Specific features of the upper sedimentary cover and slump structures in the NW Pacific and the Bering Sea based on seismoacoustic profiling data

The authors studied geology-geophysical data that had been obtained during German RV «Sonne» Cruise in NW Pacific organized in frames of the Russian-German Project KALMAR («Kurile-Kamchatka and Aleutian Marginal sea-island arc systems: geodynamic and climate interaction in space and time»). The prof...

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Main Authors: Tsukanov, N.V., Dozorova, K.A., Gaedicke, C.
Format: Article in Journal/Newspaper
Language:Russian
Published: Institute of Volcanology and Seismology FEB RAS 2019
Subjects:
Online Access:https://doi.org/10.31431/1816-5524-2019-1-41-73-8
https://doaj.org/article/ab9c0d1fb77c49169a983fbfba4aa464
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spelling ftdoajarticles:oai:doaj.org/article:ab9c0d1fb77c49169a983fbfba4aa464 2023-05-15T15:43:24+02:00 Specific features of the upper sedimentary cover and slump structures in the NW Pacific and the Bering Sea based on seismoacoustic profiling data Tsukanov, N.V. Dozorova, K.A. Gaedicke, C. 2019-04-01T00:00:00Z https://doi.org/10.31431/1816-5524-2019-1-41-73-8 https://doaj.org/article/ab9c0d1fb77c49169a983fbfba4aa464 RU rus Institute of Volcanology and Seismology FEB RAS http://www.kscnet.ru/journal/kraesc/article/viewFile/236/pdf https://doaj.org/toc/1816-5524 https://doaj.org/toc/1816-5532 doi:10.31431/1816-5524-2019-1-41-73-8 1816-5524 1816-5532 https://doaj.org/article/ab9c0d1fb77c49169a983fbfba4aa464 Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, Vol 41, Iss 1, Pp 73-84 (2019) North-Western Pacific sedimentary cover seismoacoustic profiling landslides Geology QE1-996.5 article 2019 ftdoajarticles https://doi.org/10.31431/1816-5524-2019-1-41-73-8 2022-12-31T14:53:18Z The authors studied geology-geophysical data that had been obtained during German RV «Sonne» Cruise in NW Pacific organized in frames of the Russian-German Project KALMAR («Kurile-Kamchatka and Aleutian Marginal sea-island arc systems: geodynamic and climate interaction in space and time»). The profiling was carried out using PARASOUND P70 system, including narrow-beam system and sub-bottom profiler. The study showed that besides undisturbed sedimentation, landside processes are widely spread in open areas of the ocean and the Bering Sea as well as deposits caused by strong submarine currents. Landslides were revealed on the slopes of the Emperor Ridge in the NW Pacific and the Shirshov Ridge submarine mountains, in canyons near Eastern Kamchatka coasts and apparently in many other areas. Article in Journal/Newspaper Bering Sea Kamchatka Directory of Open Access Journals: DOAJ Articles Bering Sea Pacific Shirshov Ridge ENVELOPE(171.000,171.000,57.500,57.500)
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language Russian
topic North-Western Pacific
sedimentary cover
seismoacoustic profiling
landslides
Geology
QE1-996.5
spellingShingle North-Western Pacific
sedimentary cover
seismoacoustic profiling
landslides
Geology
QE1-996.5
Tsukanov, N.V.
Dozorova, K.A.
Gaedicke, C.
Specific features of the upper sedimentary cover and slump structures in the NW Pacific and the Bering Sea based on seismoacoustic profiling data
topic_facet North-Western Pacific
sedimentary cover
seismoacoustic profiling
landslides
Geology
QE1-996.5
description The authors studied geology-geophysical data that had been obtained during German RV «Sonne» Cruise in NW Pacific organized in frames of the Russian-German Project KALMAR («Kurile-Kamchatka and Aleutian Marginal sea-island arc systems: geodynamic and climate interaction in space and time»). The profiling was carried out using PARASOUND P70 system, including narrow-beam system and sub-bottom profiler. The study showed that besides undisturbed sedimentation, landside processes are widely spread in open areas of the ocean and the Bering Sea as well as deposits caused by strong submarine currents. Landslides were revealed on the slopes of the Emperor Ridge in the NW Pacific and the Shirshov Ridge submarine mountains, in canyons near Eastern Kamchatka coasts and apparently in many other areas.
format Article in Journal/Newspaper
author Tsukanov, N.V.
Dozorova, K.A.
Gaedicke, C.
author_facet Tsukanov, N.V.
Dozorova, K.A.
Gaedicke, C.
author_sort Tsukanov, N.V.
title Specific features of the upper sedimentary cover and slump structures in the NW Pacific and the Bering Sea based on seismoacoustic profiling data
title_short Specific features of the upper sedimentary cover and slump structures in the NW Pacific and the Bering Sea based on seismoacoustic profiling data
title_full Specific features of the upper sedimentary cover and slump structures in the NW Pacific and the Bering Sea based on seismoacoustic profiling data
title_fullStr Specific features of the upper sedimentary cover and slump structures in the NW Pacific and the Bering Sea based on seismoacoustic profiling data
title_full_unstemmed Specific features of the upper sedimentary cover and slump structures in the NW Pacific and the Bering Sea based on seismoacoustic profiling data
title_sort specific features of the upper sedimentary cover and slump structures in the nw pacific and the bering sea based on seismoacoustic profiling data
publisher Institute of Volcanology and Seismology FEB RAS
publishDate 2019
url https://doi.org/10.31431/1816-5524-2019-1-41-73-8
https://doaj.org/article/ab9c0d1fb77c49169a983fbfba4aa464
long_lat ENVELOPE(171.000,171.000,57.500,57.500)
geographic Bering Sea
Pacific
Shirshov Ridge
geographic_facet Bering Sea
Pacific
Shirshov Ridge
genre Bering Sea
Kamchatka
genre_facet Bering Sea
Kamchatka
op_source Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, Vol 41, Iss 1, Pp 73-84 (2019)
op_relation http://www.kscnet.ru/journal/kraesc/article/viewFile/236/pdf
https://doaj.org/toc/1816-5524
https://doaj.org/toc/1816-5532
doi:10.31431/1816-5524-2019-1-41-73-8
1816-5524
1816-5532
https://doaj.org/article/ab9c0d1fb77c49169a983fbfba4aa464
op_doi https://doi.org/10.31431/1816-5524-2019-1-41-73-8
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