Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica
Gravity survey was carried out at 303 stations in Lutzow-Holm Bay and in the Mizuho Plateau during the wintering in 1981. Using the gravity data, the crustal structure in the Lutzow-Holm Bay region and the bedrock topography in the Mizuho Plateau have been revealed in this study. The results are as...
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Earthquake Research Institute, University of Tokyo
1984
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ftnipr:oai:nipr.repo.nii.ac.jp:00001633 2023-05-15T13:47:59+02:00 Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica Toshiyasu Nagao Katsutada Kaminuma 1984-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1633 http://id.nii.ac.jp/1291/00001633/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1633&item_no=1&attribute_id=18&file_no=1 en eng Earthquake Research Institute, University of Tokyo National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1633 http://id.nii.ac.jp/1291/00001633/ AA00733561 Memoirs of National Institute of Polar Research. Special issue, 33, 1-8(1984-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1633&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1984 ftnipr 2022-11-12T19:42:29Z Gravity survey was carried out at 303 stations in Lutzow-Holm Bay and in the Mizuho Plateau during the wintering in 1981. Using the gravity data, the crustal structure in the Lutzow-Holm Bay region and the bedrock topography in the Mizuho Plateau have been revealed in this study. The results are as follows : 1) In Lutzow-Holm Bay, the thickness of the crust increases from northwest to southeast. 2) In the Mizuho Plateau, at least two subglacial valleys exist near Mizuho Station, whose strike is estimated to be consistent with the flow direction of the ice sheet. 3) In the Yamato Mountains region, the crustal thickness is larger than that in the Lutzow-Holm Bay region by about 3.8km estimated from the result of simple Bouguer anomaly difference. And the difference of the crustal thickness between Syowa and Mizuho Stations is less than 2km. Report Antarc* Antarctica East Antarctica Ice Sheet Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan East Antarctica Syowa Station Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Yamato ENVELOPE(35.583,35.583,-71.417,-71.417) Mizuho Station ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Plateau ENVELOPE(40.000,40.000,-73.000,-73.000) |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
Gravity survey was carried out at 303 stations in Lutzow-Holm Bay and in the Mizuho Plateau during the wintering in 1981. Using the gravity data, the crustal structure in the Lutzow-Holm Bay region and the bedrock topography in the Mizuho Plateau have been revealed in this study. The results are as follows : 1) In Lutzow-Holm Bay, the thickness of the crust increases from northwest to southeast. 2) In the Mizuho Plateau, at least two subglacial valleys exist near Mizuho Station, whose strike is estimated to be consistent with the flow direction of the ice sheet. 3) In the Yamato Mountains region, the crustal thickness is larger than that in the Lutzow-Holm Bay region by about 3.8km estimated from the result of simple Bouguer anomaly difference. And the difference of the crustal thickness between Syowa and Mizuho Stations is less than 2km. |
format |
Report |
author |
Toshiyasu Nagao Katsutada Kaminuma |
spellingShingle |
Toshiyasu Nagao Katsutada Kaminuma Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica |
author_facet |
Toshiyasu Nagao Katsutada Kaminuma |
author_sort |
Toshiyasu Nagao |
title |
Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica |
title_short |
Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica |
title_full |
Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica |
title_fullStr |
Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica |
title_full_unstemmed |
Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica |
title_sort |
estimation of the crustal structure and the bedrock topography by the gravitational method around syowa station, east antarctica |
publisher |
Earthquake Research Institute, University of Tokyo |
publishDate |
1984 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1633 http://id.nii.ac.jp/1291/00001633/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1633&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(44.317,44.317,-70.683,-70.683) ENVELOPE(35.583,35.583,-71.417,-71.417) ENVELOPE(44.317,44.317,-70.683,-70.683) ENVELOPE(40.000,40.000,-73.000,-73.000) |
geographic |
East Antarctica Syowa Station Mizuho Yamato Mizuho Station Mizuho Plateau |
geographic_facet |
East Antarctica Syowa Station Mizuho Yamato Mizuho Station Mizuho Plateau |
genre |
Antarc* Antarctica East Antarctica Ice Sheet Memoirs of National Institute of Polar Research Polar Research |
genre_facet |
Antarc* Antarctica East Antarctica Ice Sheet Memoirs of National Institute of Polar Research Polar Research |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1633 http://id.nii.ac.jp/1291/00001633/ AA00733561 Memoirs of National Institute of Polar Research. Special issue, 33, 1-8(1984-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1633&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766248294385713152 |