belt which is the westerly extension of the Pickle lake belt. Rocks consist of steeply dipping, folded and faulted netavolcanic and metasedimentary rocks which extend in a west to northwest direction. These rocks have been invaded by sills, dikes, stocks and bosses of ultramafic composition, gabbro, granite, granodiorite, diorite, quartz feldspar porphyry and diabase dikes. All of these rocks are of Archean age except for the diabase dikes which are younger. The belt is interpreted as beijig an isoclinal folded syncline possibly slightly overturned to the south. Gold in the region is known to occur in fissure quartz veins, in quartz vein stockworks in silicified shear zones with sulfides, in sulfidic iron formation, in sulfidized felsic tuffs, in green carbonates of exhalative origin, in banded chert zones of possible exhalative origin and as silicified sulfidic replacement zones in iron formation. Sulfide minerals, to a greater or lesser extent, frequently accompany the gold mineralization. The claim group is almost entirely underlain by a series of basic to intermediate metavolcanic flows and pyroclastic rocks. Ground geophysics and drilling reveal the presence of gabbro, diabase, and quartz - feldspar intrusive rocks. Diamond drilling also reveals the presence of sulfidic iron formation in the southeastern sector of the property. The Duffell Lake quartz monzonite stock intrudes the volcanic - sedimentary series in the east - central part of the property. Several shear zone - fault zones are indicated by geophysics and some of these are confirmed by diamond drilling.

8 - 6 - DRILLING PROGRAM AND RESULTS A diamond drilling program consisting of 9 holes totalling 3435 feet of B.Q. core was carried out. The purpose of the drilling was to explore the anomalous features outlined by the 1987 geophysical surveys and to extend Amoco's drilling cross section further "up - ice" in an attempt to locate the bedrock source of the gold in the basal till anomaly. Complete diamond drill hole logs and sample records for 121 drill core sections are submitted herein as appendix. A summary of the drill holes is as follows: DIAMOND DRILL HOLE NO. l This hole was bored to test Conductor H and to extend Amoco's drill section. Drilling encountered a sequence of brecciated basic volcanics mineralized with up to 101 pyrite. Numerous sections were well mineralized with blue - white quartz veinlets. Several silicified fractured quartz feldspar porphyry dikes, which were well mineralized with disseminated pyrite were encountered. Significant gold values were not intersected in the drill hole. DIAMOND DRILL HOLE NO. 2 This hole was drilled to explore Conductor G and to extend Amoco's drill section up - ice. Drilling intersected intermediate volcanics and quartz feldspar porphyry. The volcanics were locally sheared and well mineralized with pyrite including a short section of semi - massive pyrite at 31.5 feet. The porphyrys were fractured, silicified and sections were well mineralized with disseminated pyrite. A rusty bleached fracture zone was encountered at 76.5 feet possibly representing a fault zone. Anomalous gold values of 110 and 185 P.P.B. were encountered in a porphyry dike mineralized with S % disseminated pyrite. DIAMOND DRILL HOLE NO. 3 This hole was bored to test a magnetic low and to extend Amoco's drill section up - ice. Drilling encountered an intrusive porphyry or a porphyritic flow, gabbro and intrusive quartz feldspar porphyry. The porphyrys were well fractured, silicified and mineralized with disseminated pyrite. Significant gold values were not encountered. DIAMOND DRILL HOLE NO. 4 This hole was bored to extend Amoco's drill section up - ice. Drilling encountered basic volcanics intruded by feldspar - quartz

9 - 7 - porphyry dikes and an intrusive gabbro dike. The porphyry dikes were mineralized with up to 3% disseminated pyrite. A short section of basic volcanics (151.1 to 152.4) was mineralized with 10?; sulfides. An open bleached, vuggy, rusty fracture zone was encountered from 244 to 294 possibly representing a fault zone. Anomalous gold values of 108 and 140 P.P.B. were encountered in a fractured, silicified porphyry mineralized with disseminated pyrite. DIAMOND DRILL HOLE NO. 5 This hole was bored to extend Amooo's drill section up - ice. It encountered a sequence of basic volcanics intruded by feldspar porphyry dikes. The porphyry dikes are fractured, silicified and mineralized with disseminated pyrite. Ihe core was broken by a large number of luronite stained open fractures between 119 and 176 feet. Anomalous gold values of 426 P.P.B. were intersected in a fractured silicified porphyry mineralized with 2% disseminated pyrite. A section of basic volcanics mineralized with disseminated pyrite and quartz - carbonate veinlets yielded anomalous gold values of 212 P.P.B. DIAMOND DRILL HOLE NO. 6 This hole was bored to test Conductor F and to extend Amooo's drill section up - ice. It intersected a sequence of intermediate to basic tuffs and intermediate aglomerates. Abundant open fractures and vuggy sections were intersected possibly representing fault or fracture zone. Fairly abundant quartz carbonate stockwork zones mineralized with minor disseminated pyrite were encountered. A l foot section from 102 to 103 conposed of 401. quartz veinlets mineralized with 2% disseminated pyrite showed anomalous gold values of 226 P. P. B. DIAMOND DRILL HOLE NO. 7 hole was drilled to explore Conductor E. It intersected a broad carbonate zone, intruded by altered basic dikes. The carbonate zone is composed of carbonatized, sericitized bleached, locally hematized, buff coloured volcanic rocks. Many open fractures with fault gouge were encountered and the rock is locally porous and vuggy possibly representing a broad fault zone. Carbonatized rocks are locally silicified and mineralized with fine disseminated pyrite. Significant gold values were not encountered.

