GEODYNAMICS OF THE CHERSKY SEISMIC BELT

dc.contributor.author	Parfenov L.M.
dc.contributor.author	Koz'min B.M.
dc.contributor.author	Grinenko O.V.
dc.contributor.author	Imaev V.S.
dc.contributor.author	Imaeva L.P.
dc.date.accessioned	2020-04-13T10:49:35Z
dc.date.available	2020-04-13T10:49:35Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30961564
dc.identifier.citation	JOURNAL OF GEODYNAMICS, 1988, 9, 1, 15-37
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16634
dc.description.abstract	The geodynamics of the Chersky seismic belt is discussed, based on seismic and geologic evidence, as well as on heat-flow and deep-structure analyses. The belt stretches across Northeast Asia from the Laptev Sea to the Komandorskie Islands. It forms a boundary between the Eurasian, North American and Sea of Okhotsk plates. The concept of the relationship between the belts seismicity and the Moma rift system is not supported. The belt is currently undergoing compression generated by the sublatitudinal convergence of the North American and Eurasian plates.
dc.title	GEODYNAMICS OF THE CHERSKY SEISMIC BELT
dc.type	Статья

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