Vivian Township Thunder Bay Mining Division · PDF fileVivian Township Thunder Bay Mining...

t48E11NW02ea 2.11038 VIVIAN 010

Report on

GEOLOGICAL. GEOCHEMICAL AND GEOPHYSICAL SURVEYS

on the

TB875326-3Mf MINING CLAIMS

Vivian Township

Thunder Bay Mining Division

Ontario

M.S. MORRISON, B.Se.

Kelowna, B.C. February 20, 1988

t42E11NW82aa 2.11838 VIVIAN 010C

PAGE

Suraraary ..................................*............ 1

Introduction ..............................*..........* J)

Location, Access, Topography, Vegetation b Climate .... 5

Mineral Property ..*................................... 7

History ...*........................................... 7

Regional Geology and Mineralization ................... 8

Surveys ............................................... 12

Grid .............................................. 12

VLF-EM 16 Ground Survey .......................... 12

Geochemical Survey ...... *........................ 13

Geological Mapping ................ *.............. 14

Property Geology ...................................... 15

Summary .......................**................. 15

Unit 1 Lower Metasediments ..................... 15

Unit 2 Mafic Metavolcanics ..................... 16

Unit 3 Mafic to Intermediate Metavolcanics ..... 18

Unit 4 Metasediments ........................*.. 18

Unit 5 Trondhjemite Intrusive .................. 19

IF Iron Formation .......................... 19

Structural Geology and Faulting ... *................... 20

Mineralization ...............................*... 21

Quartz veins with Arsenopyrite ........ *..... 21

Sulphide Mineralization Associated withIron Formation ....... *.................. *..* 22General Iron Formation ............... *...... 22

Continued . . .

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TABLE OF CONTENTS - CONTINUED

PAGE

Discussion ............................................ 23

Geology ......................*...*.........*..... 23

Geochemical Survey ............ *.................. 24

Gold Geochem in Soils ....................... 24

Arsenic Geochem in Soils .................. *. 24

Lead Geochem in Soils ....................... 25

Iron Geochem in Soils ....................... 26

VLF-EM Ground Survey ............................. 26

Summary of All Surveys ........................... 29

Conclusions and Recommendations .......... *..*...*..... 30

Summary of Initial Trenching Locations ................ 31

References .......................................t..*. 33

Appendix "A" Statement of Qualifications ............ 34

Appendix "B" Geochemical ICP Analysis ............... 35

Appendix "C" Geochemical/Assay Certificate .......... 40

Appendix "D" Laboratory Costs ....................... 41

Appendix "E" Technical Data Statement .........,..... 42

ILLUSTRATIONS

Location -Vivian Township Property Figure 1 ...... 4

Location, Access k Claims - VivianTownship Property Figure 2 ...... 6

Regional Geology, Beardmore -Geraldton Area Figure 3 ...*.. 9

General Geology - Vivian TownshipProperty Figure 4 ...... 10

Continued * .

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TABLE OF CONTENTS - CONTINUED

ILLUSTRATIONS - CONTINUED

Geology ........................... Maps V-88-3A&B .. in pocketMineral Claims TB 875326-344

VLF-EM Survey...................... Maps V-88-4A&B .. in pocketFraser Filtered Data Mineral Claims TB 875326-344

VLF-EM Survey...................... Maps V-88-5A&B .. in pocketBasic Data k Profiles Mineral Claims TB 875326-344

Geochemical Survey................. Map V-88-6B ..... in pocketGold and Arsenic in Soil Mineral Claims TB 875326-328&341

Geochemical Survey................. Map V-88-7B ...,. in pocketLead and Iron In SoilMineral Claims TB 875326-328&341

Ground Magnetic Survey............. Maps V-87-2A&B ,. in pocketInterpretationMineral Claims TB 875326-344 (February, 1987 Survey)

SSUMMARY

The Vivian Township Property is comprised of 19 mineral claims situated at the northwest corner of Vivian Township, 25 km west-southwest of Geraldton, Ontario in the Thunder Bay Mining Division. The property, 100# owned by the writer, M. Morrison of Kelowna, B.C., was staked in 1986 to cover a 3 kilometre segment of the Southern Mafic Volcanic Belt of the Beardmore- Geraldton Archean Fold Belt. The Beardmore-Geraldton Gold Camps produced l+.'i million ounces of gold over a period of 50 years.

The Southern Mafic Volcanic Belt hosts the Northern Empire Mine at Beardmore (160,000 ounces of gold produced from 1934-41) as well as several important gold prospects. The Maki, Pichette, and Craskie-Vega prospects all lying within the Southern Mafic Volcanic Belt have yielded assays of 0.1? to 0.40 ounces of gold per ton over substantial widths. Recent exploration at the Northern Empire Mine has outlined a zone of stratabound sulphide mineralization in iron formation with a grade of 9*56 g

per tonne (uncut), and dimensions of 175 m x 2.7 m x 250 m in depth (still open) (Northern Miner, March 9, 1987, p. B8).

Government aeromagnetic and geological maps indicate that the iron formation horizons of the Southern Mafic Volcanic Belt extend from the Summers, McComber and Vincent Townships of the Beardmore Gold Camp 20 to 40 km east to Vivian Township.

A ground magnetometer survey conducted over the Vivian Town ship property in February 1987 was successful in delineating several iron formation horizons occurring with intercalated sediments within mafic metavolcanic flow sequences. The mode of occurrence of the iron formation was confirmed during a September, 1987 geological mapping program. Arsenopyrite- bearing quartz veins associated with a trondhjemite intrusive, and iron sulphide replacements of iron formation were also discovered during the mapping program.

Continued . . .

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SUMMARY - Continued

An experimental soil geochemical survey conducted over four mineral claims in September, 1987 was of limited success, while a VLF-EM ground survey, conducted at the same time, proved useful in outlining several conductors associated with iron formation horizons or highly foliated, mineralized metavolcanic rocks.

The combined magnetometer and VLF-EM surveys indicate that some of the mineralized zones found on the property may have great lineal extent, and a detailed prospecting and trench ing program is recommended.

The ultimate target for exploration on the Vivian Township property is a gold-bearing zone of strataform sulphide mineral ization similar to the one recently discovered at the old Northern Empire Mine mentioned earlier.

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INTRODUCTION

During September-October 1987 the writer conducted a program of geological mapping and VLF-EM and geochemical surveying on a group of 19 mineral claims situated at the northwest corner of Vivian Township in the Thunder Bay Mining Division. The group of claims, herein called the "Vivian Township Property", is located 25 kilometres west-southwest of Geraldton, Ontario.

Aeromagnetic Maps by the Ontario Division of Mines (ODM) and the Geological Survey of Canada (GSC), and geological mapping by the ODM indicate that the iron formation horizons known to be auriferous in the Summers, Mccomber and Vincent Townships of the well-known Beardmore Gold Camp can be traced 20 to M) kilometres easterly to Legault, Colter and Vivian Townships. The Vivian Township property was staked by the writer in 1986 to cover a 3 km segment of an aeromagnetic high thought to represent iron formation horizons within a mafic metavolcanic belt of rocks. The mineral claims, owned by the writer, were recorded in Thunder Bay, Ontario, February 26, 1986.

The 1987 autumn exploration program was designed to evaluate the gold-bearing potential of the property. The results of the program are discussed within this report, while the data obtained from the surveys is displayed on several large scale geological, geochemical, and VLF-EM maps accompanying this report.

t

GERALDTON TOWNSHIP

FIGURE 1 - LOCATION - VIVIAN TOWNSHIP PROPERTY

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LOCATION. ACCESS. TOPOGRAPHY r VEGETATION AND CLIMATE

The Vivian Township property (Mineral Claims TB8?5326-3Mf) is situated at the northwest corner of Vivian Township, 25 km west- southwest of Geraldton, Ontario (Lat. 49*39'; Long. 87*19'; N.T.S. 42-E-11W).

Geraldton, a village of 3100 people, lies on a branch line of the Canadian National Railway, just 5 km north of Highway 11. The village is serviced by scheduled aircraft, and is a suitable supply centre for most exploration requirements.

The Vivian Township property lies 4 km south of Highway 11, and may be reached via the Sturgeon River Logging Road, a gravel road jointly maintained by the Ministry of Natural Resources and Domtar. The gravel road passes through the westernmost claims of the property, while an old logging road (partially grown over with alders) passes through the easternmost claims (please see figure 2).

The property features gentle relief with the main creek valley seldom cutting more than 15 metres into the peneplain surface which averages 350 metres in elevation above sea level. Glacial gravels form a thin cover over much of the property, and natural rock exposures equal approximately 10# in area across the property.

A thick new forest of spruce, balsam, poplar and pine replaces a forest logged for pulpwood some 30 to 40 years ago. Black spruce and some cedar are dominant in the large muskeg areas crossing the centre of the property and at the northeast corner of the property. Willow and alder underbrush are locally dense in low-lying regions.

The climate is typical of that of Northern Ontario with warm, often muggy summers, and cold winters. : Temperature extremes

Continued . . .

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l JELLICOE 17.3 KM -* GERALDTON 27.7 KM

COLTERWPVIVIAN TWP

0l —0

2000 4000 ——— \ ————— , ——1

6000 FT ——— l2 KM

MINERAL CLAIMS PREFIX i TB875-

FIGURE 2 - LOCATION, ACCESS ft CLAIMS

VIVIAN TOWNSHIP PROPERTY

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LOCATION. ACCESS. TOPOGRAPHY. VEGETATION MD CLIMATE - Continued

range from +30 to -45 degrees Celsius. The winter snow starts to accumulate in early November, and lingers in the bush until mid to late April. A winter snowpack of i to 1 metre is common.

MINERAL PROPERTY

Mineral Claims TB875326-344 make up the 19 claim Vivian Township Property. The claims all lie within Vivian Township in the Thunder Bay Mining Division. The claims are owned by the writer, Mr. M. Morrison of Kelowna, B.C. They were staked by the writer in February 1986 and recorded in Thunder Bay on February 26, 1986.

The acceptance of this assessment report will maintain all 19 mineral claims in good standing until February 26, 19&9.

HISTORY

There is very little evidence of past exploration work having been conducted on the Vivian Township property. Two small pits (pits A and B on Map V-87-3B) have been blasted into replacement zones of massive pyrrhotite on ground now covered by mineral claim 875326, but no attempt was made to explore the replacement zones along strike. The pits measure 1 to 2 metres in dimension.

The northern two-thirds of the present Vivian Township Property was the target of an airborne magnetic and electromagnetic sur vey by Aerodat Ltd. (Hogg, 1983) for Alclare Resources of Vancouver in 1983. The survey was filed for assessment purposes with the Ministry of Northern development and Mines, but no follow-up work was ever carried out.

A ground magnetometer survey conducted by the writer on the property in February, 1987 has also been submitted to the Ministry of Northern Development and Mines,

Continued...

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REGIONAL GEOLOGY AND MINERALIZATION

The Beardmore-Geraldton area lies at the southern boundary of the east-trending, isoclinally folded Early Precambrian metavolcanic-metasedimentary sequence of the Wabigoon Subprovince, a linear subdivision of the Superior structual province of the Canadian Shield (Mason, Mcconnell, 1983).

The Beardmore-Geraldton district has yielded 4.1 million ounces of gold over a mining life of 50 years, and has just recently become an area of renewed exploration activity. Many of the gold mines in the district are associated with isoclinally folded metasediments and iron formation lying in close proxim ity to mafic metavolcanic units. Shearing and drag folding are believed to be necessary for "ground preparation" for the em placement of gold-bearing epigenetic quartz and/or carbonate veins at most mine sites. Chemical replacement of magnetite iron formation by sulphides of iron (bearing gold values) is also widespread throughout the district, and considered an im portant feature of the "ore making process." Such replacement ores occur at the well-known MacLeod-Cockshutt and Hard Rock Mines at Geraldton.

