Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica
P(論文) 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 a...
Main Authors: | , |
---|---|
Language: | English |
Published: |
1984
|
Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/record/1633/files/KJ00000012265.pdf https://nipr.repo.nii.ac.jp/records/1633 |
_version_ | 1829301272329584640 |
---|---|
author | Nagao, Toshiyasu Kaminuma, Katsutada |
author_facet | Nagao, Toshiyasu Kaminuma, Katsutada |
author_sort | Nagao, Toshiyasu |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) 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. departmental bulletin paper |
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 |
geographic | East Antarctica Syowa Station Mizuho Yamato Mizuho Station Mizuho Plateau |
geographic_facet | East Antarctica Syowa Station Mizuho Yamato Mizuho Station Mizuho Plateau |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00001633 |
institution | Open Polar |
language | English |
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) |
op_collection_id | ftnipr |
op_relation | Memoirs of National Institute of Polar Research. Special issue 33 1 8 AA00733561 https://nipr.repo.nii.ac.jp/record/1633/files/KJ00000012265.pdf https://nipr.repo.nii.ac.jp/records/1633 |
publishDate | 1984 |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00001633 2025-04-13T14:09:24+00:00 Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica Nagao, Toshiyasu Kaminuma, Katsutada 1984-09 application/pdf https://nipr.repo.nii.ac.jp/record/1633/files/KJ00000012265.pdf https://nipr.repo.nii.ac.jp/records/1633 eng eng Memoirs of National Institute of Polar Research. Special issue 33 1 8 AA00733561 https://nipr.repo.nii.ac.jp/record/1633/files/KJ00000012265.pdf https://nipr.repo.nii.ac.jp/records/1633 1984 ftnipr 2025-03-19T10:19:56Z P(論文) 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. departmental bulletin paper Other/Unknown Material 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) |
spellingShingle | Nagao, Toshiyasu Kaminuma, Katsutada Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica |
title | 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_short | 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 |
url | https://nipr.repo.nii.ac.jp/record/1633/files/KJ00000012265.pdf https://nipr.repo.nii.ac.jp/records/1633 |