CENOZOIC CONTINENTAL-MARGIN VOLCANISM IN THE PACIFIC AND BERING SEA SECTORS OF KAMCHATKA: GEODYNAMIC IMPLICATIONS

dc.contributor.author	Bogdanov N.A.
dc.contributor.author	Chekhovich V.D.
dc.date.accessioned	2022-05-02T07:48:57Z
dc.date.available	2022-05-02T07:48:57Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=14998212
dc.identifier.citation	Geologiya i Geofizika, 2004, 45, 4, 421-429
dc.identifier.issn	0016-7886
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/37333
dc.description.abstract	The tectonic position and ages of suprasubduction continental-margin volcanoplutonic belts controlled by their Cenozoic geodynamic environments are notably different in the Pacific and Bering Sea sectors of Kamchatka and southern Koryakia. In pre-Cenozoic time the two sectors were separated by a long-existing transform fault whose western segment now coincides with the Komandor strike-slip fault and the eastern segment is clearly traceable by satellite gravity data on the Pacific floor southeastwards on the continuation of the Komandor fault.
dc.subject	Continental-margin volcanic belts
dc.subject	subduction
dc.subject	collision
dc.subject	transform faults
dc.subject	Kamchatka
dc.subject	Cenozoic
dc.title	CENOZOIC CONTINENTAL-MARGIN VOLCANISM IN THE PACIFIC AND BERING SEA SECTORS OF KAMCHATKA: GEODYNAMIC IMPLICATIONS
dc.type	Статья
dc.subject.age	Cenozoic
dc.subject.age	Кайнозой	ru

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