Figure 3 (reproduced from Mason and Mcconnell, 1983, with slight additions) illustrates the main geological formations of the Beardmore-Geraldton region. The Vivian Township prop erty covers a 3 km segment of the "Southern Mafic Volcanic Dominated Belt" extending from Lake Nipigon west of Beardmore to Long Lac east of Geraldton.

The Southern Mafic Volcanic Dominated Belt is made up of an intermediate to mafic metavolcanic sequence consisting of mas sive and pillowed amygdaloidal flows, mafic tuffs, felsic to mafic intrusions and/or coarse flow rocks (Mason and Mcconnell, 1983). Ironstone units occur within the volcanic sequence.

Continued . . .

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GOLD MINERALIZATION IN THE BEARDMORE-GERALDTON AREA

' ' V IVIAN TOWNSHIP PROPERTY

SOUTHERN MAFIC VOLCANIC DOMINATED BELT

O 10 kilemttrtl

PttWT L*(t f MILT

m GOLD DEPOSIT TYPES DESCRIBED IN THE TEXT

COPIED FROM' MASON AND MCCONNEL . 1983 (SEE REFERENCES)

Figure 1. Geology of the Beardmore-Geraldton area.

1. Solomon's Pillars Prospect (Oremond Prospect)2. Magnet Consolidated Gold Mine3. Leitch Gold Mine4. Pan-Empire Joint Venture {Northern Empire Mine)5. Maki Property6. Pichette Occurrence7. Craskie-Vega Occurrence8. Quebec Sturgeon River Mines Limited9. Orphan (Dik-Dik) Gold Mine

10. Mitto Prospect (Kengate Resources Limited)11. Greenoaks Prospect12. Crooked Green Creek Mine (Northern Concentrators Limited)

FIGURE 3 - REGIONAL GEOLOGY

BEARDMORE - GERALDTON AREA

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tJELLICOE 17.3 KM GERALDTON 27.7 KM

COLTER VIVIAN

^VIVIAN TOWNSHIP PROPERTY

GABBRO

MAFIC METAVOLCANIC ROCKS WITH IRON FORMATION

METASEDIMENTARY ROCKS

FAULTS

FIGURE 4- GENERAL GEOLOGY


(SOME DATA AFTER O.D.M. PRELIMINARY MAP P. 1 192)

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REGIONAL GEOLOGY AND MINERALIZATION - Continued

Figure 3 shows that the well-known Northern Empire Mine at Beardmore falls within the Southern Mafic Volcanic Dominated Belt as do the very interesting gold prospects at the Maki, Craskie-Vega and Pichette properties.

Historical production (1934-41) from the Northern Empire Mine yielded 160,000 ounces of gold from quartz-carbonate veins. Gold at the Pichette occurrence accompanies pyrite in shear zones within carbonatized mafic metavolcanics. Chert-magne tite-carbonate ironstones carry gold at the Maki and Craskie- Vega occurrences (as well as at a very recently discovered zone on the old Northern Empire Mine). The gold mineralization at the Maki and Craskie-Vega prospects occurs with discordant quartz-carbonate veinlets within the ironstone formation. These veinlets carry arsenopyrite, pyrrhotite and grunerite. Assay values range up to 0.81 ounces of gold per ton and 5.89 ounces of silver per ton at the Maki occurrence, while values of up to 0.25 ounces of gold per ton persist for good distances with in the ironstone zones on the Craskie-Vega property (Mason and Mcconnell, 1983).

Recent work at the Northern Empire Mine (Northern Miner March 9, 1987, p. B8) outlined a new zone called the Contact vein which "consists of stratabound sulphide mineralization in iron forma tion. The mineralization has a defined strike length (so far) of 175 m with an average width of 2.7 m, and has been found to continue to a depth of 250 m ," The zone grades 9.56 g gold per tonne (uncut).

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f SURVEYS

In February, 1987, a flagged baseline was established at a bearing of due east for 3 km across the entire Vivian Town ship property. North-south grid lines at 100 metre (328 ft) intervals were then flagged from the baseline to the northern and southern extremities of the property. A total of 30 km (18.6 miles) of grid line was established. Several "tie-lines" were also measured to check for deflections of the grid lines caused by the strong magnetic attraction of suspected bands of iron formation. Stations were marked with flagging at each 25 metres (82 feet) along the grid lines. During September- October 1987 another 1.2 km (.75 miles) of intermediate grid line was established. In all, 1250 stations are marked out across the 19 mineral claims equalling an average of 65 stations per claim. All claim corner posts were tied in to the grid. A Topolite belt chain and Silva Ranger compass were used to establish the grid lines as illustrated on all of the large scale maps accompanying this report.

VLF-EM 16 GROUND SURVEY

A Geonics VLF*-EM 16 model instrument rented from Geolease of Mississauga, Ontario was used to survey the entire grid area of the Vivian Township property. The Cutler, Maine signal at 17.8 kHz was selected for the survey. The signal was received from a direction of 94 degrees azimuth, and all readings were taken at right-angles to the station, or at 04 degrees azimuth (facing north). The Basic VLF-EM data and Line Profiles are displayed on Maps V-88-5A&B, while the Fraser Filtered In-Phase values have been plotted and contoured on Maps V-88-4-A&B. Thirteen major conductors (A to M) have been identified on the property.

Continued . . .

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SURVEYS - CONTINUED

VLF-EM 16 GROUND SURVEY - Continued

The Fraser filtering of VLF-EM data has had widespread use for several years, and a full explanation of the technique is given in the geophysical papers by Fraser, Peterson and Ronka that are listed with references at the end of this report.

The Fraser filtering technique may be briefly summarized as follows: By means of simple mathematical operations the tilt data can be transformed into contourable form, and the effects of noise and topography can be filtered from data. By averag ing pairs of stations and taking differences between pairs sep arated by the appropriate distance, values may be plotted and contoured in plan that transform cross-overs into peaks, and a low-pass smoothing mathematical operator reduces noise.

GEOCHEMICAL SURVEY

A geochemical soil survey consisting of 185 samples was con ducted over portions of mineral claims TB875326-3288*3^ 1 at 25x100 metre (82 x 328 feet) grid spacing on an experimental basis in the hope that such a survey would help to outline geology with gold-bearing potential.

A mattock was used to obtain B-horizon soil samples wherever possible. Two hundred grams of soil were placed in 10x25 cm kraft sample bags at each site. Matters notated during the survey included: the soil type and composition, the depth to the B-horizon, the slope direction, and the possibility of con tamination of the sample by exploration trenching or road building.

The average B-horizon sample collected was composed of limonitic, fine-grained sand obtained from 30 cm below surface. Most

Continued . . .

tSURVEYS - CONTINUED

GEOCHEMICAL SURVEY - CONTINUED

samples obtained were believed to be made up of residual soil, but at some sample sites weakly stratified clay, sand, and gravel layers representing shallow basins were observed. In peat bogs the organic soil horizon was found to be 60 or more centimetres in thickness, and underlain by 30 or more centi metres of gray clay. As a consequence few samples were collect ed from bog areas.

The samples were shipped to Acme Laboratories in Vancouver for ICP analysis (30 elements). The results of the ICP analysis and the laboratory procedures are listed in Appendix B.

Out of the 30 elements analyzed only arsenic, lead and iron appear to give meaningful results when compared with the geology map, and the values obtained for these elements have been plot ted and contoured on Maps V-88-6B&7B accompanying this report. Gold values are illustrated on Map V-88-6B, but they are too erratic to contour.

GEOLOGICAL MAPPING

Geological mapping was conducted over the entire Vivian Town ship Property. The geology was mapped at a scale of 1:2500 as illustrated on Maps V-88-3A&B. Large areas of the property are mantled by glacial till or covered by peat and muskeg and rock exposures occur over less than 3# of the grid area. However, most of the rock exposures occur within the mafic volcanic units which probably represent the most favourable host rocks for gold mineralization.

The nature and estimated depth of the overburden is noted on Maps V-88-3A&B.

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PROPERTY GEOLOGY

SIMM AKI

The Vivian Township property covers a 3 km segment of the Geraldton-Beardmore Archean "Southern Mafic Volcanic Dominated Belt". In detail, the belt is made up of two distinct 200 to 250 metre metavolcanic zones (map units 28*3) t separated by 200 to 300 metres of metasediments. The metavolcanics are bounded by mapped metasediments (units 1&4) to the south and north respectively. All rock units are isoclinally folded and strike at an average of 105 degrees across the property. The units dip vertically to steeply southeast (overturned). The southernmost metasedimentary unit (unit 1) is believed to be the lowermost stratigraphically.

Iron formation, i to 2 m thick, occurs with sediments as minor intercalations between volcanic flows in both the southern and northern metavolcanic zones. The iron formation horizons have good lateral extent - some crossing the entire property. Locally, the iron formation is cut by quartz veining and re placed with iron sulphides and arsenopyrite.

Coarse-grained trondhjemite lenses and dykes intrude the mafic metavolcanics on mineral claim 875328, and appear to be related to arsenopyrite-bearing quartz veins in the area.

Fault surfaces observed on the property are dominantly strike- slip surfaces.

UNIT 1 LOWER METASEDIMENTS

Highly indurated, almost gneissic, steeply dipping sandstone and siltstone of the lower metasedimentary unit (unit 1) underlies the southwestern corner of the property. The unit has been subdivided into a lower unit (1b,a) composed pre dominantly of sandstone, and an upper unit O a,b)of 250 metres

Continued . . *

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PROPERTY GEOLOGY - Continued

UNIT .1 LOWER METASEDIMENTS - Continued

thickness,composed predominantly of siltstone. The sandstone unit is a blocky to massive weathering, thick-bedded, medium- grained white quartzite with minor interbedded siltstone. The siltstone unit is comprised of flaggy-weathering, thin-bedded, fine-grained, biotitic sandstone and siltstone with minor quartzite interbeds.

The Lower Metasediments show little structural deformation and appear to lie conformably below Unit 2 metavolcanics.

UNIT 2 MAFIC METAVOLCANICS

Unit 2 mafic metavolcanics, totalling 250 metres in thickness, appear to cross the entire property from mineral claim 875338 on the west to mineral claim 875344 on the extreme southeast corner of the property. Unit 2 is made up of 9 to 10 sequences of basaltic or andesitic flows ranging from 10 to 40 metres thick, and averaging 20 metres in thickness. Each sequence is separated by intercalated sediments. The mafic metavolcanics range from massive and coarse-grained, to highly vesicular in texture, and such distinctions were made during the course of mapping as follows: (Note: this table also applies to Unit 3 rocks).

2a,(3a) is medium-grained andesite or basalt, generally mas sive in outcrop, but sometimes weakly vesicular, or weakly foliated over layers of 30 to 60 cm thick.

2b, (3b) is medium- to coarse-grained equigranular andesite or basalt (sometimes looking like a diorite) and is massive in outcrop.

2c, (3c) is fine- to medium-grained andesite or basalt, which is slightly to moderately foliated. This rock often contains 1 to 3# limonite (after pyrite?).

Continued . . .

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UNIT 2 MAFIC METAVOLCANICS - Continued

3d is fine-grained, light green volcanic flow rock of possible dacitic composition.

2e,(3e) is fine- to medium-grained andesitic flow rock,which is moderately foliated (with some 30 cm layers of well foliated rock); vesicles 1-3 mm occur in 30 cm bands; 1 to 3# limonite (after pyrite or pyrrho tite?) and 2 to 5# narrow lensy quartz veins also make up part of this rock.

3f like 2e, but lighter green (possibly more dacitic).3g fine- and medium-grained andesite with 10#,1-3 mm

feldspar phenocrysts,2h,(3h) is medium-grained andesite or basalt with large

(3 to 20 mm) white amygdules (20#) composed of quartz, carbonate, and chlorite.

2i,(3i) is like 2h, but with open vesicles.2j is composed of fine- to medium-grained, thin-bedded

tuff, and volcanic siltstone and sandstone of ande sitic composition.

The medium- and coarse-grained andesitic and basaltic basal portions (2b) of individual flows grade upwards into finer- grained (2a,c), and more vesicular (2e,f) rocks. The tipper portions of individual flows are locally highly vesicular (2i) or amygdaloidal(2h).