10 - 8 - DIAMOND DRILL HOLE NO. 8 This hole was drilled to explore a magnetic anomaly which was originally interpreted as being a possible iron formation band. Rock types intersected include gabbro, feldspar porphyry and a magnetite bearing diabase sill which is believed to represent the bedrock source of the magnetic anomaly. The porphyrys are locally mineralized with disseminated pyrite and cut by silicified fractures. Gold values of significance were not encountered. DIAMOND DRILL HOLE NO. 9 This hole was drilled to explore Conductor N which is an electromagnetic anomaly coincident with a magnetic anomaly which extends in an east southeasterly direction for a strike length of approximately 1400 feet on the Amoco claim group. The hole intersected a sequence of Tuff - Exhalite chert zones, magnetite iron formation, and mafic volcanics all of which are intruded by narrow feldspar porphyry dikes. Elevated gold values are associated with bands of semi - massive pyrite - pyrrhotite in the cherty Tuff - Exhalite zones as follows: From 89 to PPB gold From 96.2 to PPB gold From to PPB From 203 to PPB From to PPB (porphyry) From to PPB These values are not of economic grade but are significant in that they indicate a gold bearing sulfide rich strata with good exploration potential.

11 - 9 - CONCLUSIONS AND PBCCMMENDftTIONS 1. Anomalous gold values were intersected in drill holes up - ice from the basal till anomaly but these values do not appear to be the bedrock source of the basal till anomaly. The bedrock source of the till anomaly was not located in the 1988 drilling program. The best gold values up - ice were intersected in hole no Significant gold values intersected in hole no. 9 are associated with semi massive pyrite - pyrrhotite in an exhalite - iron formation - tuff environment. Conductor N which is coincident with a magnetic anomaly appears to define the auriferous sulfide zone. Hole no. 9 is down ice from the basal till anomaly and therefore cannot be the bedrock source of the till anomaly. It is recommended that additional geophysical programs be carried out in the immediate area around D.D.H. No. 9 followed by additional diamond drilling to determine the extent and persistence of the gold values encountered in this hole. Respectfully submitted, E.W. Bazipet, P. Eng. Designated Consulting Engineer Toronto, Ontario September 10, 1988

12 NAPOLEON EXPLORATION CORPORATION AMOCO PROJECT DIAVDND DRILL HOLE NO. l DUFFELL LAKE AREA SIOUX LOOKOUT MINING DIVISION ONTARIO Started: June 12, 1988 Completed: June 21, 1988 Location: 5 -f 13 W, O 4-42 N, 850 feet south and 140 feet west of post no. l claijm Pa Direction: N 40O E Dip: at collar * -45O, at 179' = 39ho, at 379' * 35HO Core Size: B.Q. O to 69 Overburden, sand, boulders, gravel. 69 to 70.3 Basic Volcanics; Dark green, fine grained, anphibolitized, chloritized, fractured with 25% silicification as narrow veinlets in fractures, 101; fine diss. crystals of crushed pyrite. C.A. = 52O 70.3 to 71.9 Basic Volcanics; Dark green, anphibolitized, fine grained, chloritic, 4% fine diss. pyrite, not silicified. C.A. = 52P 71.9 to 75 Brecciated Basic Volcanics; With 101 white brecciated quartz veinlets, abundant chlorite in fractures, 8% fine diss. crushed pyrite. 75 to 76.1 Basic Volcanics; As from 70.3 to 71.9, 3% fine pyrite to 77.8 Brecciated Basic Volcanics; With 20?; blue - white brecciated quartz veins, chloritic fractures, 10?; fine diss. crushed pyrite. C.A. = 54O 77.8 to 92.5 Basic Volcanics; As from 70.3 to 71.9, occasional silicified fractures, 31 fine diss. crushed pyrite throughout. C.A. = 55O predom to 94 Brecciated Basic Volcanics; 10% white quartz veinlets, microfolded, fractured, chloritic, 101 fine diss. crushed pyrite. 94 to 96.5 Basic Volcanics; Well fractured, chloritic, only local minor patches of silicification, 5?, fine diss. pyrite.

13 to 98.4 Brecciated Basic Volcanics; Fractured, irricrofolded, chloritized, 10% brecciated veinlets of blue - white quartz, 101 fine diss. crushed pyrite. C.A. = 530 predom to Basic Volcanics! As from 70.3 to 71.9, only minor diss. pyrite to Brecciated Basic Volcanics; With 201 Brecciated blue - white quartz veinlets, microfolded, chloritic, 61 fine diss. crushed pyrite crystals. C.A. = 46O predom to Basic Volcanics; As from 70.3 to 71.9, 51 blue - white quartz veinlets, only minor fine diss. pyrite to Quartz Vein; Blue - white, 5?; diss. pyrite and has plates in chloritic fractures. C.A. ^ 5 0O ( irregular ) to Brecciated Basic Volcanics; 201 brecciated, blue - white quartz veinlets, 41 diss. pyrite. C.A. = 39O predom to Basic Volcanics; As from 70.3 to 71.9, minor white quartz veinlets, minor diss. pyrite. C.A. ^ to 115 Brecciated Basic Volcanics; With 201 brecciated white quartz veinlets, microfolded, 31 diss. fine pyrite, chloritic. C.A. ^ 4 00 predom. 115 to Brecciated Basic Volcanics; Only minor diss. pyrite, chloritic. C.A. = 50 predom to Brecciated Basic Volcanics; With 20% brecciated blue - white quartz veinlets, chloritic, microfolded, 51 diss. crushed fine pyrite mainly in quartz veinlets. C.A. = 5 1 predom to Brecciated Basic Volcanics; As from to but with only minor quartz veinlets and minor diss. pyrite. C.A O predom.

