UNDERWATER TERRACES AND RECENT SUBSIDENCE OF THE EASTERN KAMCHATKA SHELF

dc.contributor.author	Seliverstov N.I.
dc.date.accessioned	2020-12-01T08:37:40Z
dc.date.available	2020-12-01T08:37:40Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=20957236
dc.identifier.citation	Volcanology & Seismology, 1996, , 3, 277-297
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/20021
dc.description.abstract	Presents the results of the seismic stratigraphic analysis of the data obtained on continuous reflection profiles shot above the subsiding areas of the E Kamchatka shelf, which are made up of sediments that were deposited under the conditions of glacio-eustatic fluctuations. The sedimentary sequences identified indicate a succession of progressive sea level falls during the Pleistocene. Data are presented on the volumes of the Pleistocene deposits on the shelf and in the basins of the eastern Kamchatka gulfs.
dc.subject	Pleistocene	en
dc.title	UNDERWATER TERRACES AND RECENT SUBSIDENCE OF THE EASTERN KAMCHATKA SHELF
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary::Pleistocene	en
dc.subject.age	Кайнозой::Четвертичная::Плейстоцен	ru

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