Intercalated sediments, i t o 2 metres thick, occur between flow sequences and often include iron formation (IF). These sedimentary horizons separate the highly fissile, vesicular, upper portion of one flow from the coarse-grained basal portion of the succeeding flow.

As mentioned earlier the Unit 2 mafic metavolcanics appear to conformably overlie Unit 1 metasediments.

Continued . . .

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UNIT 2 MAFIC METAVOLCANICS - Continued

The Unit 2 raetavolcanics are presumably conformably overlain by 200 to 300 metres of metasediments, but due to the muskeg and till cover these rocks do not outcrop on the property. The rocks do, however, yield magnetic values of low gradient which are characteristic of metasedimentary rocks.

UNIT 5 MAFIC TO INTERMEDIATE METAVOLCANICS

Mafic to intermediate metavolcanics (Unit 3), averaging 200 metres in thickness cross the entire property from mineral claim 875326 at the northwest corner to mineral claim 875337 on the east side. These rocks are much like those of Unit 2, and the same alphabetical notation has been used on Maps V-88-3A&B to denote texture types (ie. 3a is equivalent to 2a, and 3h is equivalent to 2h etc.) (Please see the list of texture types under the previous title of this report).

Unit 3 metavolcanics like Unit 2 metavolcanics grade upward from a coarser-grained basal portion to an upper fissile, finer-grained portion. The Unit 3 metavolcanics include andesites, andesite porphyries, and dacites, and in general form thinner flows than Unit 2 metavolcanics. The Unit 3 metavolcanic flow sequences, averaging 25 metres in thickness, are separated by intercalated sediments with iron formation like those of the Unit 2 metavolcanics. The uppermost sequence of Unit 3 metavolcanics includes 25 to 30 metres of thin-bedded andesite tuffs and volcanic siltstones and sandstones which grade upwards into the true metasediments of Unit 4*

UNIT k METASEDIMENTS

Unit 4 metasediments form a wedge, widening from west to east across the northern tier of mineral claims (875327-330). Most

Continued . . .

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UNIT k METASEDIMENTS - Continued

of mineral claim 875350 is underlain by Unit if metasediments. The Unit if metasediments appear to grade upwards impercept ibly into true sediments from the tuffs and volcanic siltstones and sandstones of the upper Unit 3 sequence. The first of Unit if metasediments are thin-bedded, silt stones and arg- illites (4c), which grade upwards over 30 metres into medium- to thin-bedded greywacke, siltstone, and argillite (*fb) and finally upwards into medium-to thick-bedded greywacke sand stone (4a).

The upper limits of Unit /f metasediments are well to the north of the property.

UNIT 5 TRONDHJEMITE INTRUSIVE

Lenses and dykes of trondhjemite intrude metavolcanics at several sites near the southeastern corner of mineral claim 875328. Intrusive contacts are sharp. The medium-to coarse- grained trondhjemite is massive weathering and generally fresh. It is composed of equigranular white plagioclase (85#) and quartz (10#) crystals of 5 to 10 mm. Biotite equals 5# of the rock.

Late, white quartz veins equalling 10 to 20# cut the intrusive at many locations.

IF IRON FORMATION

Iron formation occurs with thin-bedded intercalated sediments within both the mafic (Unit 2) and mafic to intermediate (Unit 3) metavolcanic sequences (see Geology Maps V-88-3A&B).

Continued . . .

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IF IRON FORMATION - Continued

The iron formation varies from 20 to 200 cm in thickness and can range from pure interbanded magnetite(20^) and chert (80#) to ironstone contaminated by interbedded siltstone and argil lite equalling up to 80^ of the rock. The chert is always recrystallized to a sugary quartz while the magnetite is some times altered to radiating grunerite crystals. The chert- magnetite bands range from 5 to 50 mm. Hematite equals up to 10# of the iron formation locally.

At several locations on the property the iron formation is cut by quartz veins and the magnetite is partially, or totally, re placed with iron sulphides (see section on Mineralization).

STRUCTURAL GEOLOGY AND FAULTING

The main structural elements of geology on the Vivian Township property are regional elements. They include the isoclinal folding already mentioned and district-wide strike-slip fault ing. A major fault illustrated on O.D.M. Map P1192, "Colter Township", apparently passes east-west through the property, but features of it were not observed during the mapping project as the fault is coincident with the main creek valley which is largely covered by muskeg and glacial till.

There is, however, widespread evidence of strike-slip and dip- slip movement associated with the isoclinal folding of rocks on the property. Many of the foliation planes are slippage planes, but nowhere is the displacement of rocks great. Fault surfaces were also noted cutting the brittle iron formation locally (at Pit B for example), and minor drag-folding parallel to the dip-angle of the metasediments occurs on the 20 m cliff face at the western side of the pond on mineral claim 875328.

No significant cross structures were noted during the course of mapping.

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MINERALIZATION

Two types of mineralization have been identified on the Vivian Township property so far. They are: (a) arsenopyrite-bearing quartz veins, apparently associated with the trondhjemite in trusive, and (b) sulphide mineralization associated with iron formation. Examples of each type of mineralization are given below:

QUARTZ VEINS WITH ARSENOPYRITE

Sample 8220: Grid 15+13N. 9+95E

At sample site 8220 broken quartz vein material, up to 30 cm in size, occurs within quartz-sericite-schist (which probably represents the upper, finer-grained, highly vesicular top of a mafic flow rock). The broken quartz is traceable for at least 3 metres, but the showing has not been fully prospected. The white, glassy quartz contains 40# arsenopyrite which assayed 23.60^ arsenic, 0.005 oz/T gold, and 0.19 oz/T silver.

Sample 8221; Grid 13+90N. 15+25E

Several large (30 cm) angular pieces of quartz located in the bed of the creek at sample site 8221 contain 1 cm blebs of disseminated arsenopyrite (2#) and pyrite (1#). The white, glassy quartz is weakly limonitic. The rock, believed to be of local origin, assays 1.10# arsenic, 0.001 oz/T gold, and 0.01 oz/T silver.

Several large (30 to 60 cm) white, glassy quartz veins associ ated with the trondhjemite intrusive occur on mineral claim 875328. Limonite staining of these veins is generally weak, and no samples were collected for assay during the mapping pro gram.

Continued . . .

l

- 22 -


SULPHIDE MINERALIZATION ASSOCIATED WITH IRON FORMATION

Pit A. Sample 8222: Grid 17+25N. 6+1OE

An old exploration pit, measuring 1x1 xi m, at sample site 8222 has been blasted into what appears to be a 60 cm wide zone of replaced iron formation. The magnetite has been entirely replaced, but there is some recrystallized chert (10#) and some chlorite and altered feldspars (5#) typical of dirty, banded iron formation. The rock is cut by 25# glassy quartz veining while bands of pure pyrite (30#) and pyrrhotite (30&) apparently totally replace magnetite. On analysis the mineralized rock yielded 1318 parts per million (ppm) arsenic and 280 ppm copper.

A pyrite/pyrrhotite (1090 mineralized zone, 100 metres to the west of sample site 8222 and at the equivalent geological horizon, was not sampled,

Pit B. Sample 8225: Grid 15+90N. 5+90E

A second, old exploration pit, at sample site 8223 also appears to cut replaced iron formation. The rock, well ex posed in the pit, is made up of 30# recrystallized chert and 20# feldspar and chlorite laminae (after siltstone?). It is cut by 40# glassy quartz and 2# jasper veins containing 2# pyrite and 3# pyrrhotite. Assay values were low - 49 ppm arsenic and 67 ppm copper.

Strike-slip faulting is noteable in the open cut.

GENERAL IRON FORMATION

As mentioned under the -"Iron Formation" section of this report iron formation is widespread across the property. It ranges

Continued . . .

l

- 23 -


GENERAL IRON FORMATION - Continued

from a fresh banded magnetite-chert to a heavily limonite and manganese stained rock in which the constituents are difficult to identify. Many of the heavily stained iron formations are probably replaced by iron sulphides and they are deserving of detailed prospecting. One such iron formation is at grid 7+25N, 27+60E. It contains 5# pyrite and a trace of chalco pyrite and arsenopyrite.

DISCUSSION

GEOLOGY

It has been noted by M.W. Carter of the O.D.M. that in Vincent and Mccomber Townships gold is found associated with ironstones occurring with interflow sediments, or with quartz veins cut ting the fine-grained, fissile,upper parts of flows within the metavolcanic sequences. Mineralized ironstones and quartz veins have been located within a similar geological environment on the Vivian Township property, but, so far, good gold assays have been lacking.

The ground magnetometer survey conducted over the property in February 1987 (and filed as an assessment report with the Ministry of Northern Development and Mines) proved to be very effective in defining (within 1 to 5 metres) interflow zones of iron formation on the property. Several lineal miles of iron formation were outlined (as shown on the February Magnetometer Survey Interpretation Map also accompanying this report). Dur ing the September, 1987 geological mapping program, the Inter pretation map was used with great success to find iron formation below moss covered areas. However, few zones were properly prospected due to limited time.

Continued . . .

t

- 2/f -

DISCUSSION - Continued

GEOLOGY - Continued

There is a need for greater prospecting of the iron formation horizons.

At several locations on the property iron sulphides have been introduced into the more fissile rocks near flow tops and these areas should also be prospected more diligently.

Another area deserving of more prospecting is the southern half of mineral claim 875328 where the arsenopyrite-bearing quartz veins appear to have a close spacial relationship with the trondhjemite intrusive.

GEOCHEMICAL SURVEY

The results of the geochemical soil survey were disappointing when compared with observed geology and mineralization. Only three of the 30 elements tested by ICP analysis yielded mean ingful results when compared with geology and the values and distribution of these elements (arsenic, lead and iron) are illustrated on Maps V-88-6B&7B accompanying this report. Gold values have also been plotted on Map V-88-6B.

GOLD GEOCHEM IN SOILS. MAP V-88-6B

The few anomalous gold values shown on Map V-88-6B are erratic in distribution. The highest value obtained was 23 parts per billion (ppb). Most values were 1 to 2 ppb.

ARSENIC GEOCHEM IN SOILS. MAP V-88-6B

A threshold of 10 parts per million (ppm) arsenic was selected for contouring purposes on Map V-88-6B. All arsenic values of the survey on mineral claim 875341 fall below the threshold. A few erratic arsenic anomalies occur on mineral claims 875326 k

Continued . . .

t

- 25 -


GEOCHEMICAL SURVEY - Continue^ARSENIC GEOCHEM IN SOILS. MAP V-88-6B - Continued

327, but the arsenic values in soil are surprisingly low when compared to values of arsenic in rock, and there seems to be little chemical or mechanical dispersion of arsenic from rock to soil. Two sample sites clearly point out this lack of dispersion: at pit A near grid 6E, 17N mineralized rock yielded 1318 ppm arsenic, while the nearest soil samples, 15 and 25 metres away, yielded 3 and 7 ppm arsenic respectively, and at grid 10E, 15+1 ON a sample of quartz vein material yielded 23.60& (236,000 ppm) arsenic while the nearest soil sample, 12 metres away, yielded only 2 ppm arsenic.

The only arsenic anomaly of significance on the property ex tends for 350 metres across the southern portion of mineral claim 875328. Values of greater than 10 ppm arsenic are con sistent across the mineral claim with one peak value of 83 ppm. The anomaly is coincident with a trondhjemite intrusive that is cut by up to 10# quartz veining in the area. The quartz is known to contain arsenopyrite locally. In view of the observed geology the arsenic anomaly in soil is surpris ingly restricted in width (25 to 50 metres) and again shows a great lack of dispersion.

LEAD GEOCHEM IN SOIL. MAP V-88-7B

Lead contoured at 10 ppm outlines the main arsenic anomalies on Map V-88-6B. Lead shows a larger dispersion pattern than arsenic and expands on some of the anomalies, such as those at the centre of mineral claim 875327.

