Anatectic reworking and differentiation of continental crust along the active margin of Gondwana: A zircon Hf-O perspective from West Antarctica
The Fosdick migmatite-granite complex of West Antarctica preserves evidence of two crustal differentiation events along a segment of the former active margin of Gondwana, one in the Devonian-Carboniferous and another in the Cretaceous. The Hf-O isotope co
Published in: | Geological Society, London, Special Publications |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
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Geological Society of London
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/77706 https://doi.org/10.1144/SP383.7 https://openresearch-repository.anu.edu.au/bitstream/1885/77706/5/f5625xPUB6516_2013.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/77706/7/01_Yakymchuk_Anatectic_reworking_and_2013.pdf.jpg |
Summary: | The Fosdick migmatite-granite complex of West Antarctica preserves evidence of two crustal differentiation events along a segment of the former active margin of Gondwana, one in the Devonian-Carboniferous and another in the Cretaceous. The Hf-O isotope co |
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