14 to Brecciated Basic Volcanics; With 151; brecciated blue - white quartz veinlets, chloritic, 81 diss. crushed pyrite. C.A. = 4 3 predom to Brecciated Basic Volcanics: With 10?; brecciated blue - white quartz veins, chloritic in fractures, t d iss. fine crushed pyrite. C.A. = 6 1 predom to Basic Volcanics: As from 70.3 to 71.9, 2% fine diss. pyrite, occasional narrow quartz veinlet. C.A O predom to Silicified Zone; Bluish - grey silica 95?;, 5% fine diss. pyrite, brecciated, irregular sharp contacts at 600 predom. Possible fine grained phase of intrusive porphyry to Basic Volcanics, Argillaceous; Chloritic, soft, dark green, fractured, with minor white quartz veinlets, minor fine diss. pyrite throughout. C.A. = 4 4O predom to 193 Feldspar Porphyry; With grey - white feldspar phenocrysts in grey very hard siliceous matrix, minor fine diss pyrite, sharp irregular contacts at 193 to Basic Volcanics, Argillaceous; As from to 187.5, occasional narrow blue - white quartz veinlets with fine diss. pyrite, 2 diss. pyrite throughout. C.A. s 47 predom to Silicified Zone; Or fine grained phase of intrusive porphyry, grey, silicified, 45% blue- white secondary quartz veinlets in fractures, 101 fine diss. crushed pyrite in quartz. C.A. = 72O to 235 Basic Volcanics, Argillaceous; As from 193 to 211.8, minor diss. pyrite. 235 to Basic Volcanics; Amphlbolitized, dark green, locally chloritic with minor fine pyrite throughout. C.A. = 5 6O.

15 to Porphyry?; Grey, 70% quartz phenocrysts, 25% laths of green amphibole?, locally fractured with secondary quartz in fractures, 8% fine diss. pyrite sharp contact angle at 46O predom to 360 Basic Volcanics; As from 235 to 337.5, massive, only minor diss. pyrite. C.A. E to Porphyry; Quartz and feldspar phenocrysts, medium grained, hard, siliceous, minor diss. pyrite, finer grained near contacts due to chilling, contacts conform to schistocity of wall rock, contacts sharp at to 379 Basic Volcanics; As from 235 to 337.7, minor diss. fine pyrite throughout. C.A. = 55. End of Hole at 379'

16 SAMPLE RECORD NAPOLEON - AMOCO D.D.H. NO. l Sample No Feet From Feet To dore Length 1.3' 3.1' 1.7' 1.5' ' 5.2' 1.2' 1.8' 1.5' 4.0' 4.0' 3.7' 2.2' 5.5' 4.8' Gold PPB ( 5 86 ( 5 ( 5 Silver PPB iteans less than

17 NAPOLEON EXPLORATION CORPORATION AMOOO PROJECT DIAMOND DRILL. HOLE NO. 2. DUFFELL LAKE AREA SIOUX LOOKOUT MINING DIVISION ONTARIO Started: Completed: Location: Direction: Dip: Core Size: June 21, June 27, * 00 N, E, 1370 feet south and 210 feet west of no. l post claim Pa N 40 E' at collar -45, at 179' - 43**, at 370' * 44 B. Q. O to 20.7 Overburden, sand, gravel, boulders to 57.7 Intermediate Volcanics: Light green, amphibolitized, well fractured with narrow quartz veinlets, chloritic in fractures, locally bleached and locally silicified with porphyritic phenocryst development due to proximity to porphyry intrusive. Diss. pyrite throughout. Possible fault at ^6.5, rusty bleached fractures. C.A. s 41 predom. Best pyrite sections as follows: to 27.1 : 5% fine diss. pyrite, mainly in fractures. At " of 40?;, semi massive pyrite. 33 to 34 4?; diss. pyrite to 37 6* diss. pyrite to S; diss. pyrite. 49 to diss. pyrite to diss. pyrite to % diss. pyrite to 59.2 Feldspar Porphyry?; - Siliceous, grey, fine grained phase to Intermediate Volcanics: - As from 20.7 to 57.5, locally sheared. C.A. s 41 predom., diss. fine pyrite throughout. 63 to 65 to to 70 to 79.,3 to to 104.2to 109 to , % fine diss. pyrite. 3% fine diss. pyrite. 4% pyrite, in fractures mainly. 3% diss. pyrite. 4% diss. pyrite. 5% diss. pyrite. 3* diss. pyrite, silicified. 5S; pyrite, mainly as semi massive seams in shear planes. C.A. " 280

