UPLIFT OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
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 loading. T...
Main Authors: | , |
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Format: | Report |
Language: | English |
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Department of Geography, Mie University
1993
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Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2723 http://id.nii.ac.jp/1291/00002723/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2723&item_no=1&attribute_id=18&file_no=1 |