A nice summary from page 9.Looking forward to the forest...

A nice summary from page 9.
Looking forward to the forest drilling.
what a beast.


Eleven high-grade massive / matrix / heavily disseminated sulphide zones (G1-11) have been defined to date within the Gonneville Intrusion. The discrete high-grade PGE-Ni-Cu-Co +/- Au zones comprise sulphide- rich accumulations (10-100% sulphide, defined by >1g/t Pd cut-off) and typically have a grade range of 1- 15g/t PGE+Au, 0.5-3.3% Ni, 0.4-4.5% Cu and 0.03-0.27% Co.
The Gonneville Intrusion also hosts widespread disseminated PGE-Ni-Cu-Co mineralisation (trace to 3% sulphides, on average) surrounding the high-grade zones, which typically has a grade range of 0.5-2.0g/t PGE, 0.1-0.2% Ni, 0.05-0.15% Cu and 0.01-0.03% Co.
Weathering at Gonneville extends down to ~30-40m below surface and a well-developed saprolite (oxide) profile after serpentinite contains elevated PGE-Au grades (typically ranging from 1.2-4.5g/t PGE+Au) from near surface to a depth of ~25m.