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...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Elsevier
2019-12-01
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Series: | Ore and Energy Resource Geology |
Subjects: | |
Online Access: | http://www.sciencedirect.com/science/article/pii/S266626121930001X |