Modeling multiple melt loss events in the evolution of an active continental margin

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Modeling multiple melt loss events in the evolution of an active continental margin

The Fosdick migmatite–granite complex in West Antarctica records evidence for crustal melting during two periods of tectonism along the East Gondwana margin. Initial high-temperature metamorphism in the Devonian–Carboniferous (M1) was broadly contemporaneous with emplacement of calc-alkaline arc mag...

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Bibliographic Details
Main Authors:	Korhonen, Fawna, Saito, S., Brown, M., Siddoway, C.
Format:	Journal Article
Published:	Elsevier Science BV 2010
Subjects:	Mineral equilibria modeling Melt loss East Gondwana Migmatites Partial melting
Online Access:	http://hdl.handle.net/20.500.11937/38152

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