Only two lead values of greater than 10 ppm were obtained from the survey on mineral claim 8753^1*

Continued . . .

t

- 26 -

DISCUSSION - Continued GEOCHEMICAL SirRVftY - Continued

IRON GEOCHEM IN SOIL. MAP V-88-7B

The iron anomalies as shown on Map V-88-7B correlate well with the lead and arsenic anomalies on the property and ex hibit a greater dispersion pattern than either element. For example, an area of interest associated with the trond hjemite intrusive, and nicely outlined by the arsenic anomaly on the southern half of mineral claim 875328, is greatly expanded by the iron anomaly.

The erratic high iron values on mineral claim 375341 prob ably represent narrow beds of iron formation.

VLF-EM GROUND SURVEY

The VLF-EM ground survey has outlined several strong, near- surface (25 to 75 metre depth), conductors crossing the property at 100 to 105 degrees, conformable with the strike

of the geology. Many of these conductors are thought to represent sulphide mineralization or iron forma tion. The conductors, lettered A to K, on Maps V-88-4A&B are described below:

Conductor A is a strong, near-surface, conductor that crosses the entire property from mineral claim 875326 on the west to 875337 on the east for a total distance of 2.5 km. The conductor falls near the indistinct con tact between the metavolcanic rocks of Unit 3j and the metasedimentary rocks of Unit /f. The conductor is coincident with strong (10 to 60#) pyrite and pyrrhotite replacement zones within foliated tuffs and iron formation - with the most noteable location at Pit A.

Continued . .

- 27 -

lDISCUSSION - Continued

VLF-EM GROUND SURVEY - Continued

Conductor A - Continued

Conductor B

Conductor C

Conductor D

The conductor continues strong through the eastern half of the property in an area overlain by 3 to 5 metres of glacial drift.

crosses mineral claims 875326 to 328 sub- parallel, and 100 to 150 metres, to the southeast of Conductor A. The conductor is semi-coincident with highly foliated and well mineralized (pyrite and pyrrho tite, 3-8#) flow tops in mafic volcanics.

Conductor D is the projected eastern ex tension of Conductor B. Conductor D is expressed as a broader and weaker con ductor due to a heavy cover of glacial till (10-15 m?) in the area.

is another strong,near-surface conductor, crossing mineral claims S75326&327 sub- parallel to Conductors A&B. The eastern, and stronger, segment of the conductor is coincident with pyrite and pyrrhotite mineralization (4#) associated with well- foliated flow tops in mafic volcanics.

is believed to be an extension of Conduc tor B as already mentioned.

Conductors E. JF&H are semi-continuous across the entire property for a distance of 2700 m. Part of the H segment of the conductor is

Continued

- 28 -

tDISCUSSION - Continued


Conductors E. F&H - Continuedcoincident with a 2 ra wide iron forma tion horizon on mineral claim 8753Mft Conductors E and F may mark the trace of the same iron formation horizon through the muskeg and till covered areas on the western two-thirds of the property. The magnitude of Conductors E and F has prob ably been lessened by the effects of the overburden.

Conductor G is a moderate strength conductor located in an area of deep (20 m) overburden on mineral claim 8753^3* *t roay be the eastern equivalent of Conductor C.

Conductors I. J&K cross the entire property from mineral claim 875338 on the west to 8753^ on the east. The stronger,"K" segment of the conductor is coincident with a 50 metre thick sequence of mafic flows and inter calated iron formation. A total of four bands of iron formation were inferred from the magnetometer survey within this zone of raetavolcanics during the February sur vey, and some of these zones were later confirmed during geological mapping.

The overlapping effects of the four iron formation horizons yield a broad,strong conductor in general, but the axis of Con ductor K was found to be exactly coincident with 1.5 and 2 m bands of magnetite ironformation on grid lines 18E and 21E respect ively.

Continued . . .

- 29 -

tDISCUSSION - Continued


Conductors I. J&K - ContinuedThe "J" segment of the conductor lies below a muskeg area, but is still moder ately strong, while the western "I" seg ment of the conductor is a little weaker and broader, and occurs in an area be lieved to be covered by 10 to 15 metres of glacial sand and gravel. Conductors J&I are thought to represent the same metavolcanic and iron formation sequence as that outlined by Conductor K on the eastern side of the property.

Conductor L

Conductor M

crosses the northern portion of mineral claim 875339 for 300 metres. It is of weak to moderate strength and may rep resent sulphide mineralization within the Lower Metasediments.

on the boundary of mineral claims 8753M3 &341 is very limited in extent and may mark the contact between the metasediments of Unit 1 and the metavolcanics of Unit 2.

SUMMARY OF ALL SURVEYS

The February, 1987, detailed ground magnetometer survey proved to be most effective in outlining the intercalated iron forma tion horizons within the mafic metavolcanic sequences on the property. The geological mapping in September, 1987, confirmed the iron formation horizons at several locations and was also useful in identifying mineralized fissile flow tops of individ-

Continued . . .

t

- 30 -


SUMMARY OF ALL SURVEYS - Continued

ual volcanic flows. The mapping also identified the trond hjemite intrusive, which appears to have an association with the arsenopyrite-bearing quartz veins.

The geochemical soil survey conducted in September was also useful in outlining arsenic mineralization, apparently associ ated with the trondhjemite intrusive. The soil survey appears to have been a failure elsewhere due to the lack of chemical or mechanical dispersion of elements away from mineralized zones.

The VLF-EM ground survey was useful in outlining both iron formation horizons and mineralized fissile flow tops, but the effectiveness of the survey in delineating specific horizons was hampered by the overlapping effects of several parallel conductors. In other words, the Conductor Axes on Fraser Filtered Maps V-88-A-A&B do not necessarily directly overlie single conductors. In areas of conflicting data between the magnetometer survey and the VLF-EM survey the magnetometer survey is considered to be the more accurate in delineating iron formation horizons.

Both the magnetometer and VLF-EM surveys proved to be very useful in extending the expression of iron formation horizons into areas of deep overburden cover. A high degree of con fidence is given to tho.se anomalies which are projected from areas of mapped geology.

CONCLUSIONS AND RECOMMENDATIONS

As mentioned several times throughout this report the highly fissile flow tops of individual volcanic flows or the iron formation of the intercalated sedimentary horizons offer the

Continued . . .

t

- 31 -

CONCLUSIONS AND RECOMMENDATIONS - Continued

best possibilities for gold exploration. Pyrite, pyrrhotite, and arsenopyrite-bearing quartz veins have invaded the fissile portions of flows, and pyrite and pyrrhotite have entirely re placed the magnetite of the iron formation at some localities on the property.

Several areas worthy of further investigation have been out lined by the geological mapping and by the magnetometer and VLF-EM surveys conducted on the property. Initial work should be concentrated on the stronger anomalies in the more easily accessible areas on the property,such as on mineral claims 875326 to 328. Overburden is believed to be light on these claims, and Backhoe stripping to bedrock to investigate the magnetometer or VLF-EM anomalies should be an easy matter. All sulphide samples obtained from stripping operations should be analyzed for 30 elements by the ICP system, and for gold and silver by atomic absorption.

Stripping could be continued into the deeper overburden areas to the east on mineral claims 875335-337 if the results from the initial stripping program are positive. The stripping program could also be expanded to the Unit 2 metavolcanics crossing the southern half of the property.

The drill testing of any anomalous horizon would be an easy matter as access is readily available to most areas of the property and drill water is in plentiful supply.

SUMMARY OF INITIAL TRENCHING LOCATIONS

Key sites recommended for the initial trenching program are listed on the following page.

Continued . . .

- 32 -

tCONCLUSIONS AND RECOMMENDATIONS - Continued

SUMMARY OF INITIAL TRENCHING LOCATIONS - Continued

Target l - VLF-EM Conductor A and/or magnetometer inferred iron formation:

6+50E 7+OOE 7+50E 8+50E 9+OOE

17+15N 17+15N 16+75N 16+60N 16+50N

10+OOE10+50E1 1 +OOE

1 1 +50E1 2+OOE

16+30N1 6+25N16+15N1 6+OON1 5+85N

Target 2 - VLF-EM Conductor B and/or magnetometer inferred iron formation:

11+50E11+50E11+50E12+OOE12+OOE12+OOE12+50E12+50E12+50E

5+OOE5+50E6+50E7+OOE8+50E9+OOE9+50E10+OOE10+50E

1 1 +QOE

16+05N1 6'fOON

1 5+80N

15+75N1 5+^^N1 5+itON

1 5+25N1 5* 1 5N1 5+OON14+90N

15+OON 1 if+25N

5N

February 20, 1988 M.S. Morrison, B.Se

t

- 33 -

REFERENCES

Carter, M.W.1985: Precambrian Geology of Vincent Township, Thunder Bay

District; Ontario Geological Survey, Map P.2854* Geological Series - Preliminary Map scale 1 inch to i mile. Geology 1983.

Fraser, D.C.1969: Contouring of VLF-EM Data, Geophysics, Vol. 14, No. 6,

December, 1969.Hogg, R.L.S.

1983: Report on Combined Helicopter-Borne Magnetic andElectromagnetic Survey, Geraldton, Ontario for Alclare Resources Inc. - Ministry of Northern Development and Mines Assessment Files.

Mackasey, W.O., Edwards, G.R. and Cape, D.F.1976: Colter Township, District of Thunder Bay, Ontario

Division of Mines Preliminary Map P.1192.1976: Legault Township, District of Thunder Bay, Ontario

Division of Mines Preliminary Map P.1191.Mason, J.K. and Mcconnell, C.D.

1983: Gold Mineralization in the Beardmore-Geraldton Area in The Geology of Gold in Ontario, edited by A.C. Colvine, OGS Miscellaneous Paper 110, pp. 84-97.

Morrison, M.S.1987: Ground Magnetometer Survey, Vivian Township Property,

Thunder Bay Mining Division - Ministry of Northern Development and Mines Assessment Files.

Ontario Department of Mines and the Geological Survey of Canada1963: Aeromagnetic Map 2142G, Wild Goose Lake, Thunder Bay

District, Ontario; Scale 1 inch to 1 mile.1963: Aeromagnetic Map 2135G, Beardmore, Thunder Bay Dis

trict, Ontario; Scale 1 inch to 1 mile.Peterson, N.R, and Ronka, V.

1969: Five Years of Surveying with the VLF-EM Method, a paper presented at the 1969 Annual International Meeting, Society of Exploration Geophysicists.

tAPPENDIX "A"

STATEMENT OF QUALIFICATIONS

I, Murray Morrison, of the City of Kelowna, in the Province of British Columbia, do hereby state that:

1. I graduated from the University of British Columbia in 1969 with a B.Se. Degree in Geology,

2. I have been working in all phases of mining exploration in Canada for the past seventeen years.

3. During the past seventeen years, I have intermittently held responsible positions as a geologist with various mineral exploration companies in Canada.

if. During the past five years I have examined many mineral properties in Northwestern Ontario.

5. I personally conducted the Geological Mapping, and Geo chemical and VLF-EM Ground Surveys outlined in this report.

6. I own a 100^ interest in the Vivian Township Property described in this report.

February 20, 1988Kelowna, B.C. M.S. Morrison, B.Se.

