CENOMANIAN VOLCANISM OF THE EASTERN SIKHOTE-ALIN VOLCANIC BELT: GEOCHEMICAL FEATURES

dc.contributor.author	Simanenko V.P.
dc.contributor.author	Khanchuk A.I.
dc.date.accessioned	2022-01-13T08:02:22Z
dc.date.available	2022-01-13T08:02:22Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13433135
dc.identifier.citation	Geochemistry International, 2003, 41, 8, 787-798
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34279
dc.description.abstract	A geochemical study of the Cenomanian andesitic and basaltic volcanic rocks in the lower part of the Eastern Sikhote-Alin volcanic belt was performed. Petrologic and geochemical features of the rocks correspond to products of calc-alkaline magmas of the subduction-related continental-margin belts. The Cenomanian volcanics differ in some geochemical features from the Aptian-Albian Sikhote-Alin island-arc rocks and the Albian-Cenomanian rocks characterizing the geodynamic regime of a Californian-type transform continental margin.
dc.subject	Cenomanian
dc.title	CENOMANIAN VOLCANISM OF THE EASTERN SIKHOTE-ALIN VOLCANIC BELT: GEOCHEMICAL FEATURES
dc.type	Статья
dc.subject.age	Mesozoic::Cretaceous::Upper::Cenomanian
dc.subject.age	Мезозой::Меловая::Верхний::Сеноманский	ru

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