EVOLUTION OF THE KOMANDORSKAYA BASIN

dc.contributor.author	Shipilov E.V.
dc.contributor.author	Yunov A.Yu.
dc.date.accessioned	2020-10-09T08:55:42Z
dc.date.available	2020-10-09T08:55:42Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31128646
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 3, 39-42
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17854
dc.description.abstract	The wedgelike shape of the Komandorskaya Basin in plan view, the distribution of thicknesses of the sedimentary mantle and its structure, the characteristic topography of the basement in the region, the crustal structure at depth and the anomalously high heat-flow values suggest that destructive processes dominated in the evolution of the crust in this area of the sea. The cyclical development of this zone of the sea fits the major transgressive and regressive Cenozoic cycles identified by Vail in the ocean. It is obvious in this case that Vail's eustatic cycles are closely connected with tectonic activation phases.
dc.subject	Cenozoic	en
dc.title	EVOLUTION OF THE KOMANDORSKAYA BASIN
dc.type	Статья
dc.subject.age	Cenozoic	en
dc.subject.age	Кайнозой	ru

Files in this item

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