UPLIFT OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
P(論文) The Sør Rondane Mountains, East Antarctica, originated from a marginal swell formed during the breakup of Gondwanaland, and the area is now in isostatic equilibrium. Altitude of the mountains is estimated to be controlled by the isostatic rebound associated with glacial denudation and ice load...
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Language: | English |
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National Institute of Polar Research
1993
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Online Access: | https://nipr.repo.nii.ac.jp/record/2723/files/KJ00002368353.pdf https://doi.org/10.15094/00002723 https://nipr.repo.nii.ac.jp/records/2723 |