ACME [ICAL LABORATORIES 852 E. HASTINGS ST. VANCOUVER 1C. V6A 1R6 PHONE 2S3-3158 DATA LINE 251

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.08

.11

.14

.11

.44

.13

.04

.13

.14

.17

.13

.05

.20

.21

.07

.08

.14

.12

.08

.07

.24

.12

.20

.09

.05

.241.09.04.24.83

.04

.44

PI

.013

.028

.027

.031

.034

.017

.029

.013

.004

.018

.008

.032

.004

.092

.007

.023

.044

.004.007.010

.013

.004

.004

.024

.023

.021

.014

.023

.049

.007

.013

.042.003.010.031

.021.087

LAPPM

755

12B

910IS

822

119

101410

101111148

91189*

209988

19178

1741

938

CRPPH

2438273427

2343773344

2332177120

29414B3023

2723193222

2414133412

24318

31SI

2342

ttl

.18

.37

.39

.27

.13

.14

.37

.74

.321.43

.20

.14

.19

.34

.22

.24

.25

.49

.24

.15

.18

.23

.21

.22

.18

.27

.14

.12

.22

.07

.22

.47

.07

.28.38

.13

.80

BAPPH

1424192938

393554IS44

2320174428

2323253124

2929213521

3929182121

2222153090

23179

TII

.10

.13

.32

.11

.09

.08

.13

.14

.09

.22

.08

.10

.07

.18

.08

.13

.12

.11.08.09

.09

.08

.08

.09'.08

.08

.07

.04.12.05

.08

.08

.07

.09

.08

.08.08

BPPH

22294

42e24

127

117

10

42493

42453

3573

10

54222

237

AL1

.821.47.83

1.441.59

1.241.792.84

.843.15

.781.53.38

3.97.82

1.031.37.9*.79

1.13

1.10.70.44

1.44.84

.88

.75

.491.59.48

.49

.54

.39

.842.28

1.101.48

NA4

.01

.01

.01

.01

.01

.01.01.01.01.01

.01

.01

.01

.01.01

.01

.01

.01.01.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01.01

.01

.05

x1

.02

.02

.02

.05

.03

.03

.04

.03

.02

.04

.02

.02

.02

.13

.02

.04

.04

.02

.03.03

.03

.02

.02

.03

.03

.04.03.02.04.02

.03

.03

.02

.03

.04

.03

.13

H AUIPPM PPG

11111 2

11111

11121

21111

11111

11111

11111

1 113 49

WS*oM X

~ l

o\ l

h- V-73 /fHf l^ V-74 Ifiot lf* V-7S w* l

1034

IS B

18

M.S. MORRISON FILE tt 87-4441

NI CO MN 'PH PPH PPH

12 4 94 7 2 49

14 4 54

FE AS 1 PPR

1.14 10 .91 21.94 4

U AU PPH PPH

5 ND S W 5 ND

TH SR PPH PPH

5 92 53 7

CD SB PPH PPH

1 2 1 2 1 3

81 V PPH PPH

2 20 2 14 2 32

CA P 1 1

.23 .008

.14 .007

.12 .014

LA CD PPH PPH

12 IB 8 15 8 27

H6 BA 1 PPH

.18 33

.17 IS

.22 50

TI 1I PPR

.04 2

.04 2

.10 2

AL NA l l

.95 .01

.54 .01 1.42 .01

K N AUI Z PPH PPi

.02 13

.01 1 1

.03 1 1

ACME ANALTTlCAL LABORATORIES 852 E. HASTINGS ST. VANCOUVER B. C. V6A 1R6 PHONE 253-3158 DATA LINE 251-1011

GEOCHEMICAL- ANALYSIS

.300 GRAN SAMPLE IS DIGESTED NITM 3NL 3-1-2 HCL-HN03-H20 AT 93 DES.C FOR ONE HOUR AND IS DILUTED TO 10 ML NITH HATER. THIS LEACH IS PARTIAL FORNNFECAPLACRN68ATIIDANB LINITEB FOR MA K MB AL. Ml DETECTION LIMIT IT ICP IS 3 PPM. - SAMPLE TYPEi SOIL AUI ANALYSIS IV AA FUN 10 (MN SAMPLE.

DATE RECEIVED! SEPT 28 l W DATE REPORT MA I LED l W. . DEAN TOYE, CERTIFIED B.C. ASSAYER

M.S. MORRISON File # 87-4595 P*ge l

SAMPLEI HOPPM

^ V-74 /4~fS~o^ V-77 f**X

___ V-78 '-f "*V-79 /(+MV-80 K+ir

^ V-81 ff+te^ V-82 /jyzr^ V-83 if+n^ V-84 tf+X

V-85 /ftot

V-84 'f*-*"V-87 /4*r*V-88 '-Htf

——— V-B9 /4.+0*V-90 'f -f ~' 'f

r-\ V-91 ir+iS^ V-92 tr+ot\i V-93 *HW^ V-94 /•f'i'o*** V-95 /Hff

——- V-94 /f C**V-97 '(tooV-98 /T/V

f- v-99 tt+f*^ V-IOO /JViT*•t^ V-101 /r+X11h, V-102 Woo

V-103 /4/*"V-104 /-f/r*V-105 '***f

V-104 /4t"0fftof V-107 'f*)f

V-108 //"tfvjT v-109 /x*a-•v V-110 itioo

^ V-lll "t**"STB C/AU-S

j|11'

21117

,1i13

113I1

122^3

2221l

,1

2373

819

CUPPN

11734

13

149

1010IS

9li44li

iB

Bi134

718117359

21101799

118

335942

4041

PBPPN

7747i

1244

1111

743S

18

24

1443

413

91319

717B72

45

199

19

1038

ZNPPN

2424IB2720

1921243439

2122311831

li21

1183423

2727384449

3134302122

37207080

118

,j132

AGPPN

.1.1.1.1.1

.1

.1

.1

.2

.1

.1

.1

.1

.1.3

.1.1:5.1.1

.3

.1.1.2.1

.1.1.1.2.1

.1

.2

.3

.1

.1

.37.2

NIPPM

2422

99

19

1211121421

1523191013

B1138li18

1212144027

2113147

IP

915283448

2368

COPPN

97328

i3347

S10i43

33

518i

55S

2614

Si743

4i

151814

1328

MNPPN

144129101

7497

71155138179120

172233204Hi153

949i

450118104

9495

195303170

12510312810782

85118294324444

2231143

fEI

2.331.741.231.272.12

1.901.381.411.722.94

1.492.071.981.342.70

.931.514.921.941.59

2.052. 354.034.444.33

2.391.942.372.781.47

1.441.715.524.194.42

3.043.94

ASPPN

2142i3

4433

44

408934

27

19H3

447

437

754

873

54529

8339

UPPN

355S5

S3535

S5553

53S55

53353

33555

53555

519

AUPPN

NDNDNDNDND

NDNDNDNDND

NDNDNDNDND

NONDNDNDND

NDNDNDNDND

NDNDNDNDND

NDNDNDNDND

ND8

THPPN

43324

33442

44431

34323

44111

33372

14211

338

SO CD SBPPN PPN PPN

1299i7

i9

1015i

98784

9797B

7i331

iii55

iB4

10It

22222

22222

42222

22222

32222

22222

22222

9 1 231 11 11

81PPN

22232

22222

23223

22222

22222

22222

22222

222

VPPN

3328202827

38322132S3

27283023(1

1723

2354224

3037

184235107

3041573230

3829

143Hi217

140Si

CAI

.22

.19

.23.08.12

.08

.28

.33

.52

.11

.21

.15

.11

.11

.10

.19

.11

.24

.12.13

.10

.04

.03.08.09

.08

.08

.12

.06.07

.06

.15

.11

.21

.19

.19

.47

Pl

.014

.012

.015

.008

.019

.007

.007

.014

.011

.024

.011

.030.024.013.010

.004

.012

.017

.Oil

.019

.024

.028

.021

.009

.915

.009

.009

.012

.037

.016

.009.023.018.014.034

.021

.085

LAPPN

91012

711

111ISIS12

10101010

5

121099

10

19424

7111

158

B1249i

738

CRPPN

4034192733

2025252942

3030342039

1724903023

24343470Si

3434252921

li255277

237

54it

KI

.32.42.20.20.23

.IS

.30

.29

.35

.52

.35

.29

.31

.11

.57

.20

.221.94.37.23

.20

.18

.701.75.59

.42

.27.31.20.li

.14.29.87.44.55

.45

.89

DAPPN

5940312348

2238375928

35S3343723

2432422738

2233131722

4341291228

1729224439

41183

TII

.09.08.04.07.08

.08

.07.07.09.11

.07

.09

.08

.08

.13

.04.07.14.09.07

.08

.07

.13.18.21

.09

.08.12.10.07

.08.08.29.19.34

.18

.04

B ALPPN I

2 1.935 1.243 .972 .742 1.B2

2 .952 1.042 .913 1.342 1.57

4 .91S 1.353 1.242 1.152 1.29

2 .452 1.29li 2.772 1.052 1.19

2 1.172 2.282 1.244 2.522 US

4 l.iS2 1.322 1.312 .792 1.07

2 .84i 1.142 1.914 1.504 1.19

B 1.2137 1.84

KAI

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01

.01.01

.01

.01.01.01.01

.01

.01

.01

.01.01

.01.01.01.02.02

.01

.04

KI

.04

.03

.02

.01

.03

.01

.02

.03

.03

.04

.03

.04

.04

.03

.02

.01

.02

.02

.03

.03

.03

.02

.02

.01

.02

.02

.02

.03

.03

.02

.01.03.03.03.04

.04

.13

H AUIPPN PP8

11111

11111

1111I

11211

21211

12l11

11111

1 113 32

T)

o o

3o

M.S. MORRISON F lfl 87-4595

SAMPLE! W CDPPM PPM

^ V-112 /*tfoS V-113 /*^WS V-114 /4^*o** V-115 /?*7T

V-lli IS4gV

M 17 Iftgf^ V-118 /.rf oo-K V-119 /•++7S'~^T V-120 /4-WoS1 V-121 /4-*fr

V-122 /f**V-123 lUffm C/AU-S 1

____ V-124 /j/iroV-125 /^,a

V-124 lwV-127 ffj-oV-128 *iT

^ V-129 *.ooS V-130 t t?f-

V-131 **f*V-132 S t isV-I33 4*0V-134 7Y"a-V-135 Wt

V-136 ry*rV-137 1**V-138 **wV-139 Wir

^ V-140 iff^itn v-141 w

V-142 W*V-143 WI

_____ V-144 rcaoV-143 " fee

*{ V-146 *vS V-147 Ufa

27143810

7

4B7B7

64

5964

710

41014

S545

17

43357

21tt

PI INPPM PPM

19 33i 253 SB6 172 16

6 164 104 18

10 284 14

7 134 21

37 1276 144 18

6 183 248 198 309 22

2 113 124 137 13

IS 26

6 215 137 206 214 16

3 259 255 236 197 31

9 254 16

AGPPM

.5

.1

.2

.3

.1

.2

.1

.1

.1

.2

.3

.17.2

.1

.7

.2

.3

.1

.2

.1

.1

.1

.1

.2.2

,l.2.1.2.1

.1

.1

.1

.2.1

.2

.1

NIPPM

IS1740

BB

1299

IB12

912646

11

1014112621

71B3

22

11B

13146

1920

91512

12S

CO MN FEPPM PPM 1

S 197 1.917 114 1.96

16 231 3.013 61 1.443 104 1.13

J 130 1.704 77 1.214 84 1.556 118 2.104 86 1.43

3 B3 1.274 134 1.67

29 1094 3.663 56 1.356 182 2.21

4 134 1.38S 1SS 1.784 104 1.37

10 174 3.15B 116 1.84

3 69 1.201 36 1.293 77 2.122 61 1.589 132 3.44

5 131 1.723 63 1.146 BS 2.27S 103 2.333 84 1.39

7 121 1.977 122 2.413 B6 1.236 103 2.03B 271 3.09

S 176 1.502 63 1.21

ASPPH

53B732

234

558

33

3738

87253

22327

32342

232k4

22

U AU TH SR CD SBPPM PPH PPM PPM PM PPM

8 NOS NO5 ND5 NO5 ND

5 NO3 NO5 NO5 NOB NO

6 ND3 ND

24 7 36 NO3 NO

5 NO3 NO5 NO5 NO6 NO

3 ND5 NO3 NO3 NO3 NO



128999

107i98

9B

49 168

9109

139

74769

87B97

69999

5 NO 5 II5 NO 3 7

22232

2222t

22

1632

22222

22223

22222

2Z222

22

BI V CA P LA CR H6 BA II B AL NA KPPM PPM I I PPM PPM I PPM I PPM I I i

2 33 .25 .014 12 35 .59 39 .09 7 1.21 .01 .OS4 32 .14 .011 11 27 .33 40 .08 4 1.26 .01 .043 40 .23 .013 12 50 .34 31 .10 5 1.38 .01 .082 23 .09 .008 13 21 .08 32 .06 3 1.36 .01 .042 16 .13 .010 14 17 .20 23 .06 2 .78 .01 .03

