PSEUDOTACHYLITE FROM McINTYRE ISLAND, ENDERBYLAND, EAST ANTARCTICA : EVIDENCE FOR A RAPID CRYSTALLIZATION
P(論文) Pseudotachylite from McIntyre Island in Enderby Land, East Antarctica, occurs in a breccia zone composed of black material with glassy luster and fragments of host pyroxene gneiss which has undergone ultra-high temperature metamorphism as a constituent of the Archean Napier Complex. Under the...
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Language: | English |
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National Institute of Polar Research
1996
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Online Access: | https://nipr.repo.nii.ac.jp/record/2824/files/KJ00002409871.pdf https://doi.org/10.15094/00002824 https://nipr.repo.nii.ac.jp/records/2824 |