Fragments of the Vendian convergent borderland in the South Urals

The fragments of the Vendian convergent borderland in the South Urals are of undoubted significance for solving the problem of inherited development of the Uralian domain from the Proto-Uralides, i.e., from the pre Ordovician epoch into the Uralides [1, 2], as well for clarifying the character and l...

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Bibliographic Details
Published inDoklady earth sciences Vol. 432; no. 2; pp. 726 - 731
Main Authors Samygin, S. G., Belova, A. A., Ryazantsev, A. V., Fedotova, A. A.
Format Journal Article
LanguageEnglish
Published Dordrecht SP MAIK Nauka/Interperiodica 01.06.2010
Springer
Springer Nature B.V
Subjects
Cambrian
Earth and Environmental Science
Earth Sciences
Geology
Igneous rocks
Mountains
Ordovician
Petrology
Sediments
Ural Mountains
Ordovician
Accretionary Prism
DOKLADY Earth Science
Zone Zircon
Calc Alkaline
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Summary:The fragments of the Vendian convergent borderland in the South Urals are of undoubted significance for solving the problem of inherited development of the Uralian domain from the Proto-Uralides, i.e., from the pre Ordovician epoch into the Uralides [1, 2], as well for clarifying the character and location of its boundary with the East European paleocontinent (Baltika) during the Late Cambrian.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X10060036