2 26 .43 .015 13 23 .24 35 .08 2 1.25 .01 .042 23 .14 .011 U 15 .16 15 .07 7 .70 .01 .032 34 .12 .008 10 18 .22 21 .07 3 1.21 .01 .032 43 .20 .013 10 62 .62 33 .10 8 1.36 .01 .042 23 .15 .413 9 20 .17 24 .07 5 .96 .01 .04

2 20 .21 .020 10 18 .19 30 .06 3 .90 .01 .OS2 27 .14 .025 11 22 .23 39 .08 4 1.16 .01 .04

22 35 .47 .083 38 SB .87 176 .06 37 1.91 .06 .132 22 .09 .013 12 IB .13 33 .06 7 1.08 .01 .042 36 .32 .012 12 31 .28 31 .08 3 .99 .01 .04

2 21 .33 .012 14 23 .26 27 .06 16 .73 .01 .042 29 .37 .024 IB 31 .36 32 .08 10 1.03 .01 .052 23 .21 .008 13 22 .27 33 .07 9 1.03 .01 .035 42 .19 .018 9 47 .44 68 .12 6 1.97 .01 .062 25 .19 .024 12 29 .30 74 .07 3 1.83 .01 .05

2 20 .16 .019 10 IB .18 20 .06 2 .90 .01 .032 18 .05 .009 7 7 .04 11 .04 2 .33 .01 .032 43 .10 .012 f 22 .17 27 .10 2 .97 .01 .032 36 .07 .011 10 19 .14 13 .09 7 .76 .01 .032 46 .14 .020 10 38 .29 70 .11 4 2.30 .01 .05

2 26 .24 .025 9 23 .31 27 .07 2 .95 .01 .042 22 .14 .003 10 16 .16 26 .07 4 .94 .01 .022 28 .11 .010 10 29 .20 40 .08 5 2.00 .01 .042 33 .12 .013 11 28 .24 32 .09 2 1.31 .01 .042 26 .12 .016 10 17 .17 23 .07 B .93 .01 .04

2 28 .16 .021 10 23 .28 27 .06 6 1.54 .01 .032 31 .17 .027 11 32 .32 56 .09 3 1.64 .01 .052 21 .23 .007 14 19 .22 37 . .07 7 1.06 .01 .032 31 .14 .017 10 26 .25 40 .09 4 1.55 .01 .062 50 .33 .007 16 40 .44 25 .11 9 .97 .01 .03

2 23 .56 .023 20 24 .43 34 .07 4 .97 .01 .052 25 .20 .006 10 IS .14 29 .06 3 .BS .01 .02

H AUtPPM PPB

I 11 11 11 11 1

1 11 11 11 11 1

1 11 4

12 481 11 2

1 161 11 11 11 1

i 11 11 21 12 1

1 11 11 11 11 t

1 21 11 11 11 1

1 11 1

Oo

O O^

H

M.S. MORRISON FILE # 87-4595 Page |

SAHPLEI HO CU PIPPH PPH PPH

Ut f V-148 WfUff. V-149 /tt ,o

V-150 f/**V-151 t+VV-152 8 *ZS

V-153 t tooSTD C/AU-S 1V-154 7V7J-

____ V-153 ftstV-154 q too

V-157 *fVV-158 t-tnV-139 jw

LfH^Of. V-160 f/ooV-161 *V

V-162 W*V-163 *ST

_____ V-164 7*o*V-163 f*oV-166 *wrr

1 IS f V-167 **wV-168 UKV-169 0/00

_____ V-170 f 'fV-I71 '(M.O

V-172 tVWZ/f"*^ 0f V-173 ?*f*

V-174 *'*rV-175 f***V-176 /w*0

V-177 4V3TV-17B f/**V-179 **r

Z/4/ V-1BO *aoV-I8I J*ar

V-IB2 *WV-183 #,ar

6 913 1010 810 19

9 9

B 959 37

9 818 7

8 2

8 57 89 94 S2 8

10 49 3

10 314 43 9

11 S8 39 106 4

IS 6

IB S13 114 910 310 6

6 B14 614 116 46 2

10 59 2

SAHPLEI NO CU PIPPH PPH PPH

i'+f y-184 *"* l 1 2 1i~irf V-183 *V 1 13 5

UPPH

1724283523

25131232918

252316149

1917242010

2617IB1516

3828151221

1322192114

2418

MPPH

2321

ABPPH

.1

.2

.1

.4

.1

.27.4.3.3.2

.3

.2

.1

.3

.1

.1.1.2.1.1

.1

.1

.1

.2

.1

;1.1.2.1.1

.2

.1

.1

.1.1

.2

.1

AEPPH

.1

.1

NlPPH

215

71012

176415246

II16983

117

1922

7

13151475

15187

1010

4191114

9

1614

NlPPH

17IB

CO IW FEPPH PPH X

2 49 1.277 166 2.083 69 2.523 60 2.004 84 2.19

8 118 2.4328 1106 3.853 103 2.486 120 2.233 101 1.09

4 166 1.475 102 2.814 127 2.272 81 1.462 35 .99

5 98 1.903 89 1.026 153 1.758 98 2.154 71 1.52

4 135 1.546 93 1.976 75 1.993 102 1.153 91 1.36

8 278 3.955 163 I.BI4 62 1.894 67 1.774 121 2.32

2 60 1.307 106 2.635 93 2.034 100 1.653 59 1.48

7 105 2.484 92 1.38

CO HN FEPPH PPH I

6 137 1.456 9! 2.30

ASPPH

43332

431

342

2S424

52272

22422

23629

23224

42

ASPPH

22

U AUPPfl PPH

3 ND3 NDS ND5 ND5 ND

S ND22 8

5 ND5 NDS ND

5 ND5 ND5 NOS ND5 ND

5 ND5 ND5 ND5 ND3 ND

3 ND5 NDS NDS NDS ND

5 NDS ND5 ND5 ND3 ND

S ND5 NOs m5 ND5 ND

S ND3 ND

U AUPPH PPN

3 ND3 ND

TH SR CD SI 81 V CA P LA CR US IA TI 1 AL NA K H AUtPPH PPN PPH PPN PPM PPN I I PPH PPH I PPH I PPN 1 I l m m

3 36 93 63 63 7

4 738 49 1

S 74 122 7

3 93 93 63 12 6

3 74 92 104 73 6

4 105 93 104 83 9

1 61 54 94 33 6

2 53 64 62 73 3

3 83 7

22 t

! 39 .08 .007 B 14 .10 B .OB 13 .56 .01 .02 1t 35 .29 .010 21 29 .21 42 .08 2 1.72 .01 .03

2 2 SO .07 .008 9 25 .15 15 .12 3 1.05 .01 .043 i 38 .09 .009 B 24 .13 23 .08 2 1.23 .01 .032 2 38 .08 .009 9 23 .17 39 .09 3 1.41 .01 .03

3 :t 30 .15 .021 10 32 .28 36 .09 11 1.54 .01 .0618 21 55 .47 .086 37 59 .85 175 .06 39 1.91 .06 .13 19

M

M

34 .12 .018 11 28 .24 38 .09 6 1.43 .01 .0632 .51 .024 43 37 .30 86 .08 6 2.01 .01 .0324 .21 .009 8 16 .23 33 .06 2 .73 .01 .03

22 .38 .011 IS 23 .31 31 .07 4 1.00 .01 .0446 .18 .013 10 29 .25 49 .11 6 1.59 .01 .0536 .10 .019 10 24 .20 21 .09 2 1.09 .01 .0426 .11 .008 10 IB .18 26 .07 2 .87 .01 .0426 .07 .005 10 11 .10 17 .07 3 .52 .01 .02

2 2 29 .11 .024 10 24 .21 24 .08 6 1.79 .01 .03222

t 18 .39 .010 16 17 .18 45 .05 3 .83 .01 .031 29 .36 .012 13 38 .43 36 .08 5 1.03 .01 .03l 28 .12 .013 10 32 .24 36 .08 2 1.88 .01 .03

2 3 26 .11 .010 10 20 .17 IS .07 4 .10 .01 .03

22 iJ

22

*

j22M

2m

A

24

3 ;2 J

l 23 .34 .019 16 22 .38 32 .08 4 1.05 .01 .04t 29 .18 .011 12 31 .23 54 .08 6 2.23 .01 .03

31 .23 .012 9 24 .19 37 .07 4 1.49 .01 .0318 .27 .027 14 19 .21 II .06 5 .52 .01 .0333 .24 .008 12 IS .11 29 .06 3 .94 .01 .02

79 .12 .013 1 45 .49 34 .09 8 1.96 .01 .0233 .11 .016 6 26 .54 24 .09 2 1.36 .01 .0212 .13 .til 14 20 .12 26 .07 6 1.76 .01 .0337 .M .010 f 21 .13 27 .07 16 1.43 .01 .02IS .07 .012 12 17 .24 27 .08 4 1.23 .01 .03

39 .05 .008 1 14 .12 14 .08 3 .73 .01 .0241 .07 .013 10 34 .28 52 .10 3 2.04 .01 .0333 .08 .010 9 26 .21 27 .08 4 1.75 .01 .0326 .11 .006 II 25 .26 27 .07 3 1.42 .01 .0325 .05 .009 B 18 .13 23 .06 3 1.18 .01 .03

t 37 .09 .019 10 31 .25 52 .09 4 1.79 .01 .04t 24 .10 .012 12 38 M 23 .07 5 1.15 .01 .03

3112

132

111

11111

1212I

t1231

11121

11111

12

TH SR CD SI 81 V CA P LA CR W 8A TI 1 AL NA K 1 AUIPPH PPN PPN PPM PPH PPH 1 I PPH PPH 1 PPH IPPH I I I PPH PPI

S 10 1 23612

2 25 .20 .016 16 29 .36 35 .08 1 1.13 .01 .05 2 12 32 .09 .Oil U 10 .20 33 .09 6 2.18 .01 .04 1 1

X

c5

io o

M

iD

S

APPE

ND

IX

"C"

GE

OC

HE

MIG

AL

/ASSA

Y

CE

RT

IFIC

AT

E

S"

3

2 '

'

s sas

SS

SS

S

^. \ n

'•x M^nistryof Report of Work iDOCltowSlices (Geophysical. Geological, y^SO

Geochemical and Expenditures' -

l 42EiiNwea0a a.neae VIVIAN900

Type of Survey(s) \ liownsnipor

Geological, Gepphysical Jk Geochemical j ^Vivian^ Gr- H 7;'Claim Holder (si JProspecfor's Licence~Na

Kr. Murray S. Morrison j S5848Address

684 Balsam Road, Kelowna, B. C. V1W 1B9[Date of SurveV ifromJsLtof ~"~ "~' rfotal,MJies"bf rine"CuT"""~Ln, Q A9 i06 10 87:1 9( nagged onl

Survey Company

M. Korrison Geological Consulting [f*Y j Day J Mp. j Jr. |Name and Add'ess of Author (of Geo-Techmcal report)

Murray Morrison, 684 Balsam Road, Kelowna, B. C. V1W 1B9Credits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Geophysical Days per Claim

Man Days

Complete reverse side and enter total(s) here

RECEIVEDFEB29

NPS SECT'.

' Electromagnetic l 20

- Magnetometer j

- Radiometric

- Other

Geological

Geochemical

Geophysical

20

Days per Claim

O*3

, - Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological i

eochemical

Credits

Note: Special provisions Electromagnetic credits do not apply to Airborne Surveys. Magnetometer

Radiometric

Days per Claim

Mining Claims Traversed (List in numerical sequence)

Expenditures (excludes power stripping)Type of Work Performed

GeochemicalPerformed on Claim(s)

TB 875326,327,3288.3^1

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

s 2035.00 135Instructions

Total Days Credits may be apportioned at the claim holder's choice, Enter number of days credits per claim selected in columns at right.

