PSEUDO MAGNETIC ANOMALIES IN THE ANTARCTIC SEA
Pseudo magnetic anomaly in the Antarctic Sea has been calculated using the gravity data derived from altimetric geoid. Comparison of the pseudo magnetic anomaly thus calculated with the theoretical magnetic anomaly predicted from topography has been made with respect to the large fracture zones comp...
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Japan Marine Science and Technology Center
1988
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ftnipr:oai:nipr.repo.nii.ac.jp:00002560 2023-05-15T13:48:59+02:00 PSEUDO MAGNETIC ANOMALIES IN THE ANTARCTIC SEA マツモト タケシ カミヌマ カツタダ Takeshi MATSUMOTO Katsutada KAMINUMA 1988-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2560 http://id.nii.ac.jp/1291/00002560/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2560&item_no=1&attribute_id=18&file_no=1 en eng Japan Marine Science and Technology Center National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2560 http://id.nii.ac.jp/1291/00002560/ AA1072335X Proceedings of the NIPR Symposium on Antarctic Geosciences, 2, 41-45(1988-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2560&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1988 ftnipr 2022-11-19T19:41:20Z Pseudo magnetic anomaly in the Antarctic Sea has been calculated using the gravity data derived from altimetric geoid. Comparison of the pseudo magnetic anomaly thus calculated with the theoretical magnetic anomaly predicted from topography has been made with respect to the large fracture zones composed of short-wavelength ridges and troughs in the Southeastern Pacific, which shows that these two anomalies coincide well with each other. Gravity anomaly calculated from topography only also coincides well with that observed with respect to the fracture zones. Report Antarc* Antarctic National Institute of Polar Research Repository, Japan Antarctic The Antarctic Pacific |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
Pseudo magnetic anomaly in the Antarctic Sea has been calculated using the gravity data derived from altimetric geoid. Comparison of the pseudo magnetic anomaly thus calculated with the theoretical magnetic anomaly predicted from topography has been made with respect to the large fracture zones composed of short-wavelength ridges and troughs in the Southeastern Pacific, which shows that these two anomalies coincide well with each other. Gravity anomaly calculated from topography only also coincides well with that observed with respect to the fracture zones. |
format |
Report |
author |
マツモト タケシ カミヌマ カツタダ Takeshi MATSUMOTO Katsutada KAMINUMA |
spellingShingle |
マツモト タケシ カミヌマ カツタダ Takeshi MATSUMOTO Katsutada KAMINUMA PSEUDO MAGNETIC ANOMALIES IN THE ANTARCTIC SEA |
author_facet |
マツモト タケシ カミヌマ カツタダ Takeshi MATSUMOTO Katsutada KAMINUMA |
author_sort |
マツモト タケシ |
title |
PSEUDO MAGNETIC ANOMALIES IN THE ANTARCTIC SEA |
title_short |
PSEUDO MAGNETIC ANOMALIES IN THE ANTARCTIC SEA |
title_full |
PSEUDO MAGNETIC ANOMALIES IN THE ANTARCTIC SEA |
title_fullStr |
PSEUDO MAGNETIC ANOMALIES IN THE ANTARCTIC SEA |
title_full_unstemmed |
PSEUDO MAGNETIC ANOMALIES IN THE ANTARCTIC SEA |
title_sort |
pseudo magnetic anomalies in the antarctic sea |
publisher |
Japan Marine Science and Technology Center |
publishDate |
1988 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2560 http://id.nii.ac.jp/1291/00002560/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2560&item_no=1&attribute_id=18&file_no=1 |
geographic |
Antarctic The Antarctic Pacific |
geographic_facet |
Antarctic The Antarctic Pacific |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2560 http://id.nii.ac.jp/1291/00002560/ AA1072335X Proceedings of the NIPR Symposium on Antarctic Geosciences, 2, 41-45(1988-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2560&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250279925186560 |