Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом (Morphology of the Piip submarine volcano in the Komandorsky Basin based on multibeam echosounder data)
We analyzed the bathymetric data obtained during the cruises on the German research vessel “Sonne” using multibeam echosounders within the framework of the Russian-German projects KALMAR (cruise SO201-2, 2009) and BERING (cruise SO249-2, 2016) in the Komandorsky Basin of the Bering Sea. Detailed bat...
Published in: | Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences |
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Language: | Russian |
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Institute of Volcanology and Seismology FEB RAS
2021
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Online Access: | https://oceanrep.geomar.de/id/eprint/55802/ https://oceanrep.geomar.de/id/eprint/55802/1/663-820-1-PB.pdf https://doi.org/10.31431/1816-5524-2021-2-50-6-21 |
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ftoceanrep:oai:oceanrep.geomar.de:55802 2023-05-15T15:43:43+02:00 Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом (Morphology of the Piip submarine volcano in the Komandorsky Basin based on multibeam echosounder data) Baranov, B. V. Werner, Reinhard Rashidov, V. A. Tsukanov, N. V. Dozorova, K. A. 2021-06-30 text https://oceanrep.geomar.de/id/eprint/55802/ https://oceanrep.geomar.de/id/eprint/55802/1/663-820-1-PB.pdf https://doi.org/10.31431/1816-5524-2021-2-50-6-21 ru rus Institute of Volcanology and Seismology FEB RAS https://oceanrep.geomar.de/id/eprint/55802/1/663-820-1-PB.pdf Baranov, B. V., Werner, R., Rashidov, V. A., Tsukanov, N. V. and Dozorova, K. A. (2021) Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом (Morphology of the Piip submarine volcano in the Komandorsky Basin based on multibeam echosounder data). Open Access Bulletin of Kamchatka Regional Association Educational-Scientific Center: Earth Sciences, 50 (2). pp. 6-21. DOI 10.31431/1816-5524-2021-2-50-6-21 <https://doi.org/10.31431/1816-5524-2021-2-50-6-21>. doi:10.31431/1816-5524-2021-2-50-6-21 info:eu-repo/semantics/openAccess Article NonPeerReviewed 2021 ftoceanrep https://doi.org/10.31431/1816-5524-2021-2-50-6-21 2023-04-07T16:01:50Z We analyzed the bathymetric data obtained during the cruises on the German research vessel “Sonne” using multibeam echosounders within the framework of the Russian-German projects KALMAR (cruise SO201-2, 2009) and BERING (cruise SO249-2, 2016) in the Komandorsky Basin of the Bering Sea. Detailed bathymetric maps of the Piip submarine volcano were constructed. New morphological features of its summit edifices and their age relations are described, hydrothermal activity confined to the edifices is localized, and all side cones and lava flows are mapped. Based on the flank cones and fissure lava flows alignments we determined the tectonic paleostress that existed at the time of their formation, presumably after the Late Miocene-Early Pliocene. It differs from the recent tectonic stress caused by right-lateral displacements along the Bering fault zone. Article in Journal/Newspaper Bering Sea OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Bering Sea Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences 2(50) 6 21 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
Russian |
description |
We analyzed the bathymetric data obtained during the cruises on the German research vessel “Sonne” using multibeam echosounders within the framework of the Russian-German projects KALMAR (cruise SO201-2, 2009) and BERING (cruise SO249-2, 2016) in the Komandorsky Basin of the Bering Sea. Detailed bathymetric maps of the Piip submarine volcano were constructed. New morphological features of its summit edifices and their age relations are described, hydrothermal activity confined to the edifices is localized, and all side cones and lava flows are mapped. Based on the flank cones and fissure lava flows alignments we determined the tectonic paleostress that existed at the time of their formation, presumably after the Late Miocene-Early Pliocene. It differs from the recent tectonic stress caused by right-lateral displacements along the Bering fault zone. |
format |
Article in Journal/Newspaper |
author |
Baranov, B. V. Werner, Reinhard Rashidov, V. A. Tsukanov, N. V. Dozorova, K. A. |
spellingShingle |
Baranov, B. V. Werner, Reinhard Rashidov, V. A. Tsukanov, N. V. Dozorova, K. A. Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом (Morphology of the Piip submarine volcano in the Komandorsky Basin based on multibeam echosounder data) |
author_facet |
Baranov, B. V. Werner, Reinhard Rashidov, V. A. Tsukanov, N. V. Dozorova, K. A. |
author_sort |
Baranov, B. V. |
title |
Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом (Morphology of the Piip submarine volcano in the Komandorsky Basin based on multibeam echosounder data) |
title_short |
Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом (Morphology of the Piip submarine volcano in the Komandorsky Basin based on multibeam echosounder data) |
title_full |
Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом (Morphology of the Piip submarine volcano in the Komandorsky Basin based on multibeam echosounder data) |
title_fullStr |
Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом (Morphology of the Piip submarine volcano in the Komandorsky Basin based on multibeam echosounder data) |
title_full_unstemmed |
Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом (Morphology of the Piip submarine volcano in the Komandorsky Basin based on multibeam echosounder data) |
title_sort |
морфология подводного вулкана пийпа в командорской котловине по данным съемки многолучевым эхолотом (morphology of the piip submarine volcano in the komandorsky basin based on multibeam echosounder data) |
publisher |
Institute of Volcanology and Seismology FEB RAS |
publishDate |
2021 |
url |
https://oceanrep.geomar.de/id/eprint/55802/ https://oceanrep.geomar.de/id/eprint/55802/1/663-820-1-PB.pdf https://doi.org/10.31431/1816-5524-2021-2-50-6-21 |
geographic |
Bering Sea |
geographic_facet |
Bering Sea |
genre |
Bering Sea |
genre_facet |
Bering Sea |
op_relation |
https://oceanrep.geomar.de/id/eprint/55802/1/663-820-1-PB.pdf Baranov, B. V., Werner, R., Rashidov, V. A., Tsukanov, N. V. and Dozorova, K. A. (2021) Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом (Morphology of the Piip submarine volcano in the Komandorsky Basin based on multibeam echosounder data). Open Access Bulletin of Kamchatka Regional Association Educational-Scientific Center: Earth Sciences, 50 (2). pp. 6-21. DOI 10.31431/1816-5524-2021-2-50-6-21 <https://doi.org/10.31431/1816-5524-2021-2-50-6-21>. doi:10.31431/1816-5524-2021-2-50-6-21 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.31431/1816-5524-2021-2-50-6-21 |
container_title |
Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences |
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2(50) |
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6 |
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21 |
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1766377920453935104 |