With all due respect JD,you posted this on NOT forum several days ago:
The first striking point is that DE2 is a different type of deposit structure than DE1…DE2 is “Shear Hosted Deposit”..It is very similar to DE1 in Minerals and Sulfides content , except that DE@ contains in addition ,Chromite, both in layers and veins, as well as notable increases in Pyrrhotite , Magnetite and Large Crystals of Pentlandite, in addition to the regular sulfides found at DE1….
So you agree that DE2 has very similar "Minerals and Sulfides"content,2 kms. removed from DE1 but seem to doubt that this occurance of pentlandite and chalcopyrite would be present in an anomaly that is a mere 500 meters from DE1 and apparently connected.This opinion,you state,is based on the color(red) of the conductor anomaly.FYI, I see plenty of"red"zones on FNC's map.
cs