HIGH-GRADE NI-CU-PT-PD-ZN-CR-AU-V-TI DISCOVERIES IN THE "RING OF FIRE"

NI 43-101 Update (September 2012): 11.1 Mt @ 1.68% Ni, 0.87% Cu, 0.89 gpt Pt and 3.09 gpt Pd and 0.18 gpt Au (Proven & Probable Reserves) / 8.9 Mt @ 1.10% Ni, 1.14% Cu, 1.16 gpt Pt and 3.49 gpt Pd and 0.30 gpt Au (Inferred Resource)

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Message: Some interesting info from 43-101

Some interesting info from 43-101

posted on Jun 29, 2009 11:08PM

This paragraph is from the 43-101:

The large amounts of sulphide of ultramafic cumulate make it absolutely

clear that the Eagle One deposit formed in a magmatic conduit. No magma could have carried

the observed amount of sulphide in solution; therefore the sulphides have been left behind by a

through-going volume of magma much greater than what presently remains in the intrusion.

And today we have the proof of what Prof Mungall theorized in the 43-101!

Here is a picture of the Voisy'Bay deposit in cross section:

OK, I could not post this picture here, could someone more savy please put up that picture. It can be found on page 20/119 in the 43-101. TIA.

Glorieux

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