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To: Diamond Daze who wrote (3605)12/14/1999 3:48:00 PM
From: Dave Pavlik  Read Replies (1) | Respond to of 4884
 
I agree. I especially like these 2 comments.

Follow-up geochemical programs have tested over 1,200 modern
alluvium, lake sediment and glacial till samples, with results being
positive beyond expectations. Numerous well-defined indicator
mineral dispersion haloes have been identified, and in some
cases, indicator mineral counts of up to several hundred grains
per sample have been recorded. Morphological characteristics
and surface textures on the indicator minerals are consistent with
a proximal source. In addition, the presence of significant
numbers of G10 garnets and high interest chromites establishes a
positive diamond potential for the targets.

Positive beyond expectations! can't be much more positive than that!

and this

These minerals define discrete plumes
in certain areas, the best of which occur within two groups of
claims staked by the joint venture in 1999. In one area, numerous
highly subcalcic G10 garnets with compositions similar to some
of the best occurring at Lac de Gras, NWT, have been recovered.
This provides compelling evidence for the presence of richly
diamondiferous kimberlites in the region. Moreover, the
morphology and surface textures of the grains indicate that they
have undergone minimal transportation in the secondary
environment, implying that the source kimberlite(s) should be
close by.

with all these positive results they have got to hit paydirt somewhere.
or I guess that should be pay kimberlite!

Dave