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...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2010
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/38152 |