SUBDUCTION OF THE PACIFIC PLATE BETWEEN 1978 AND 1981

dc.contributor.author	Saprygin S.M.
dc.contributor.author	Vasilenko N.F.
dc.date.accessioned	2020-10-31T11:22:50Z
dc.date.available	2020-10-31T11:22:50Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31094674
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 6, 107-111
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18310
dc.description.abstract	Oceanic plate subduction under continental one took place as a result increase of lithospheric kinetic energy by value of order 1027 erg/year (because of the Earth rotation acceleration in 1978–1981) that caused response of region interiors in form of standing wave of horizontal compression of amplitude 10–5 and surface slope of the Honshu and Shikotan islands in the direction of deep-water trenches. The Pacific plate possessing the greatest inert mass involve in rapid regime of rotation for the last turn, before that’ll do offer resistance rotating lithosphere that conduce to its subduction.
dc.title	SUBDUCTION OF THE PACIFIC PLATE BETWEEN 1978 AND 1981
dc.type	Статья

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