Origin and emplacement of a middle Cretaceous gneiss dome, Fosdick Mountains, West Antarctica
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
Main Authors: | , , , |
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Format: | Book Part |
Language: | unknown |
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Geological Society of America Inc
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Online Access: | http://hdl.handle.net/1885/87237 https://doi.org/10.1130/0-8137-2380-9.267 |