The ~2730 Ma onset of the Neoarchean Yilgarn Orogeny
Author:
Affiliation:
1. Geological Survey of Western Australia; East Perth Western Australia Australia
2. School of Earth, Atmosphere and Environment; Monash University; Clayton Victoria Australia
3. Institute of Geosciences; University of Mainz; Mainz Germany
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017TC004562/fullpdf
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1. The importance of being molten: 100 Myr of synmagmatic shearing in the Yilgarn Craton (Western Australia). Implications for mineral systems;Precambrian Research;2024-06
2. 2730–2670 Ma rifting triggers sagduction prior to the onset of orogenesis at ca 2650 Ma: implications for gold mineralisation, Eastern Goldfields, Western Australia;Australian Journal of Earth Sciences;2024-05-09
3. The Neoarchean, a turning point for geodynamic and magmatic processes within the Superior craton?;Laurentia: Turning Points in the Evolution of a Continent;2023-01-23
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5. Seismic Reflection and Potential Field Constraints on Imbrication and Exhumation of the Paleoarchean Narryer Terrane, Yilgarn Craton;Tectonics;2022-10
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