BASALTS FROM THE FRANZ JOSEF LAND ARCHIPELAGO: NEW GEOCHEMICAL DATA

dc.contributor.author	Chernysheva E.A.
dc.contributor.author	Kharin G.S.
dc.contributor.author	Stolbov N.M.
dc.date.accessioned	2022-01-16T05:05:34Z
dc.date.available	2022-01-16T05:05:34Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13444726
dc.identifier.citation	Doklady Earth Sciences, 2003, 390, 4, 550-553
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34358
dc.description.abstract	Mesozoic intraplate continental basaltic volcanism at the Franz Josef Land (FJL) archipelago is related to the activity of the Iceland plume [1, 2]. The volcanic activity was less significant but genetically close to the Permian-Triassic plateau basalt magmatism in eastern Siberia. New data on the geology of the islands and on petrology and geochemistry of basalts were obtained during long-term systematic investigations of the FJL archipelago by the All-Russia Research Institute of Geology and Mineral Resources of the World Ocean [3, 4]. The results of these investigations provide insight into the tectonic evolution of the Arctic region.
dc.title	BASALTS FROM THE FRANZ JOSEF LAND ARCHIPELAGO: NEW GEOCHEMICAL DATA
dc.type	Статья
dc.subject.age	Mesozoic::Triassic
dc.subject.age	Paleozoic::Permian
dc.subject.age	Палеозой::Пермская	ru
dc.subject.age	Мезозой::Триасовая	ru

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