VMS mineralization in the Yilgarn Craton

VMS mineralization in the Yilgarn Craton, Western Australia
Excerpt, conclusions page 62:
”Petrochemically prospective felsic rocks have been recognized in several areas across the Yilgarn Craton, most of which are associated with base metal occurrences (e.g. Copper Hills, Dalgaranga, and Windimurra) or HFSE-enriched intrusions (e.g. Twin Peaks greenstone belt). Additional areas which appear to be prospective for VMS mineralization, based on the prospectivity parameters described in this report, include but are not limited to: Abbotts, Big Bell, Gullewa, Lake Weelhamby, Koolanooka and Marda in the Youanmi Terrane; Bore Well in the Kurnalpi Terrane; and Tobin Hill in the Yamarna Terrane. Areas of prospective crust have been defined using Zr/Y, La/Yb and Th/Yb ratios that are broadly equivalent to the Cue and Kurnalpi rift zones.”

https://geodocs.dmirs.wa.gov.au/Web/documentlist/3/Combined/N16BM

A new period of volcanogenic massive sulfide formation in the Yilgarn: a volcanological study ofthe ca 2.76 Ga Hollandaire VMS deposit, Yilgarn Craton, Western Australia
Excerpt:
”The Archean Hollandaire volcanogenic massive sulfide deposit is a felsic–siliciclastic VMS deposit located in the Murchison Domain of the Youanmi Terrane, Yilgarn Craton, Western Australia.”

”The ca 2.76 Ga Hollandaire VMS deposit, Yilgarn Craton, Western Australia Range up as far as the Abbots greenstone belt breccias. in the north.”

https://eprints.qut.edu.au/81602/

DYOR,

Kind regards