A revised stratigraphic model for the 2.7 Ga Agnew-Wiluna greenstone belt, Yilgarn Craton, Western Australia

The lower stratigraphy of Agnew-Wiluna greenstone belt is composed of two main elements; a mafic/komatiite domain and a felsic/komatiite/basalt domain. Previous stratigraphic models show the mafic domain overlying the felsic domain. Komatiites in the latter host the vast majority of the nickel sulph...

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Bibliographic Details
Main Authors: Martin J. Gole, Erin Western, Alexandre Diragitch
Format: Article
Language:English
Published: Elsevier 2019-12-01
Series:Ore and Energy Resource Geology
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S266626121930001X