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

dc.contributor.authorSimanenko V.P.
dc.contributor.authorKhanchuk A.I.
dc.date.accessioned2022-01-13T08:02:22Z
dc.date.available2022-01-13T08:02:22Z
dc.date.issued2003
dc.description.abstractA 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.identifierhttps://www.elibrary.ru/item.asp?id=13433135
dc.identifier.citationGeochemistry International, 2003, 41, 8, 787-798
dc.identifier.issn0016-7029
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/34279
dc.subjectCenomanian
dc.subject.ageMesozoic::Cretaceous::Upper::Cenomanian
dc.subject.ageМезозой::Меловая::Верхний::Сеноманскийru
dc.titleCENOMANIAN VOLCANISM OF THE EASTERN SIKHOTE-ALIN VOLCANIC BELT: GEOCHEMICAL FEATURES
dc.typeСтатья

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