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Gold/Mining/Energy : Abacus Minerals Corporation (V.AMC)
AMC 2.590+3.0%Nov 6 3:59 PM EST

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To: Mr.Staya who wrote (111)5/11/1998 5:01:00 AM
From: John Fairchild  Read Replies (1) of 397
 
Hi Ric again I am no geologist but I do enough reading to know what looks good.
AMC have done enough surface reconnaissance (along with Barrick's bulldozer trenching) to give them a pretty good idea of the minimum extent of surface mineralization is. There were as usual areas of trenching the ended in mineralization but were not extended due to overburden. Epithermal systems tend to be very large bulk tonnage and as you can see by the description below. this one is. Note also "Epithermal stockwork quartz veining similar to the trench area was
discovered approximately 2 kilometres northeast where grab samples
returned values as high as 10.7 g/t gold and 52.0 g/t silver."

From some of the old NR's

Oct 27/97
Abacus personnel accompanied by the Company's independent
engineer, Mr. Giles Peatfield, visited La Manchuria in early
October. The gold mineralization occurs in large epithermal
chalcedonic stockwork hosted in an intensely
clay-adularia-hematite-silica altered rhyolite. This intense
alteration is exposed in all three of Barrick's trenches.
Multiple phases of cross-cutting chalcedony veins, varying in size
from hairline fracture fillings to 15 centimetres in width, occur
throughout the exposures.

The stock work veining and altered rhyolite outcrop over an area
of at least 700 metres by 700 metres on a prominent silicified
ridge which protrudes 75-100 metres above the general valley
floor. The La Manchuria stock work zone appears to be open in all
directions and trends under the alluvial cover in the valley
floor.

Jan 27/98
La Manchuria Property

Work on La Manchuria included 7.2 kilometres of IP and 8.6
kilometres of CSAMT geophysical surveys, geological mapping, the
collection of approximately 575 grid soil samples, 260 prospector
rock samples and 244 trench samples.

Mapping confirms felsic volcanic rocks that host the known
epithermal mineralization extends under overburden cover both to
the north and south.

Both geophysical surveys clearly identify a large and depth
persistent zone of high resistivity straddling a weather resistant
topographic high. This is interpreted to reflect extensive
silicification of the host units. The area of this zone of
silicification as indicated by the geophysical surveys is in
excess of 200,000 square metres at 50 metres in depth with deep
seated feeder zones. Work to date including sampling and
geological mapping indicates a correlation between gold and silver
values with the amount of silicification.
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E. Charters made an apearance on this thread some time ago and made reference to how good the property looked. That was based on surface results only. Now that they have drilled and hit in one of their first two holes I beleive that a great step has been made in demonstrating the potentilial of this property.

" LM98-2 is believed to represent the
most significant discovery since the discovery of Anglo American's
Cerro Vanguardia Mine (80 kilometres east of La Manchuria) in the
mid-1980's. " This is a stong statement that obviously met VSE approval.

John
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