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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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- 11 -
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 * .
t- ill -
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
t. 5 .
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 . . .
- 6 -
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
l
- 7 -
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 meta- volcanic-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 . . .
t
-9-
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
- 10 -
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
VIVIAN TOWNSHIP PROPERTY
(SOME DATA AFTER O.D.M. PRELIMINARY MAP P. 1 192)
l
- 11 -
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).
- 12 -
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 . . .
t
- M -
PROPERTY GEOLOGY - Continued
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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- 18 -
PROPERTY GEOLOGY - Continued
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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PROPERTY GEOLOGY - Continued
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 silt- stones 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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- 20 -
PROPERTY GEOLOGY - Continued
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.
S
- 21 -
PROPERTY GEOLOGY - Continued
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 -
PROPERTY GEOLOGY - Continued
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 -
PROPERTY GEOLOGY - Continued
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 -
DISCUSSION - Continued
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 note- able 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
VLF-EM GROUND SURVEY - 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
VLF-EM GROUND SURVEY - 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 metasedi- ments 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 -
DISCUSSION - Continued
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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75
108S
47453
124455
81251
18
2222
22222
22222
22222
23222
34422
22322
5 1 231 18 17
BIPPR
22222
22242
32222
22222
22222
23222
22222
223
VPPR
34107171
4442
34495430
132
2444187122
48SO322228
2921213129
2120224817
2223182733
3040
CAt
.07
.04
.12
.11
.07
.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
3 NO3 NO3 NO3 NO3 NO
5 NO5 NO3 NO5 NO5 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
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'•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
CLAIM POSTS WERE TIED IN WITH COMPASS AND BELT CHAIN
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
ZYGOTE RESOURCES LTD.VIVIAN TOWNSHIP PROPERTY
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 ? )
CLAIM POSTS WERE TIED IN WITH COMPASS AND BELT CHAIN
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 ?)
CLAIM POSTS WERE TIED IN WITH COMPASS AND BELT CHAIN
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
ZYGOTE RESOURCES LTD.VIVIAN TOWNSHIP PROPERTY
GERALDTON AREA , THUNDER BAY M. D. , ONT.
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
CLAIM POSTS WERE TIED IN WITH COMPASS AND BELT CHAIN
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
ZYGOTE RESOURCES LTD.VIVIAN TOWNSHIP PROPERTY
GERALDTON AREA , THUNDER BAY M. D. , ONT.
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
CLAIM POSTS WERE TIED IN WITH COMPASS AND BELT CHAIN
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.
VIVIAN TOWNSHIP PROPERTY
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
CLAIM POSTS WERE TIED IN WITH COMPASS AND BELT CHAIN
PLEASE SEE MAP V-88-3B FOR GEOLOGY
5O IOO 2OO m
42E11NW8242 2 .11030 VIVIAN 270l in : 208 f f
ZYGOTE RESOURCES LTD.VIVIAN TOWNSHIP PROPERTY
GERALDTON AREA , THUNDER BAY M. D. , ONT.
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
CLAIM POSTS WERE TIED IN WITH COMPASS AND BELT CHAIN
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
CLAIM POSTS WERE TIED IN WITH COMPASS AND BELT CHAIN
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
ZYGOTE RESOURCES LTD.VIVIAN TOWNSHIP PROPERTY
GERALDTON AREA , THUNDER BAY M. D. , ONT.
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