18 to 122 : 3% diss. pyrite to 125 Porphyry?; Fine grained phase, hard, siliceous, minor diss. pyrite, contacts irregular, sharp. 125 to Intermediate Volcanics; As from 59.2 to to 128 Porphyry?; Fine grained phase, 31 fine diss. pyrite throughout, siliceous, contacts irregular at 250 predom. 128 to Intermediate Volcanics; As from 125 to 126.8, C.A. ** 480 predom to Porphyry?; Fine trained phase, grey to locally pink, 3?; fine pyrite, hard, siliceous, contacts sharp at to Intermediate Volcanics; As from 128 to 129.4, short sections of up to 5% pyrite at 139, 148, 149, 151, 159, 162. C.A. very irregular 30O to 65O to 167 Porphyry; Fine grained phase, hard, siliceous, grey to locally pink, contacts sharp at 50, S 5* fine diss. pyrite throughout. 167 to Intermediate Volcanics; As from to 164.4, medium green, well fractured with white quartz filling fractures locally. C.A predom. Short sections with up to 5% diss. pyrite as follows; at 188, 211, to 225.4, C.A. - 15O predom to 389 Feldspar Porphyry; Dark grey, mainly fine grained, hard, siliceous, becoming medium to coarse grained towards 300' with light grey to white feldspar phenocrysts pp to 3/16 inches. From 340 becomes increasingly finer grained. Usually grey cherty appearance but locally pinkish in colour, diss. pyrite throughout. Shearing and fracturing prominent approaching contacts. Sericite in shear planes and slips. Contact angles sharp at feet = 20O.

19 - 3 - End of Hole at 389' Best pyrite sections as follows: to 274 4% diss. pyrite. 278 to diss. pyrite to 289 4% diss to diss. pyrite. pyrite. 329 l to % diss. pyrite to % diss. pyrite. Short sections up to 5% diss. pyrite at 333',337', 339.5', 344', 348', 352', 355' C.A. at 389' * 120.

20 SAMPLE RECORD NAPOLEON AMOCO D.D.H. NO. 2 Saitple No Feet From Feet To Core Length 6.4' 1.2' ' 6.6' 3.0' 2.0' 1.2' 1.0' 6.6' 2.8' 8.6' 10.5' ' Gold 5 ( " Silver PEJ3 CHECK ASSAYS NAPOLEON - AMOCO D.D.H. NO. 2 Sample No. Feet From Feet Tb Core Length Gold (ozs/ton) Silver (ozs/ton) ' ( means less than

21 NAPOLEON EXPLORATION CORPORATION AMOCO PROJECT DIAMOND DRILL HOLE NO. 3 DUFFELL LAKE AREA SIOUX LOOKOUT MINING DIVISION ONTARIO Started: Completed: Total Depth: Dip: Location: Direction: Core Size: O June 28, 1988 June 30, feet at collar 46O, i 179' - 379' = * 60 E, N. N 400 E B.Q. Overburden. Porphyritic Dacite Flow or Intrusive Porphyry. Grey to light green in colour, hard, siliceous, fine pyrite throughout, locally flow banding? well fractured with silica in fractures. O to 73: massive, siliceous, hard, medium grained. 73 to 88: flow banding? banded. 88 to 165: fine grained, less siliceous. 165 to 195: banded, flow banding? 14 to 22.6: B* pyrite cubes up to 3/16 inches to 31.2: 3* fine diss. pyrite to 61.3: 4S; fine diss. pyrite. 89 to 90.5: 3% diss. pyrite to 110.5: 3S; diss. pyrite. 119 to 129: 4 * diss. pyrite. 134 to 143: 6% diss. pyrite. C.A. e 80' - - IT0, e 180' * 16O. Coarse Grained Basic Volcanic Flow or Gabbro Dark green, fairly massive, rare diss. py. 195 to 219.2: fairly fine grained to 282.5: coarse grained up to 1/4 inch, gabbroic.

22 Feldspar Porphyry Grey to cream coloured, medium grained, hard, siliceous, 3% fine, diss pyrite. C.A. = 550 to Coarse Grained Basic Flow or Gabbro As from 195 to ' = 260. End of Hole at 379'

23 Sanple Record Napoleon Exploration Corp. D.D.H. No. 3 Sanple No. Feet From Feet To Core Length Gold PFB Silver PPB ( i GJ ( Means "Less Than"

24 NAPOLEON EXPLORATION CORPORATION AMOCO PROJECT DIAMOND DRILL HOLE NO. 4 DUFFELL LAKE AREA SIOUX LOOKOUT MINING DIVISION ONTARIO Started: July l, 1988 Completed: July 4, 1988 Total Depth: 379 feet Dip: at collar - 179' - 46O, g 379' - 4 5O. Location: E, 16 * 90 N. Direction: N 40O E. Core Size: B.Q. O -6.5 Overburden Basic Volcanics Dark green, amphibolitic, mainly fine grained, fairly well fractured with narrow guartz-calcite veinlets, possible bleached, epidotized pellowselvages? only minor pyrite throughout. C.A. = 200 to 400, variable Feldspar Porphyry Grey, fine grained phase, well fractured with white quartz veinlets in fractures, 31 diss. pyrite throughout, hard, siliceous, contacts sharp but ragged irregular at from 34O to Basic Volcanics As from O to 6.5, minor diss. pyrite Gabbro Dike Medium grained, dark green, mottled, medium grained, irregular sharp contacts at 15O predom Basic Volcanics Minor diss. pyrite, as from 6.5 to 16. C.A. variable at 420 predom to 152.4: 3*fe quartz carb with 101 blibs and coarse cryste.?s of pyrrhotite and pyrite, minor chalcopyrite Feldspar Porphyry Grey, fine grained to medium grained, hard, minor diss pyrite. C.A. = Basic Volcanics As from 6.5 to 16.

