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Origin and emplacement of a middle Cretaceous gneiss dome, Fosdick Mountains, West Antarctica

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Siddoway, Christine Smith
Richard, Stephen
Fanning, Christopher
Luyendyk, Bruce

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Geological Society of America Inc

Abstract

The Fosdick Mountains, West Antarctica, form an 80 × 15 km migmatite dome comprising massive paragneisses that exhibit polyphase fabrics, nappe-scale folds that involve granodiorite to leucogranite intrusions, and diatexite. High strain zones developed o

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Book Title

Gneiss Domes in Orogeny

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