HORIZONTAL MOTIONS AND PLATE BOUNDARIES IN SAKHALIN AND HOKKAIDO

dc.contributor.author	Saprygin S.M.
dc.contributor.author	Kononov V.E.
dc.contributor.author	Senachin V.N.
dc.date.accessioned	2022-07-20T06:12:19Z
dc.date.available	2022-07-20T06:12:19Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13457128
dc.identifier.citation	Doklady Earth Sciences, 2004, 398, 7, 1043-1046
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38301
dc.description.abstract	The present communication is devoted to geological and instrumental data on horizontal motions in the deep zones of Sakhalin and Hokkaido. We have first established the existence of horizontal motions along two (north-northeastern and south-southeastern) directions in Sakhalin and substantiated the boundary between the Eurasian and Sea of Okhotsk plates. Taking into account the data of Japanese researchers on Hokkaido, one can assume that the Sea of Okhotsk Plate is undergoing anticlockwise rotation at a rate of up to 2 cm/yr.
dc.title	HORIZONTAL MOTIONS AND PLATE BOUNDARIES IN SAKHALIN AND HOKKAIDO
dc.type	Статья

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