Mining ClaimPrefix Number

875326875327875328875329875330875331

.! 875332875333

l 875334875335875336875337

i-A?533?.. | 875340i 875341j 875342 ^875343, r 875344

KARO QSOLOOICAU SURVEY ASSESSMENT F'

'-.OFFJCF.._

Expend. Days Cr.

404040

15

Mining ClaimPrefix Number

O.*^ 33

Expend. Days Cr.

Total niynber of mining claims ctejred by this report on work.

1 y

DateFeb. 11/88

Regorded Holder orSgent (Signature)

Certification Verifying Report of Work

For Office Use OnlyTotal DaytCr.jDate Recorded jMimJI Record

Date Approved as ecorded t

Jl hereby certify that l have a personal end intimate knowledge of the facts set forth in the Repon of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.^^^(rePQrt tn fnl 1

Name and Postal Address of Person Certifying

Morrison. 684 Balsam Road, Kelowna, B. C. V1W IRQ

]Date CertifiedFeb. 11/88

Certified by (Signature) ,*

SLignaturei ;~2±

1362 (81/9)-?

Ontario

Ministry ofNorthern Developmentand Mines

- 42 -Geophysical-Geological-Geochemlcal Technical Data Statement

APPENDIX E File.

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Siirvpy(s)Geological t Geochemical k Geophysical Township or Area Vivian Township.—————————.——— Claim Holder(s) MR. M. S. Morrison————.——^———

684 Balsam Rd. . Ke&owna. B, C. ——— . Morrison Geoloical Consultin

Author of Report M. S. Morrison ,Address of Author 684 Balsam Rd T Kelowna, B. C.Covering Dates of Si.rvey Sept. 1 0X87-Feb.2Q / W 1 B9

(linecutting to officef

Total Miles of Line r..t 19 (flagged only)

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical—Electromagnetic.—Magnetometer--—Radiometric———Other—————.

DAYS per claim

20

Geological.Geochemical.

20

AIRBORNE CREDITS (Special provision credit* do not apply to airborne lurveyi)

Magnetometer Electromagnetic Radiometric(enter days per claim)

20/88 SIGNATURAuthor of Report or Agent

Res. Geol.. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

TB 875326(prefix) (number)

TB 875327***t**************t**l*Y**f***r************l

..TB...8..7.5.3.2.8..,

..T.OZ53S9..

J.OZ5.33.TB 875332

••••••••••••••••••••••4X

TB 875333TB 875334

TB 875335

TB 875336

TB 875337

TB 875338

TB 875339

TB 875340

TB 875341

TB 875342

TB 875343

TB 875344

TOTAL CLAIMS. 19

837 (85J12)

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS If more than one survey, specify data for each type of survey

Number of Stations, Station interval —— Profile scale -———Contour interval.

125025 metres (82 ft.)

.Number of Readings _____1250——-—TOO metres (328 ft,

Xine spacing ________________1:2,500

Fraser Filtered dip angle

ctiz o

Instrument.Accuracy — Scale constant. Diurnal correction method.Base Station check-in interval (hours). Base Station location and value ———

U

g IsSJ W

Instrument Geonics Model VLF-EM 16Coil configuration Coil separation Accuracy Method: D Fixed transmitter

17.8 kHz Cutler. MaineD Shoot back D In line D Parallel line

Parameters measured.(ipecify V.L.F. station)

In-Phase Tilt Angle and Quadrature

O

Instrument.Scale constantCorrections made.

Base station value and location.

Elevation accuracy.

zo

a x

gc z

c/355W t*

Instrument ————————— Method D Time DomainParameters — On time .

- Off time— Delay time ———— Integration time.

Q Frequency Domain _ Frequency _____ _ Range ^^——^—,

Power.Electrode array — Electrode spacing . Type of electrode

SELF POTENTIALInstrument^————————-—.^—--——-————-——-..^———^-^—^-—... Range.Survey Method .^—-—-—-—-—^^———————-—-———^^—————..—-..———.—-.

Corrections made.

RADIOMETRICInstrument.Values measured.Energy windows (levels)———^^——-^——————————-.....-^——..—.—.—.—.—-—.Height of instrument———————————————————————————Background Count. Size of detector——————————————————————————————————————————Overburden .^-————-——-————..——-———^———.-—————™....-—-..—.——

(type, depth — include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.) Type of survey—————————————————————————Instrument —-—^^—^^-———^-—.-^—————— Accuracy——————————————————————————Parameters measured

Additional information (for understanding results).

AIRBORNE SURVEYS Type of survey(s) ——— Instrument(s) —————

(specify for each type of survey) Accuracy^————-————-——..—-.

(specify for each type of survey) Aircraft used-^-—————————-———-———.^——.......^——.

Sensor altitude.Navigation and flight path recovery method.

Aircraft altitude-—————..——————-—.—.—.———..———Line SparingMiles flown over total area________________________Over claims only.

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples TB 875326-328&341

Total Number of Samples—— Type of Sample. SO11

185

Average Sample Weight Method of Collection—

(Nature of Material)200g

mattock

BSoil Horizon Sampled.Horizon Development generally goodSample Depth, average 30 cm

generally flat, shallow glacial till ——^-———

Drainage generally good

Estimated Range of Overburden Thickness0.5 to 2 m —^—-——

SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)

— Mesh size of fraction used for analysis "*

General.

ANALYTICAL METHODSValues expressed in: per cent

p. p. m. p. p. b.

Fe,Ca,Mg mostAu

Others

o g o (As) and others, see Appendix B

Field Analysis (. tests)Extraction Method. Analytical Method. Reagents Used——

Field Laboratory AnalysisNo. ———————^— .tests)Extraction Method. Analytical Method . Reagents Used——

Commercial Laboratory ( ^0 element N^nfT^j^t^yAcne Analytical Labs Ltd. Extraction u^n3ml 3-1-2 HC1~HN03~H20 , 95 "C

Analytical Reagents

analysisHC1 1 HNQ 3

General Further details are given in Appendix B. The geochemical survey credits have only been applied to four mineral claims. An invoice of the lab costs has been included in Appendix D. ____

6Qk Balsam Road, Kelowna, B.C. V1W 1B9

April 6, 1988

Mining Lands,Ministry of Northern Developmentand Mines,6610 Whitney Block,Toronto, OntarioM?A 1W3

Dear Sir:

Re: Geological, Geochemical St Geophysical Work Conducted onMineral Claims TB875326-344 Located in Vivian Township,

___Thunder Bay Mining Division.—--.----------.—--———-..-1—-—-.

On February 19, 1988 a "Report of Work" for the above listed mineral claims was filed at the Thunder Bay Mining Division Office.

As required by the Mining Act, I herewith enclose 2 copies of a report entitled "Geological, Geochemical b Geophysical Surveys - Vivian Township Property, Thunder Bay Mining Division, Ontario"for the claims listed in the Report of Work.

I hope that the report meets all of the requirements for Special Provisions Coverage on the property.

Yours sincerely,

Murray Morrison

MM/fh Encls. PRIORITY POST

7N

16 N

5 N

14 N

— I3N

I2N

— II N

ON

— 9 N

8 N

— r N

— 6 N

CDm i

CO COl

CL

5

00

oQ

ro -^m

roCOm m

balsam, poplar

alder poplar

spruce muskegspruce muskeg

poplar, alder , spruce , '

' birch,spruce

v\ birch, poplar

3 m glacial till

3 m glacial till

glacial sand, gravel ,

spruce and pine flat balsam , poplar

spruce muskeg

balsam . pop] ar

2o,e

im IF 5 0X0 Urn (pyl

- . :2a ' . - - ---' Im , ._.

.- - porp.dyke.' 2a T- 2a.' '.

py; tr cpy.asp

* ' sPr

2e,a * * .V

?5m glacial till

2 h ,;.-"2h 2-- 2a.e

OJo m

MAG NET l C DECLINATION

l 0 30 ' WEST

GEOLOGY

CLAIM POSTS WERE TIED IN WITH COMPASS AND BELT CHAIN

42E11NW0202 2 .11838 VIVIAN

PRECAMBRIAN

ARCHEAN

INTRUSIVE ROCKS

5 Trondhjemite

METASEDIMENTS

50

4a Greywacke sandstone, med. to thick—bedded

4 b Greywacke, si Itstone and ar g l l life, med. to thi n-bedded

4c Siltstone and argillite, thin-bedded

METAVOLCANlCS

Mafic to Intermediate (3) ( Andesitic to Dacitic )

Mafic l 2 ) Basaltic to Andesitic

3o,2a m. g,. ; weakly vesicular; weakly foliated

3b,2b m. g. to e.g. equigranular; massive

3c,2c f. g. to m. g.; slight to moderate foliation; l t o 30/*. limonite (after py d po)

3d f. g . dac i t i c ? flow

3e,2e f. g. to m. g.; moderately foliated, 3O cm vesicular zones;

1 t o y/o l imonite (after py a po);2 to 5 0Xo narrow, tensy quartz veins

3f like 3c, but lighter colour {more dacitic)

3g f. g. f o m. g.; with l OVo feldspar phenocrysts

3 h, 2 h m. g. ; with IQ-20% large white amygdules

3i , 2 i like 3h or 2h, with open vesicles

2 j f. g- to m. g. thin bedded tuff

IF IRON FORMATION

LOWER METASEDIMENTS

la biotitic siltstone, weakly schistose

Ib quartzite

asp

cpy

f. g.

fo l .

l i m

m. g.

o. b.

po

po r p

ppm

pyqtz

t r

vn s

arsenopyrite

chai copyr i re

fine-grained

f o l i at e d

l i ma n i T e

medium-grained

overburden

pyrrhot Ste

porphyry

parts per million

pyrite

quartz

trace

veins

outcrop

angular float

\ \ bedding, foliation

X* vein, shearing

assumed geological contact

"' inferred flow top

2. 11030

100 200 m

200lin: 208 ft

ZYGOTE RESOURCES LTD.VIVIAN TOWNSHIP PROPERTY

GERALDTON AREA , T HUNDER BAY M. D , ONT.

GEOLOGY

MINERAL CLAIMS TB875 330, 335-337, 342"344

VI V l AN TOWNSHIP

GEOLOGY BY M M

DRAWN BY M.M., AH

JANUARY 1988

SCALE l : 2500

NTS 42- E- II W

MAP V-88-3A

I7M

16 N

15 N

14 N

I3N

12 N

M N

ION

9 N

8 N

7 N

6 N

om m

4 KM TO HIGHWAY M5-10 "/o py,po 2Vogt! vns F 5 Vo py, po

Pit A see text sample 8222 28Oppm Cu 1318 ppm As

semi- l muskeg

shallow boulder till 5 0Xo Mm ^2*4' i ' 3O 0Xo qtz^vns .-.| 3c fol. bleached vol. l./... over 30 cm

2-3 m Htill .

2-3m Hill alder . spruce spruce muskegol.5Vopy.po 7 ,' .' 3j

•-.-2-3Vopy,po7 see

'//Pitv'fol. 'f 6"' Pp™

v -/' 49 ppm As ,2-3y.py,po: ;

4b 3vopy,po..3c

3Ocm qtz vn J. '^'3g sample 8220-^

23.60 0Xo Ae* 0.005 OZXT Au

- - ,O.I9ozX,T Ag

mixed forest

fol. l-3V.py.po10m ? /'l 3 fol.5y0 lim

qtz and 4bcm

pieces balsam, poplar50cm IF/ 5 * .;-. of qtzfol. oy. py t po,,4b

IO DXo qtz vns

poplar. spruce

HO cm) IF toy. 11 msand flaf

shallow till10- 15 m sandy.10 m bench sandy gravel 2~3m sand and gravel flatspruce muskeg 30cm qtz pieces

sample 8221 .10 y* As 0.001 oz/T Au O.OI oz/T Ag

15m sandy l gravel

5 - IO m

sandy,gravel

sand , grovel,

spruce, poplar, pine

sandy, gravel flat

10-15 m ? o.b. glacial sand, gravel. boulderswet spruce muskeg

spruce , pi ne flatpine,spruce, poplarpine , spruce

5cm 50cm IF

•-J IF 40cm2e * .V-2a,e

2b --2a

.•"" IF 150cm

875340 . oeat ' .'---2b.a

-•2a 2-4mspruce T flatpeat . spruce

V.2a,e -- fc .- (alder/^- *

peat, sprucesand, gravel till

2-3 m o. b.

