Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica
The Fremouw and Falla Formations are part of a thick sequence of alluvial sediments that accumulated in a foreland basin (foredeep) between the Antarctic craton and the Gondwanian orogen, an Andean-type mountain belt along the Pacific margin of Gondwana. This study examines the petrology of Fremouw...
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Format: | Report |
Language: | English |
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Institute of Polar Studies, The Ohio State University.
1984
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Online Access: | http://hdl.handle.net/1811/48692 |