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Michael T.D. Wingate

Researcher at Geological Survey of Western Australia

Publications -  156
Citations -  9312

Michael T.D. Wingate is an academic researcher from Geological Survey of Western Australia. The author has contributed to research in topics: Zircon & Craton. The author has an hindex of 50, co-authored 153 publications receiving 8286 citations. Previous affiliations of Michael T.D. Wingate include University of Western Australia & Australian National University.

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Book ChapterDOI

Accretionary growth and crust formation in the Central Asian Orogenic Belt and comparison with the Arabian-Nubian shield

TL;DR: Kroner, A., Windley, B.T. as discussed by the authors, 2007, Accretionary growth and crust formation in the Central Asian Orogenic Belt and comparison with the Arabian-Nubian shield, in Hatcher, R.D., Jr., Carlson, M.M., Gruschka, S., Khain, E.V., Demoux, A.
Journal ArticleDOI

Global record of 1600–700 Ma Large Igneous Provinces (LIPs): Implications for the reconstruction of the proposed Nuna (Columbia) and Rodinia supercontinents

TL;DR: In this paper, the authors review the record of large igneous provinces (LIPs) emplaced during the 1600-700-Ma interval and identify such spatially separated but coeval LIPs at 1460, 1380, 1270, and 1115-1070-Ma.
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Ion microprobe U–Pb ages for Neoproterozoic basaltic magmatism in south-central Australia and implications for the breakup of Rodinia

TL;DR: In this paper, the age of the Gairdner dyke swarm (GDS) is estimated to be at least 40 times older than the intrusions of North America and therefore cannot have been emplaced during the same event, and it has been proposed that the GDS and related rocks in Australia are roughly coeval with mafic igneous rocks in similar stratigraphic position in the Lower Sinian System.
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Models of Rodinia assembly and fragmentation

TL;DR: In this article, a new model of Rodinia is proposed, integrating the most recent palaeomagnetic data with current stratigraphic, geochronological and tectonic constraints from around the world.
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Age and palaeomagnetism of the Mundine Well dyke swarm, Western Australia: implications for an Australia–Laurentia connection at 755 Ma

TL;DR: In this article, the authors employed integrated U-Pb geochronology and palaeomagnetic studies of the Mundine Well dyke swarm (MDS) of the Pilbara Craton, Western Australia, to test the hypothesis that Australia and Laurentia were joined as part of the Rodinia supercontinent.