THE KEMA ISLAND-ARC TERRANE, EASTERN SIKHOTE ALIN: FORMATION SETTINGS AND GEODYNAMICS

dc.contributor.author	Malinovsky A.I.
dc.contributor.author	Golozoubov V.V.
dc.contributor.author	Simanenko V.P.
dc.date.accessioned	2024-10-27T02:28:43Z
dc.date.available	2024-10-27T02:28:43Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13516252
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1026-1029
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46247
dc.description.abstract	The Kema Terrane is situated in eastern Sikhote Alin and extended along the coast of the Sea of Japan. The terrane is exposed in erosion windows among Late Cretaceous igneous rocks of the East Sikhote Alin volcanic belt. The terrane is composed of the Barremian (?)–Albian turbidites that contain siltstones, sandstones, gravelstones, conglomerates, mixtites, and tuff units, and basaltic volcanic flows. The Kema Terrane is thrust over the western Zhuravlevka Terrane, which is filled with the Lower Cretaceous turbidites and considered a continental-margin pull-apart basin.
dc.subject	Kema terrane
dc.subject	Sikhote Alin
dc.title	THE KEMA ISLAND-ARC TERRANE, EASTERN SIKHOTE ALIN: FORMATION SETTINGS AND GEODYNAMICS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070051
dc.subject.age	Мезозой::Меловая::Нижний::Барремский
dc.subject.age	Мезозой::Меловая::Нижний::Альбский

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