25 Feldspar Porphyry Grey, medium grained, 11; diss. fine pyrite, fine fractures with quartz filling, core angles irregular at from 45O to 70O Basic Volcanics As from O to 6.5, well fractured with quartzcarbonate veinlets, minor pyrite throughout. Predom C.A. = Feldspar Porphyry Grey, medium grained, rare fine pyrite. C.A. = Basic Volcanics As from to 206. End of Hole at 379' Core angle irregular. 244 to 249: open fracture zone, bleached, locally vuggy, rusty, fractures at 700 predom.

26 Sanple Record.Napoleon ExplorationCorp. D.D.H. No. 4 Sanple No. Feet From Feet To Core Length Gold PH3 Silver tr * tr * i.to l * Ozs per ton

27 NAPOLEON EXPLORATION CORPORATION AMOOO PROJECT DIAMOND DRILL HOLE NO. 5 DUFFELL LAKE AREA SIOUX LOOKOUT MINING DIVISION ONTARIO Started: July 4, 1988 Completed: July 6, 1988 Total Depth: 379 feet Dip: at collar = 179' ^ 42O, e 379' location: 18 -f 85 N, 9 * 70 E Direction: N 40O E Core Size: B.Q. O -19 Overburden, sand and gravel Basic Volcanics :, dark green, well fractured with quartz carbonate veinlets, only minor diss pyrite throughout, possible pillow selvages with quartz and biotite associated. Core angle irregular ~ 26 Feldspar Porphyry Fine grained phase, hard, siliceous, irregular sharp contacts at 45O to 7bO, 3% fine diss pyrite Basic Volcanics As from 19 to24.3, locally chloritic, fractured. 26 to 34: 30% quartz-carbonate with W diss. pyrite in fractures Feldspar Porphyry Hard, siliceous, occasional fractures filled with quartz veinlets mineralized with 2% fine diss. pyrite, sharp chilled contacts at 75O Basic Volcanics medium to dark~green, amphibolitized, fairly well fractured with 1-2" quartz and lesser carbonate veinlets in fractures, only minor diss pyrite and pyrrhotite throughout, abundant patches of brown biotite. 119 to 176: open fracture zone, oxidized with hemifite staining, core angle irregular at 450 predom. 225' well developed at 320.

28 to 76.4; 2* diss. pyrrhotite, pyrite. 119 to 129; 31 diss. pyrite, brecciated with 1(^ quartz-carbonate in fractures to 139.8; pink quartz veinlets at to 142.7; pink quartz veinlets, minor diss pyrite, C.A. ~ to 214; fractured, 301 white, irregular quartz veinlets with 4% coarse pyrite Feldspar Porphyry 3% fine diss pyrite, hard, siliceous, grey to pink, fractured with quartz in fractures. C.A. " 239 to Banded Tuff? or Banded Contact Phase of Porphyry? Minor pyrite in fractures. C.A ~ Basic Volcanics As from 61.3 to 226.5, possible pillow selvages. Predom. C.A. ^ 15O predom Feldspar Porphyry Fine to medium grained, phenorysts not well developed, well fractured with quartz filling, occasional vuggy quartz veinlets, It fine pyrite throughout. End of Hole at 379'

29 Sanple Iteoord Napoleon Exploration Corp. D.D.H. No. 5 Sanple No. Feet From Feet To Core Length Gold PPB Silver PFB, ? :.-: tr * tr *, * w tr *, * Ozs per ton

30 NAPOLEON EXPLORATION CORPORATION AMOOO PROJECT DIAMOND DRILL HOLE NO. 6 DUFFELL LAKE AREA SIOUX LOOKOUT MINING DIVISION ONTARIO Started: July 6, 1988 Completed: July 7, 1988 Total Depth: 409 feet Dip: at collar 199' ** 4 409' ^ 40O Location: N, 11 H- 35 E Direction: N 40O E Core Size: B.Q. O -80 Overburden, sand, gravel, boulders, basal till Intenrediate to Basic Tuff? and Agglomerate Light to dark green, abundant brown biotite in seams, abundant narrow white to pink quartz veinlets throughout at varied core angles with occasional pyrite cubes, well fractured, with many open fractures, rare cubic pyrite throughout. 102 to 103: mainly tuff, 40 ife quartz, 2 * diss. pyrite cubes. C.A. 70O predom. 108' = Gradational into Intermediate Agglomeratei at 1291*: 130 to 409: Abundant open fractures with quartz carbonate veinlets, and comb quartz with cubic pyrite in open fractures. 130 to 135: vuggy soft, core mostly ground to 152: 30% white quartz carbonate veinlets with l to 21 fine cubic 129': gradational into agglomerate. 205 to 206.5: glassy white quartz vein at 20O C.A. 229 to 231.1: 25% white quartz-carbonate veinlets at varied core angles to 277: 25^ vuggy white quartz-carbonate veinlets with minor diss. pyrite cubes in open vuggy and along open quartz fractures to 302.3: 251 vuggy comb quartz veinlets with fine diss cubes py veinlets at varied angles to 350.6: 351 white quartz carbonate veinlets

31 - 2 - End of Hole at 409' 389 to 398.5: 4(^ brecciated quartz carbonate veinlets, minor diss pyrite. C.A. - 35O predom to 403.5: 101 quartz-carbonate veinlets, ^ diss cubes of pyrite, minor chaloo. Core 145' - 215' * 285' " 350' ** 395' ~ 30O.

