gold recovery, page-83

DD,
Even the JRV reports say -

" The source of the nickel/cobalt mineralisation is the Wambidgee Serpentinite of Cambrian age. The serpentinites (originally harzburgites) have intruded the Jindalee Beds in elongate north-south bodies associated with faulting.
Regionally the serpentinites are mapped from Grenfell in the north to Tumut in the south, a distance of 150 kilometres. In the Young/Cootamundra area they are flanked on the eastern side by the Silurian, Young Granodiorite. It is believed that this is an important factor in the formation of the mineralised laterites. "

This gem makes me think the JRV may have a winner on their hands -

" A further feature of the cross section shown is that the mineralisation can spread laterally across the underlying serpentinite/granite contact." :-)

If JRV is on a winner, then I think INL may have done a very good thing taking these leases up.

Cheers

Datrat