EARLY STAGES OF THE PALEOASIAN OCEAN FORMATION: RESULTS OF GEOCHRONOLOGICAL, ISOTOPIC, AND GEOCHEMICAL INVESTIGATIONS OF LATE RIPHEAN AND VENDIAN-CAMBRIAN COMPLEXES IN THE CENTRAL ASIAN FOLDBELT

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dc.contributor.author Yarmolyuk V.V.
dc.contributor.author Kovalenko V.I.
dc.contributor.author Kovach V.P.
dc.contributor.author Rytsk E.Yu.
dc.contributor.author Kozakov I.K.
dc.contributor.author Kotov A.B.
dc.contributor.author Sal'nikova E.B.
dc.date.accessioned 2024-10-27T02:28:37Z
dc.date.available 2024-10-27T02:28:37Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13514681
dc.identifier.citation Doklady Earth Sciences, 2006, 411, 8, 1184-1189
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46221
dc.description.abstract The term “Paleoasian Ocean” designates a system of different-age structures formed within the oceanic lithosphere. They were accreted to the Siberian Craton to form the Central Asian Foldbelt (CAFB) in the course of the Caledonian, Hercynian, and Indosinian epochs of tectogenesis. The appearance of the CAFB is related to the breakup of the Rodinia supercontinent and, in particular, to the breakup of its Laurasian segment into the Siberian and Laurentian cratons.
dc.subject Cambrian
dc.subject Riphean
dc.subject Vendian
dc.title EARLY STAGES OF THE PALEOASIAN OCEAN FORMATION: RESULTS OF GEOCHRONOLOGICAL, ISOTOPIC, AND GEOCHEMICAL INVESTIGATIONS OF LATE RIPHEAN AND VENDIAN-CAMBRIAN COMPLEXES IN THE CENTRAL ASIAN FOLDBELT
dc.type Статья
dc.identifier.doi 10.1134/S1028334X06080046
dc.subject.age Paleozoic::Cambrian
dc.subject.age Палеозой::Кембрийская
dc.subject.age Precambrian::Proterozoic::Riphean
dc.subject.age Докембрий::Протерозой::Рифей
dc.subject.age Precambrian::Proterozoic::Neoproterozoic::Vendian
dc.subject.age Докембрий::Протерозой::Неопротерозойская::Вендский


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