32 Sanple Record Napoleon Exploration Corp. D.D.H. No. 6 Sairple No. Feet From Feet To Core Length Gold PPB Silver PPB ( 5 ( 5 Cancelled i OJ l

33 NAPOLEON EXPLORATION CORPORATION AMOOO PROJECT DIAMOND DRILL HOLE NO. 7 SIOUX LOOKOUT MINING DIVISION ONTARIO Started: July 10, 1988 Completed: July 12, 1988 Location: N, E Direction: North Dip: e collar * 159' - 329' = - 37O Core Size: B.Q. O -86 Overburden, sand, gravel, boulders 81 to 86: excellent basal till In^termediate to Acid Volcanic, Carbonate Zone Bleached white, sericitized, heavily carbonated, locally pinkish colour, abundant open slips and fractures with porous rock sections, possible fault zone, slips locally contain hematite and fault gouge, locally minor cubic pyrite developed in vugs, fine grained, locally well fractured with white quartz in fractures and minor fine diss pyrite, silicification extends into wallrock Gabbro Dike Dark green, medium grained, fractured, porous, irregular sharp cilled contacts from 20O to 30O Carbonate Zone As from 86 to 87. Best sections of silicification with minor diss cubic pyrite are as follows: to to to to to to to to to Core 125' = 4 160' - 200' ' Intermediate Dike Green, fine grained, chilled contacts at 258', conformable, contact at 292' is ragged and cuts across schistocity, rare cubes of pyrite, becoming coarser grained with feldspar phenocrysts developed

34 - 2 - towards centre, well fractured with white quartzcarbonate veins in fractures. Predon C.A. = Carbonate Zone As from 86 to 87', core angle at 300' = 45O,. silicified section, 292 to best Gabbro Dike Altered, porous, vuggy, contacts cut schistocity of wall rock at 30O core axis Carbonate Zone As from 86 to 87', hematite in fractures. C.A. s Gabbro Dike Altered vuggy as from 324 to 329.5' Carbonate Zone As from 86 to 87', hematite stained open fracture. C.A. = 4 30 predom. End of Hole at 339'

35 Sample Iteoord Napoleon Amoco D.D.H. No. 7 Sanple No. Feet From Feet T\o Pore Length Gold PPB silver PPB i w l

36 NAPOLEON EXPLORATION CORPORATION AMOCO PROJECT DIAMOND DRILL HOIS NO. 8 SIOUX LOOKOUT MINING DIVISION ONTARIO Started: July 13, 1988 Completed: July 16, 1988 location: E, 35 * 25 N Direction: North Dip: at collar - 200' - 394' * - 38O Dore Size: B.Q. O Overburden, sand, gravel, boulders Gabbro or Coarse Grained Basic Volcanics Green, frequent fractures at 25Q predom with carbonate filling, locally epidote in fractures, occasional quartz patches, rare crystals of magnetite, rare narrow quartz veinlets to 96.8: grey quartz veinlets at 270 predom. 165 to 184.5: open rusty fractures at varied angles. 184 to 184.5: fault zone, fault gouge Feldspar Poryphyry Hard, very siliceous, mainly fire grained with small poorly developed feldspar phencrysts, grey to locally pink, well fractured with quartz in fractures, frequent open liironitic fractures, spec of native copper in fracture at 185.7, rare diss. py. in quartz veinlets, contacts chilled at 52, sampled from to 193, 193 to Gabbro or Coarse Grained Basic Flow As from 26.6 to but not as coarse grained Feldspar Poryphyry As from to to 290.2: feldspar phenocrysts are well developed, well fractured with nany open linonitic fractures, contacts sharp but irregular at approx. 45O, hard, siliceous but fractures are not silicified, no visible sulfides Gabbro or Coarse Grained Basic Flow As from 26.6 to but becoming progressively finer grained towards 294'.

37 Diabase Sill Medium grained, dark green, contact angle at 294' sharp at 59O, fine diss magneitie, fairly magnetic Feldspar Porphyry As from to , sharp contacts at 35O to 520, fractured with thin quartz veinlets in fractures, l to 2Ss diss pyrite throughout White Quartz Vein At 360, not mineralized Diabase As from 294 to 322.6, some fine diss magnetite, magnetic. End of Hole at 394'

