Bottom Morphology and Tectonics of the Southern Ocean
P(論文) The paper gives the brief characteristics of the main bottom morpho-structures, revealed as the result of geomorphological analysis and according to separate geophysical data taken by expeditions of different countries. Differences in the type of the earth's crust under ocean floor serve...
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ftnipr:oai:nipr.repo.nii.ac.jp:00000087 2024-09-09T19:08:31+00:00 Bottom Morphology and Tectonics of the Southern Ocean Zhivago, Alexander V. 1967-02 application/pdf https://nipr.repo.nii.ac.jp/record/87/files/KJ00000000939.pdf eng eng Japanese Antarctic Research Expedition scientific reports. Special issue 1 124 135 AA00246775 https://nipr.repo.nii.ac.jp/record/87/files/KJ00000000939.pdf 1967 ftnipr 2024-06-17T04:04:30Z P(論文) The paper gives the brief characteristics of the main bottom morpho-structures, revealed as the result of geomorphological analysis and according to separate geophysical data taken by expeditions of different countries. Differences in the type of the earth's crust under ocean floor serve as the main taxonomic principle. Thus the shelf on the margin of Antarctica is characterized by purely continental features. To the transition continental-oceanic area belong the continental slopes, the zones of island arcs and the basins of marginal seas. Structure areas of the oceanic crust are represented by gigantic depressions of oceanic basins and arched uplifts of oceanic swells, by linear folded-block elevations of median ridges, by oceanic trenches and their marginal swells. Seven bathymetrical, geomorphological and tectonic maps have been compiled for "The Atlas of the Antarctic". departmental bulletin paper Other/Unknown Material Antarc* Antarctic Antarctica Southern Ocean National Institute of Polar Research Repository, Japan Antarctic Southern Ocean The Antarctic |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
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ftnipr |
language |
English |
description |
P(論文) The paper gives the brief characteristics of the main bottom morpho-structures, revealed as the result of geomorphological analysis and according to separate geophysical data taken by expeditions of different countries. Differences in the type of the earth's crust under ocean floor serve as the main taxonomic principle. Thus the shelf on the margin of Antarctica is characterized by purely continental features. To the transition continental-oceanic area belong the continental slopes, the zones of island arcs and the basins of marginal seas. Structure areas of the oceanic crust are represented by gigantic depressions of oceanic basins and arched uplifts of oceanic swells, by linear folded-block elevations of median ridges, by oceanic trenches and their marginal swells. Seven bathymetrical, geomorphological and tectonic maps have been compiled for "The Atlas of the Antarctic". departmental bulletin paper |
author |
Zhivago, Alexander V. |
spellingShingle |
Zhivago, Alexander V. Bottom Morphology and Tectonics of the Southern Ocean |
author_facet |
Zhivago, Alexander V. |
author_sort |
Zhivago, Alexander V. |
title |
Bottom Morphology and Tectonics of the Southern Ocean |
title_short |
Bottom Morphology and Tectonics of the Southern Ocean |
title_full |
Bottom Morphology and Tectonics of the Southern Ocean |
title_fullStr |
Bottom Morphology and Tectonics of the Southern Ocean |
title_full_unstemmed |
Bottom Morphology and Tectonics of the Southern Ocean |
title_sort |
bottom morphology and tectonics of the southern ocean |
publishDate |
1967 |
url |
https://nipr.repo.nii.ac.jp/record/87/files/KJ00000000939.pdf |
geographic |
Antarctic Southern Ocean The Antarctic |
geographic_facet |
Antarctic Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Antarctica Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctica Southern Ocean |
op_relation |
Japanese Antarctic Research Expedition scientific reports. Special issue 1 124 135 AA00246775 https://nipr.repo.nii.ac.jp/record/87/files/KJ00000000939.pdf |
_version_ |
1809822748651814912 |