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...
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Department of Geography, Mie University
1993
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ftnipr:oai:nipr.repo.nii.ac.jp:00002723 2023-05-15T13:49:00+02:00 UPLIFT OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA イワタ シュウジ Shuji IWATA 1993-09 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 en eng Department of Geography, Mie University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2723 http://id.nii.ac.jp/1291/00002723/ AA1072335X Proceedings of the NIPR Symposium on Antarctic Geosciences, 6, 116-125(1993-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2723&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1993 ftnipr 2022-11-26T19:42:11Z 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. The denudational depth and extent of ice load subsidence were inferred from topographic cross sections of subglacial topography. The total mean erosion depth during 30Ma since the preglaciation was approximated 1.3km with an associated rebound of 1.1km. As a result of the uplift, the summit altitude in the preglacial time is estimated to have been 2.1km above the present sea level. The average rates of the denudation and surface uplift are 43m/Ma and 37m/Ma, respectively. Report Antarc* Antarctica East Antarctica National Institute of Polar Research Repository, Japan East Antarctica Sør Rondane Mountains ENVELOPE(25.000,25.000,-72.000,-72.000) Sør-Rondane ENVELOPE(25.000,25.000,-72.000,-72.000) |
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Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
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. The denudational depth and extent of ice load subsidence were inferred from topographic cross sections of subglacial topography. The total mean erosion depth during 30Ma since the preglaciation was approximated 1.3km with an associated rebound of 1.1km. As a result of the uplift, the summit altitude in the preglacial time is estimated to have been 2.1km above the present sea level. The average rates of the denudation and surface uplift are 43m/Ma and 37m/Ma, respectively. |
format |
Report |
author |
イワタ シュウジ Shuji IWATA |
spellingShingle |
イワタ シュウジ Shuji IWATA UPLIFT OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
author_facet |
イワタ シュウジ Shuji IWATA |
author_sort |
イワタ シュウジ |
title |
UPLIFT OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
title_short |
UPLIFT OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
title_full |
UPLIFT OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
title_fullStr |
UPLIFT OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
title_full_unstemmed |
UPLIFT OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
title_sort |
uplift of the sør rondane mountains, east antarctica |
publisher |
Department of Geography, Mie University |
publishDate |
1993 |
url |
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 |
long_lat |
ENVELOPE(25.000,25.000,-72.000,-72.000) ENVELOPE(25.000,25.000,-72.000,-72.000) |
geographic |
East Antarctica Sør Rondane Mountains Sør-Rondane |
geographic_facet |
East Antarctica Sør Rondane Mountains Sør-Rondane |
genre |
Antarc* Antarctica East Antarctica |
genre_facet |
Antarc* Antarctica East Antarctica |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2723 http://id.nii.ac.jp/1291/00002723/ AA1072335X Proceedings of the NIPR Symposium on Antarctic Geosciences, 6, 116-125(1993-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2723&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250302739054592 |