38 Sairple Record Napoleon - ftroooo P.P. H. No. 8 Semple No. Feet From Feet To Core length Gold Silver PFB i w

39 NAPOLEON EXPLORATION CORPORATION AMOCO PROJECT DIAMOND DRILL HOLE NO. 9 SIOUX LOOKOUT MINING DIVISION ONTARIO Started: Completed: Location: Direction: Dip: Core Size: O JUly 17, 1988 July 19, S, W North at collar - -45C 179' B.Q. Overburden, sand and ocassional small boulders. Tuff Exhalite Zone, Banded Chert and fimph ibolite Approx. 20% thin bands of bluish chert : alb alternating with dark green amphibole bands, 10i white quartzcarbonate bands, minor diss pyrite throughout, frequent thin bands of semi-massive pyrrhotite and pyrite up to 1/8 inches, locally garnets. 89 to 90: 25% bands of mainly semi-massive pyrite, and minor pyrrhotite to 104: 5% thin bands of semi-massive pyrrhotite to 113: 3% thin bands of semi-massive pyrrhotite and minor pyrite, from 109 to 110 white quartz vein at 16O with minor pyrrhotite patches. 131 to 139: 41 diss and thin semi-massive pyrrhotite and lesser pyrite Gabbro or Coarse Grained Mafic Flow Dark green, fractured with abundant veinlets of white carbonate, minor diss pyrrhotite usually associated with biotite rich seams, at 184' becoming fine grained. 198' o Feldspar Po: or lyritized Chert Grey, medium grained, feldspar phenocrysts poorly developed, very siliceous, minor diss pyrite Tuff-ExhaUte tone, Alternating Banded Chert 70% and Banded Amphibole Locally grunerite, locally fractured with massive pyrrhotite veins up to l" and as lesser semimassive bands of pyrite, average 251 sulfides,.' '-if' M

40 - 2 - abundant garnets, locally thin bands of massive magnetite Feldspar Porphyry As from to 203, contacts at 63O Tuff-Exhalibe Zone As from 203 to 210.4, 81 pyrite-pyrrhotite in fractures and as bands of semi-massive sulfides. C.A. = Basic luff Dark green, banded, fine grained, mainly amphibolite, fairly well fractured with white carbonate veinlets in fractures, chloritic to 235.1: fractured, with 101 pyrite as massive bands and fracture filling. C.A. - 61O Banded Chert~Magnetite-(arunerite Iron Formation Locally vuggy carbonate bands, some actinolite rich bands, locally splashes of pyrite and ocassional specs of chalcopyrite.c.a..- 62O Basic Volcanics Massive, dark green Banded ^ertksrunerite-amphibple 10?. pyrite, vuggy. C.A. * 63O Basic Tuff As from 215 to Chert Grey, some garnets developed, rare specs of pyrite, fractured with secondary silicification in fractures. Core Angles; 630' - 60' - 140' ~ 57", i ISO' Basic Tuff As from 215 to 235.1, occasional thin chert band, rare diss pyrite, biotite rich seams locally. 267 to 278: talc rich, broken, several slips containing talcose fault gouge. 260' B 280' Basic Volcanics Fairly massive dark green, fine grained, fractured with quartz-carbonate in fractures. C.A. e 298' - 65.

41 Basic Banded, locally thin chert bands, chloritic bands. C. 350' Exhalite Zone/ Banded Chert and Arophibole Grey-green, chloritic, feactured with secondary quartz in fractures, extremely rare specs of pyrite. C.A. at Exhalite -Tuff Zone Up to 25% thin bands of chert alternating with amphibole bands, rare fine diss pyrite Basic Volcanics Grey-green, fractured with quartz veins at from 200 to 300 core axis. 378 to 379: 60S; quartz veins mineralized with 21. diss pyrite Exhalite -Tuff Zone With up to 301 bands of chert alternating with amphibole bands, only rare specs of pyrrhotite and pyrite, locally chloritic. C.A. B 670. End of Hole at 388'

42 ... 'X' "..-" ~ Anxxo D.D.H. NO. 9 Sairple No. Feet From Feet To Pore Length Gold PEB Silver tr * * 2.5 tr * 10.0 tr * * 9.4 tr * 3.1 tr * 3.4 tr * * Ozs per ton

43 Check Assays Napoleon - fttoco D.D.H. No. 9 Sanple No. Feet From Feet To Pore Length Gold (ozs per ton) Silver (ozs per ton)

44 KORTHWESTERN ONTARIO, LOCATION MAP ^ *tf' NAPOLEON PETROLEUM CORPORATION - - L E C EH D [T l' l'l WLEOZOIC PRECAMBRIAN EXISTING ROADS PROPOSED ftailway

45 ^^33 4 * \ ^4 \ O^ IF.' fer1 /v-'.^ ^ '/' 11)i **^~ "- ~^l 1 \ ^,'J/f 9 t~^fzfi \ ^ A l PROPERTY M W \! v^ X/V ^ -\ r*. */^ ^L*** ^sr^~^ _. Leg*nd 1*1 GRANITE I * I MIGMATITE i * l METASEDiMEflTS [ * l FELSIC TO INTERMEDIATE METAVOCCANICS I ' J MAFIC TO INTERMEDIATE METAVOLCANICS ^ IRON FORMATION f^. 4** MINERAL OCCURRENCE 'WngM.Cote -ST. ^s-. PROPERTY l Knupp LO** tp iott 'Whi Late C f ir Lone ^ r 4 mitt 'Pickle ir N.**0fl ^' r^y l x. ^^-^^.^ '- MILES OuffefLofie4 Stock LA K f 0^ 5T. JOSEPH GENERAL GEOLOGY ANQ PROPERTY LOCATION MAP NAPOLEON PETROLEUM CORPORATION MEEN - OEMPSTER LAKES AREA MTMCIA MINING DIVISION, OfSTHlCT OF KENORA ONTARIO

