5SF85SE«e3« 63.4546 ROWAN LAKE
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Report on The Humus Soil Geochem
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Property of Golden Transit Resources Jhc.
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Area of Nolan
Otterskin Lakes
District of Kenora, Kenora Mining Division
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N.T.S. 52-F-5
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Whitby, Ontario
December 27, 1984
Introduction;
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A program of collecting humus geochem samples was performed
over a limited portion of the claim group during >nily 12 to 28, 1984
and August 25 to 27, 1984 inclusive '(near'i- conductors)
in order to •.
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establish the value of such a survey.
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Result* appear to be
favourable to continuing the program over the remainder of the
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property when time permits.
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The correspondence of higher than
background ppb Au to some of the VLF corxJuctorB as well as
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correspondence to favourable geology favoum further
follow-op as
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October 14, 1983.
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Property
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The property consists of twenty-five <25) contiguous
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unpatented mining claims located in the Kenora Mining DiviafUxi,
District of Kenora.
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The claims are numbered K 754 539 to 563 induslve and can be
found on government daim maps M2473 and M 2580. , .;
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Regional Geology
The regional geology is predominately schistose mafic Keewatin
metavolcanics overlain by intermediate
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interlayers of mafic to gabbcoic sills.
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These rocks were then
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folded into anticline and syncline assemblages with an east to
northeast trending axial plane.
The recks were intruded by <
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Quartz-feldspar dykes and sills.
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Humus Geochem Survey
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One hundred and sixty (160) humus geochem aafflpTae were
collected in a limited area with preference to areas with VLF
conductors.
AE samples were assayed foir ppb old. Tivej laethod
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used for analysis being Fire Assay/Carbon Rod using aqua i^egia for
extraction.
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Sample weight being' 10 grams unLaas '*''•,•..--r
otherwise
stated with the:
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^.'-'"^.- -^'"E-->*."''„•"' -.-yi.'., l7 'i^- •'. ' 'v-detection limit being 2 ppb Au.
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Results of The Humus Geochem Survey
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A strong correlation exists between the Humus Geochem
Survey, VLF conductor D and the rhyolite horizon opritaining the
pyrite mineralized outcrop at 32E, 1 -I- SON.
The geochem abomaly1
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appears to continue to the NE, towai^ conductor C, although no
humus sampling was performed in this area to substantiate a
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continuing trend towards the conductor.
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A. • weaker
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continues west along this same anomalous '-;^ec^^.;'|i^M'\ii^waxidl8;:
the old trench workings.
Additional detailed humus sampilj^ in the trench area may
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further expand the anomaly in this area.
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Cc«ductors A and F
appear as shear related with most of these cxsnductctt being in the
lakes.
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Conclusions
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With the limited amount of humus geochem work done, it would
appear that the survey has some mertis CM the pitiparty.
Higher
than background values being associated with VLF coiiductor D and
the old trench workings,
nt is recommended that the remaining
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portion of unsurveyed ground be completed next year (1985)
if
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recommended drilling on the VLF conductors is encouraging.
Geology Report dated December 27, 1984).
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Recommendations
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Diamond drilling of conductor B, c and p as well as the old
pit area as outlined in the Geological
1984.
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63.4546 ROWAN LAKE
CONSISTS
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