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