46 f Pickle Lakl \ DuffeHLoke Stock GENERAL GEOLOGY PROPERTY LOCATION MAP NAPOLEON PETROLEUM CORPORATION MEEN - DEMPSTER LAKES AREA PATRICIA MINING DIVISION, DISTRICT OF KENORA ONTARIO

47 Legend L xxxxx *^*^. AREA COVERED BY RC DRILLING PROGRAM (AMOCO) GROUND GEOPHYSICAL CONDUCTOR ASSUMED GEOLOGICAL CONTACT SECTION FOR AMOCO DIAMOND DRILL HOLES Not f^ APRIL 1987 * 8 \ * i 0.3 MILE *? M K) \ l to n o S w tf.s \ ^-4. Duffell Lake GENERAL GEOLOGY a GEOPHYSICAL COMPILATION MAP NAPOLEON PETROLEUM CORPORATION DUFFELL LAKE AREA.PATRICIA MINING DIVISION, DISTRICT OF KENORA ONTARIO

48 Kominogant ' Lot* Out tt II LaKt CLAIMS LOCATION MAP PETROLEUM CORPORATION DUFFELL LAKE AREA PATRICIA MINING DIVISION, DISTRICT OF KENORA ONTARIO

49 Kowinogont,- Lokt Duff ill Lo k t CLAIMS LOCATION MAP NAFfOLEON PETROLEUM CORPORATION DUFFELL LAKE AREA PATRICIA MINING DIVISION, DISTRICT OF KENORA ONTARIO

50 ACCURASSAY UVBORATORIES LTD. P.O. BOX 604 KIRKLAND LAKE, ONTARIO, CANADA TEL.: (706) P2N 3J5 President: Dr. GEORGE DUNCAN. M se. P* o. c err i.o.n.i, c U.K i, v.c.i c... M. R s c. A R c s t Certificate of Analysis Mr. E, V. Bazinet 1 Q1 R4 Napoleon Exploration Corp. k ^'LOH SS3 Site 6 Camp 20 Penetang, Ontario Date: Vork Order # Project P Page: l 19 8S SAMPLE NUMBERS Accurassay Ci 'mer Gold ppb 226 9^ ( Check Check Per:

51 19165 ACCURASSAY UBORATORIES LTD. P.O. BOX 604 KIRKLAND LAKE, ONTARIO, CANADA TEL.: (705) P2N 3J5 President; Dr, GEORGE DUNCAN, M.SC, Ph c. c oer- tot t c o**~ 'U K,. ve, c., M. R s c *.R C.S.T Certificate of Analysis Mr. E. V, Bazinet Napoleon Exploration Corp. SS3 Site 6 Camp 20 Penetang, Ontario SAMPLE NUMBERS Accurassay Customer Gold ppb Check 7 ^86 5 ( Check U 12 Check Date: Vork Order Project P Page Per:

52 ACCURASSAY LABORATORIES LTD. P.O. BOX 604 KIRKLAND LAKE, ONTARIO, CANADA TEL.: (705) P2N 3J5 President: Dr. GEORGE DUNCAN, M.SC. PH. o c, c***-, ior,t' c o*r iu.*.'. v c i c. M.R.S.C, A o c s; Certificote of Analysis Mr. E. V. Bazinet Napoleon Exploration Corp. Penetang, Ontario SAMPLE NUMBERS Accurassay Customer Gold ppb Check Check Check 21 Date: Work Order Project P Page: 2 Per:

53 ACCURASSAY UBORATORIES LTD. P.O. BOX 604 KIRKLAND LAKE, ONTARIO, CANADA TEL.: (705) P2N 3J5 President: Dr. GEORGE DUNCAN, M.SC, "v D c, cr..r-, 10*... c Cher : \j\ i. w c.i.c.. w s.s c, A a.c s Certificate of Rnolysis Mr. E, V. Bazinet Napoleon Exploration Corp. SS3 S ite 6 CM, P 20 Penetang, Ontario SAMPLE NUMBERS Accurassay Customer Gold ppb Check Page; Date:.July-20 Work Order # : Project P Pdr:......

54 Napoleon - Anoco D.D.H. #1 Vertical Section Scale l inch = 50 feet

55 NE Napoleon - AITOCO D.D.H. #2 Vertical Section Scale l inch ^ 50 feet

56 Surface Napoleon - Amoco D.D.H. #3 Vertical Section Scale l inch s 50 feet

57 Napoleon - Anoco D.D.H #4 Vertical Section Scale l inch ~ 50 feet

58 Napoleon - Anoco D.D.H. #5 Vertical Section Scale l inch ** 50 feet

59 Surface NE Napoleon - Anoco D.D.H. #6 Vertical Section Scale l inch = 50 feet

60 Surface - N Napoleon - Arnoco D.D.H #7 Vertical Section Scale l inch ^ 50 feet

61 Napoleon - Amooo D.D.H. #8 Vertical Section Scale l inch ** 50 feet

62 Napoleon - Aniooo D.D.H. #9 Vertical Section Scale l inch * 50 feet

63 N Post #4 Post # 1 Pa D.D.H 41 Post #3 Post #2 D.D.H. location Map Scale l inch = 200'

64 Pa D.D.H. No. 7 N Pa Pa D.D.H. Location Map Scale l inch ** 200'

65 D.D.H. No D.D.H Location Map Scale l inch = 200'

66 Post #1 D.D.H. Location Map Scale l inch = 200' Claim Pa D.D.H. #9 Post #2