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Project Overview

Project Number
Project Theme
Mineral Systems

Komatiite sequences at Honeymoon Well (in the northern part of the Agnew – Wiluna belt) and in the Walter Williams Formation (in the Siberia – Menzies – Mt. Ida region), with contrasting styles of komatiite volcanism, have been studied to add to the understanding of the physical volcanology of komatiites and improve recognition of varied volcanic environments in which nickel sulphides occur.

Page was last reviewed 7 July 2020

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