High-temperature granite magmatism, crust-mantle interaction and the mesoproterozoic intracontinental evolution of the Musgrave Province, Central Australia

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High-temperature granite magmatism, crust-mantle interaction and the mesoproterozoic intracontinental evolution of the Musgrave Province, Central Australia

The Musgrave Province lies at the convergence of major structural trends formed during the Proterozoic amalgamation of the North, West and South Australian Cratons prior to c. 1290 Ma. The Musgrave Orogeny, one of three Mesoproterozoic orogenies to affect the province, produced the granites of the P...

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Bibliographic Details
Main Authors:	Smithies, R., Howard, H., Evins, P., Kirkland, Chris, Kelsey, D., Hand, M., Wingate, M., Collins, A., Belousova, E.
Format:	Journal Article
Published:	2011
Online Access:	http://hdl.handle.net/20.500.11937/3490

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