Hydrothermal alteration, contact metamorphism, and authigenesis in Ferrar Supergroup and Beacon Supergroup rocks, Carapace Nunatak, Allan Hills, and Coombs Hills, Victoria Land, Antarctica
Permian-Triassic Beacon Supergroup (dominantly quartz-rich sandstones with coal) and Jurassic Ferrar Supergroup (mafic intrusives, extrusives, and phreatomagmatic clastic rocks), in the region studied, are separated by 20 m.y. of uplift, erosion, and nondeposition. Probable pre-Ferrar secondary mine...
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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Royal Society Of New Zealand
2002
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Online Access: | http://hdl.handle.net/2292/4877 |