An isotopic perspective on growth and differentiation of Proterozoic orogenic crust: From subduction magmatism to cratonization

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An isotopic perspective on growth and differentiation of Proterozoic orogenic crust: From subduction magmatism to cratonization

The in situ chemical differentiation of continental crust ultimately leads to the long-term stability of the continents. This process, more commonly known as ‘cratonization’, is driven by deep crustal melting with the transfer of those melts to shallower regions resulting in a strongly chemically st...

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Bibliographic Details
Main Authors:	Johnson, S., Korhonen, F., Kirkland, Chris, Cliff, J., Belousova, E., Sheppard, S.
Format:	Journal Article
Published:	Elsevier BV 2017
Online Access:	http://hdl.handle.net/20.500.11937/22112

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