AGE OF THE KURIL DEEP-SEA BASIN (SEA OF OKHOTSK)

dc.contributor.author	Bezverkhny V.L.
dc.contributor.author	Gorovaya M.T.
dc.contributor.author	Markevich V.S.
dc.contributor.author	Pletnev S.P.
dc.contributor.author	Nabiullin A.A.
dc.date.accessioned	2022-01-16T05:05:35Z
dc.date.available	2022-01-16T05:05:35Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13444839
dc.identifier.citation	Doklady Earth Sciences, 2003, 391, 6, 802-806
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34368
dc.description.abstract	Determination of the age of the Kuril deep-sea basin, one of the key structures of the Sea of Okhotsk region, is very important for solving the problem of its origin and structural evolution. In this connection, we studied the upthrusted part of the northern slope of the basin in the Terpeniya Swell area. Based on the geological-geophysical data on the seafloor and island, it is established that a horst related to a system of upthrusts and thrusts of the Terpeniya Peninsula and mainly composed of Upper Cretaceous-Danian volcanosedimentary and volcanic rocks is a main morphostructural element of the Terpeniya Swell.
dc.title	AGE OF THE KURIL DEEP-SEA BASIN (SEA OF OKHOTSK)
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.