META-ULTRAMAFIC ROCK FROM THE AUSTKAMPANE AREA OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
P(論文) In the Austkampane area of the S∅r Rondane Mountains, East Antarctica, a meta-ultramafic rock occurs as a lenticular block enclosed within the host garnet-biotite gneiss of the granulite facies. The rock consists of olivine, orthopyroxene, amphibole, spinel, apatite, ilmenite, magnetite, chalc...
Main Authors: | , , , , , |
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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/2822/files/KJ00002409869.pdf https://doi.org/10.15094/00002822 https://nipr.repo.nii.ac.jp/records/2822 |