15m ? sand.

spruce muskeg alder, spruce

spruce . pine

spruce muskeglow glacial i ridges

sand , gravel

balsam forest

spruce muskeg

spruce , pine

MAGNETIC D ECLI NATION

l 0 30' WEST

OC-O

C/)

iOD O)

lOJ

H030

TO ACCOMPANY

A GEOLOGICAL REPORT BY M. MORRISON

:--. I b


PLEASE SEE MAP V88-3A FOR GEOLOGICAL LEGEND

50 IOO 20O m

42E11NW0202 2.11030 VIVIAN 210

cm - 2 5m2OO 4OO ft 5^

l in s 208 ft


GERALDTON AREA , THUNDER BAY M. D. , ONT.

GEOLOGY

Ml NERAL CLAIMS TB975 326~ 329 t 331 - 334 , 338-34

VI VI AN TOWNSHIP

GEOLOGY BY MM.

DRAWN BY M.M. , AH.

JANUARY 1 988

SCALE l : 250O

NT. S. 42-E-IIV

MAP V - 88 - 3B

17 N

r*oG

N)to

IS! ts) U1

morn

N* -J CB

m•o u; o

FIRST ORDER MAGNETIC ANOMALIES (iRON FORMATION ? )

SECOND ORDER MAGNETIC ANOMALIES (iRON FORMATION ? )


PLEASE SEE MAP V-87-1A FOR CONTOURED MAGNETOMETER SURVEY RESULTS

42E11NW0202 2,11030 V IVIAN

MAGNETIC DECLINATION

l 0 30' WEST

14 N

13 N

12 N

11 N

10 N BASELINE

9 NLEGEND

B N

ROADS

MUSKEG

CREEKS

-STATIONS ON GRID LINES

INTERMEDIATE READINGS

7 N

2. 1103050 100 200 m

6 N

400 ft1 cm = 25m

200 -±

1 in s 208 ft

TO ACCOMPANY A GEOPHYSICAL REPORT BY M. MORRISON

VIVIAN TOWNSHIP PROPERTYGERALDTON AREA THUNDER BAY M. D. . ONT.

GROUND MAGNETOMETER

INTERPRETATION

MINERAL CLAIMS TB 875 326 VIVIAN TOWN SHIP

SURVEY

- 3 44

SURVEY BY M.M.

DRAWN BY M.M., AH.

APRIL 1987

SCALE 1'2500

NTS. 42-E-11W

MAP V-87-2A

17 N

16 N

15 N

Mt- N

13 N

12 N

if K M TO HIGHWAY 11

iMAGNETIC DECLINA1

1" 30 WEST

LEGEND

STATIONS ON GRID LINES

INTERMEDIATE READINGS

11 N

10 N

9 N

e N

Di—O

T)

lGO-O

l

7 N

2. 110306 N

TO ACCOMPANY A GEOPHYSICAL REPORT BY M. MORRoo

rn m

"O

rnO m

IS)

m

f-

m

FIRST ORDER MAGNETI C ANOMALIES (iRON FORMATION ?)

SECOND ORDER MAGNET! C ANOMALIES (l RON FORMATION ?)


PLEASE SEE MAP V-87-2A FOR CONTOURED MAGNETOMETER SURVEY RESULTS

50 100 200 m

42E11NW0202 2.11830 VIVIAN

1 cm - 2 5m200 400 ft H h

1 \ r\ - 208 ft230

VIVIAN TOWNSHIP PROPERTYGERALDTON AREA THUNDER BAY M. D. , ONT

GROUND MAGNETON ETER

INTERPRETATION

MINERAL CLAIMS VIVIAN

T B 875 326 TOWNSHIP

SURVE

- 3 k if

SURVEY BY M.M.

DRAWN BYM.M., A.H.

APRIL 1987

SCALE 1^ 2500

NTS. 42-E

MAP V - 67

7N

16 N

— 15 N

14 N

3N

I2N

— II N

ON

— 9 N

— 8 N

— 7 N

GD lO

t00 GOi >

Q.

CO Z

o-3a

ro00m

rotDm

OJom

— 6 N

CLAIM POSTS WERE TIED IK WITH COMPASS AND BELT CHAIN

PLEASE SEE MAP V-88-4A FOR FRASER FILTERED DATA

PLEASE SEE MAP V-88-3A FOR GEOLOGY

MAG NET l C DEC LI N ATI ON

l 0 3O ' WEST

N-PHASE READINGS QUADRATURE READINGS

60 40 20 0-20-40 -60

QUADRATURE PROF l LE

N-PHASE PROFILE

NSTRUMENT : GEONICS EM,- 16

READINGS TAKEN FA C l NG NORTH

2. 11030

^4, /*V

TO ACCOMPANY A GEOPHYSICAL REPORT BY M. MORRISON

50 100 200 m

42E11NW82e2 VIVIANl in ~ 2O8 ft

240



VLF-EM SURVEYBASIC DATA a PROFILES

MINERAL CLAIMS T B875 330, 335-337, 342" 344

Vt VI AN TOWNSHIP

SURVEY BY M.M

DRAWN BY M.M., AH

JANUARY 1988

SCALE l : 2500

NTS 42- E* H W

MAP V-88-5A

o m

I7N

!6N

15 N

14 N

I3N

12 N

N

ION

9N

8 N

7 N

rn

6 N

wt. f \4 KM TOvHIGHWAY II

QUADRATURE READINGSIN-PHASE READINGS

QUADRATURE PROF l LE

IN-PHASE PROFILE

42EI1NWC2&2 2 .11038 V IVIAN

60 40 20 O -20-40 -60lcm - 2 O "/o


PLEASE SEE MAP V-88-4B FOR FRASER FILTERED DATA

PLEASE SEE MAP V-88-3B FOR GEOLOGY

MAGNETI C DECLI NATI ON

l 0 30' WEST

OC-OZ C/)

TJ

00 OD

l01

1030

TO ACCOMPANY

A GEOPHYSICAL REPORT BY M. MORRISON

5O IOO 200 m

NSTRUMENT GEONICS EM-16

READINGS TAKEN FACING NORTH

250

cm s 25m

2OO

l i n ~ 208 f t

4OO ft



VLF-EM SURVEYBASIC DATA PROFILES

MINERAL CLAIMS TB875 326-329,331-334,338-341

VIVIAN TOWNSHI P

SURVEY BY M.M.

DRAWN BY MM f A.M.

JANUARY 1988

SCALE t : 250O

NT.S. 42-E -HW

MAP V - 88 -58

7N

16 N

15 N

4 N

3N

2N

N

—— ION

— 9 N

— 8 N

— 7 N

6 N

m sr t

CO CO

Q.

C/)Z

O

Q

OD

mto m

Om

ro m

PO rom

ro oJm

ro 4* m

ro dm

en m

ro Nm

ro CDm

ro(Dm

OJo m

17


PLEASE SEE MAP v-as-3A FOR GEOLOGY

WAGNETI C DECLI N ATI ON

l 0 30' WEST

INSTRUMENT: G EON l C S EM- l 6

PLEASE SEE BASIC DATA ON MAP V88-5A

CONTOUR INTERVAL: 0,20,40,80, ISO Vo

FRASER FILTERED DIP ANGLE

———— ————— ————— AXES OF CONDUCTORS

2. 1 1030

TO ACCOMPANY A GEOPHYSICAL REPORT BY M MORRISON

50 100 200 m

42E1tNWese2 2.11039 VIVIAN

cm - 25m

200 400 ft-tasss*

n - 208 f T260

ZYGOTE RESOURCES LTD.


GERALDTON ARtA , THUNDER BAY M D , O N T.

VLF-EM SURVEY FRASER FILTERED DATA

MINERAL CLAIMS TB875 330, 335-337, 342' 344

VI V l AN TOWNSHI P

SURVEY BY M.M

DRAWN BY M.M , A H

JANUARY I988

SCALE 25OO

NTS 42- E- M W

MAP v - ea-4A

7N

16 N

15 N

14 N

3N

12 N

N

ION

9N

8 N

7 N

6 N

Om

KM TO HIGHWAY II

±5753*

- sre 8 75334

NST RUMENT: GEONICS EM'16

PLEASE SEE BASIC DATA ON MAP V-88-5B

CONTOUR INTERVAL : O , 20 . 40 . 80 , l 60 "/o

FRASER FI L T E RED DIP ANGLE

AXES OF CONDUCTORS

MAG NE TIC DECLINATION

l 0 30* WEST

OC-OZ C/)

"D

00OD

i-P*

2. 11030

TO ACCOMPANY

A GEOPHYSICAL REPORT BY M MORRISON


PLEASE SEE MAP V-88-3B FOR GEOLOGY

5O IOO 2OO m

42E11NW8242 2 .11030 VIVIAN 270l in : 208 f f



VLF-EM SURVEY FRASER FILTERED DATA

Ml NERAL CLAIMS TB875 326 - 3 29 , 331 - 3 34 . 338-341

VIVIAN TOWNSHIP

SURVEY BY M. M.

DRAWN BY M.M. , AH.

JANUARY 1988

SCALE l : 2500

N T. S. 42 - E - 11 W

MAP V - 88-4B

I7N

16 N

15 N

14 N

12 N

M N

ION

9N

8 N

7 N

6 N

O m rn

KM TO HIGH WAY M


PLEASE SEE MAP V-88-3B FOR GEOLOGYppb Au

25

As ppm

ARSENIC CONTOURED AT l O , 20 , 4O , 80 PPM

GOLD NOT CONTOURED

N.S. DENOTES NO SAMPLE

50 100

42E11NW0202 2.11830 V IVIAN 280

l cm - 2 5m 200-tea

l in : 208 f T

MAGNETIC DECLINATION

l 0 30' WEST

TO ACCOMPANY

A GEOCHEMICAL REPORT BY M. MORRISON

200 m

400 ft

ZYGOTE RESOURCES LTD.VIVIAN TOWNSHIP P ROPERTY

GERALDTON AREA , THUNDER BAY M. D. t ONT.

GEOCHEMICAL SURVEYGOLD AND ARSENIC IN SOIL

MINERAL CLAIMS TB875326- TB 875326,TB675341

VIVIAN TOWNSHIP

SURVEY BY M. M.

DRAWN BY MM. , A.M.

JANUARY 1988

SCALE l - 2 5OO

NTS. 42-E-MW

MAP V-88-6B

m m

I7N

16 N

15 N

14 N

I3N

12 N

N

ION

9N

8 N

7 N

6 N

4 KM TO HIGHWAY II

MAG NET! C D EC LI NATION

T 30' WEST

TO ACCOMPANY

A GEOCHEMICAL REPORT BY M. MORRISON


PLEASE SE'E MAP V-88-3B FOR GEOLOGY

2.63

Pb in ppm Fe in

N.S. DENOTES NO SAMPLE

10 ppm lead

2.SO "/o iron

4.60 "/o i ron

5O IOO 200 m

42E11NWe282 2 .11038 VIVIAN

cm ~ 2 S m

200 400 ft1

in : 208 ft



GEOCHEMICAL SURVEYLEAD AND IRON IN SOIL

MINERAL CLAIMS TB875326-328 , TB87534I

VIVIAN TOWNSHIP

SURVEY BY M. M.

DRAWN BY M.M. , A.M.

JANUARY 1986

SCALE l : 2800

NTS. 42-E- It W

MAP V -88-7B

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