This program was suspended due to COVID-19 containment measures.
As previously reported (Santana ASX Announcement,
To develop magmatic sulphide style mineralisation requires fluids from the mantle to migrate close to the surface and bond with sulphur. These ascending fluids can be enriched in metals such as iron, nickel, platinum, copper, and cobalt, but devoid of sulphur, which has to be added by an external source on ascension.
The intersection layers of pyrrhotite massive sulphide in holes PLDD006 and PLDD008 supports the concept that sulphur was added to the ultramafic intrusion at the Phu Lon Nickel Prospect increasing prospectivity.
Contact:
Tel: +61 (0) 417 671 301
Email: shane.pike@santanaminerals.com
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