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Article
The tectonic setting and evolution of the 2.7 Ga Kalgoorlie–Kurnalpi Rift, a world-class Archean gold province
The Yilgarn Craton results from three major mantle input events (at ca 3.0–2.9, 2.8 and 2.7 Ga) that have interacted with > 3.0 Ga continental crust. Zircon geochronology and Sm-Nd isotopic data subdivide the ...
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Article
Open AccessNo evidence for high-pressure melting of Earth’s crust in the Archean
Much of the present-day volume of Earth’s continental crust had formed by the end of the Archean Eon, 2.5 billion years ago, through the conversion of basaltic (mafic) crust into sodic granite of tonalite, tro...
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Chapter and Conference Paper
Crustal evolution constraints on the metallogeny of the Yilgarn Craton
Improved understanding of the evolution of the Archean Yilgarn Craton, Western Australia, indicates a collage of crustal fragments formed through both autochthonous and allochthonous processes. Komatiite-assoc...
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Chapter and Conference Paper
Tectonic controls on the endowment of Archean cratons in VHMS deposits: Evidence from PB and Nd isotopes
Comparison of Pb and Nd isotopes of the well-endowed Abitibi-Wawa Subprovince with the poorly endowed Eastern Goldfields Province implies that volcanic-hosted massive sulfide (VHMS) endowment in Archean terrai...