Isostasy of the Bering Sea (Izostaziya Beringova Morya)
The study of the deep-seated structure and dynamics of the earth's crust and upper mantle requires knowledge of isostasy. Among all forms of gravity reductions, the abyssal heterogeneities are most clearly reflected in the isostatic anomalies. The analysis of the latter is especially effective...
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1971
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ftdtic:AD0728302 2023-05-15T15:06:35+02:00 Isostasy of the Bering Sea (Izostaziya Beringova Morya) Gainanov,A. G. Isaev,E. N. Stroev,P. A. Ushakov,S. A. AERONAUTICAL CHART AND INFORMATION CENTER ST LOUIS MO TECHNICAL LIBRARY SECTION 1971-06 text/html http://www.dtic.mil/docs/citations/AD0728302 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0728302 en eng http://www.dtic.mil/docs/citations/AD0728302 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Geology Geochemistry and Mineralogy (*ISOSTATIC CHANGE ARCTIC OCEAN) STRUCTURAL GEOLOGY ANOMALIES GRAVITY PACIFIC OCEAN USSR GRAVITY ANOMALIES TRANSLATIONS EARTH CRUST EARTH MANTLE Text 1971 ftdtic 2016-02-19T01:01:52Z The study of the deep-seated structure and dynamics of the earth's crust and upper mantle requires knowledge of isostasy. Among all forms of gravity reductions, the abyssal heterogeneities are most clearly reflected in the isostatic anomalies. The analysis of the latter is especially effective in the areas of the most active tectonics. One such area is the peripheral belt of the Pacific Ocean. A calculation and analysis of isostatic anomalies, pertaining to the transition area from the Asiatic and American continents to the northern part of the Pacific Ocean, were performed by the authors. The region of investigation is interesting because it includes almost all the most characteristic elements of the relief of transition zones, such as continental shelf and slope, marinal sea, island arc, abyssal trench, marginal oceanic swell, and underwater ridges. In addition, the shelf of the Bering Sea is the connecting continental link between Asia and North America, and this makes it possible to consider it as a subsided part of the continent. (Author) Trans. of Geofizicheskii Byulleten (USSR) n20 p15-19 1969, by George Synenko. Text Arctic Arctic Ocean Bering Sea Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Bering Sea Pacific |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Geology Geochemistry and Mineralogy (*ISOSTATIC CHANGE ARCTIC OCEAN) STRUCTURAL GEOLOGY ANOMALIES GRAVITY PACIFIC OCEAN USSR GRAVITY ANOMALIES TRANSLATIONS EARTH CRUST EARTH MANTLE |
spellingShingle |
Geology Geochemistry and Mineralogy (*ISOSTATIC CHANGE ARCTIC OCEAN) STRUCTURAL GEOLOGY ANOMALIES GRAVITY PACIFIC OCEAN USSR GRAVITY ANOMALIES TRANSLATIONS EARTH CRUST EARTH MANTLE Gainanov,A. G. Isaev,E. N. Stroev,P. A. Ushakov,S. A. Isostasy of the Bering Sea (Izostaziya Beringova Morya) |
topic_facet |
Geology Geochemistry and Mineralogy (*ISOSTATIC CHANGE ARCTIC OCEAN) STRUCTURAL GEOLOGY ANOMALIES GRAVITY PACIFIC OCEAN USSR GRAVITY ANOMALIES TRANSLATIONS EARTH CRUST EARTH MANTLE |
description |
The study of the deep-seated structure and dynamics of the earth's crust and upper mantle requires knowledge of isostasy. Among all forms of gravity reductions, the abyssal heterogeneities are most clearly reflected in the isostatic anomalies. The analysis of the latter is especially effective in the areas of the most active tectonics. One such area is the peripheral belt of the Pacific Ocean. A calculation and analysis of isostatic anomalies, pertaining to the transition area from the Asiatic and American continents to the northern part of the Pacific Ocean, were performed by the authors. The region of investigation is interesting because it includes almost all the most characteristic elements of the relief of transition zones, such as continental shelf and slope, marinal sea, island arc, abyssal trench, marginal oceanic swell, and underwater ridges. In addition, the shelf of the Bering Sea is the connecting continental link between Asia and North America, and this makes it possible to consider it as a subsided part of the continent. (Author) Trans. of Geofizicheskii Byulleten (USSR) n20 p15-19 1969, by George Synenko. |
author2 |
AERONAUTICAL CHART AND INFORMATION CENTER ST LOUIS MO TECHNICAL LIBRARY SECTION |
format |
Text |
author |
Gainanov,A. G. Isaev,E. N. Stroev,P. A. Ushakov,S. A. |
author_facet |
Gainanov,A. G. Isaev,E. N. Stroev,P. A. Ushakov,S. A. |
author_sort |
Gainanov,A. G. |
title |
Isostasy of the Bering Sea (Izostaziya Beringova Morya) |
title_short |
Isostasy of the Bering Sea (Izostaziya Beringova Morya) |
title_full |
Isostasy of the Bering Sea (Izostaziya Beringova Morya) |
title_fullStr |
Isostasy of the Bering Sea (Izostaziya Beringova Morya) |
title_full_unstemmed |
Isostasy of the Bering Sea (Izostaziya Beringova Morya) |
title_sort |
isostasy of the bering sea (izostaziya beringova morya) |
publishDate |
1971 |
url |
http://www.dtic.mil/docs/citations/AD0728302 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0728302 |
geographic |
Arctic Arctic Ocean Bering Sea Pacific |
geographic_facet |
Arctic Arctic Ocean Bering Sea Pacific |
genre |
Arctic Arctic Ocean Bering Sea |
genre_facet |
Arctic Arctic Ocean Bering Sea |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0728302 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
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1766338157182189568 |