MARINE PALEOGENE SEDIMENTS FROM THE NORTHERN SLOPE OF THE KURIL DEEP-SEA BASIN, SEA OF OKHOTSK

dc.contributor.author	Bezverkhnii V.L.
dc.contributor.author	Gorovaya M.T.
dc.contributor.author	Nabiullin A.A.
dc.contributor.author	Markevich V.S.
dc.date.accessioned	2021-11-23T00:58:45Z
dc.date.available	2021-11-23T00:58:45Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13439255
dc.identifier.citation	Stratigraphy and Geological Correlation, 2003, 11, 6, 594-605
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/32395
dc.description.abstract	Micropaleontology and lithology of rocks dredged near the Terpeniya Rise of the Kuril Basin slope are studied. Bio-, litho-, and seismostratigraphic records are used to distinguish the Paleocene-Lower Oligocene (Seismocomplex E), Upper Oligocene (Seismocomplex D), and Upper Oligocene-Middle Miocene (Seismocomplex C) sequences of the Lower Cenozoic sedimentary cover. The sequences are correlated with concurrent deposits of the region, and their paleotectonic settings are reconstructed. It is concluded that in the southern transitional zone of the Sea of Okhotsk there was a full succession of the Paleocene morphological structures, i.e., the shelf, slope, and deep-sea basin, which were separated from the ocean by the paleo-Kuril system of islands or submarine rises.
dc.subject	Paleogene
dc.title	MARINE PALEOGENE SEDIMENTS FROM THE NORTHERN SLOPE OF THE KURIL DEEP-SEA BASIN, SEA OF OKHOTSK
dc.type	Статья
dc.subject.age	Cenozoic::Paleogene
dc.subject.age	Кайнозой::Палеоген	ru

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