Geochronology and geochemistry of acid metavolcanites, Losevo Series, Voronezh crystalline massif

The Losevo structural formation zone is a part of the East Sarmatian orogen in the junction of the Sarmatian and Volgo Uralian segments of the East European Craton. To solve the problem regarding the age and geody namical position of the lower (Strelitsa) stratum of the Losevo Series, which includes...

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Veröffentlicht in:Doklady earth sciences 2014-02, Vol.454 (2), p.136-139
Hauptverfasser: Terentiev, R. A., Savko, K. A., Samsonov, A. V., Larionov, A. N.
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Sprache:eng
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Zusammenfassung:The Losevo structural formation zone is a part of the East Sarmatian orogen in the junction of the Sarmatian and Volgo Uralian segments of the East European Craton. To solve the problem regarding the age and geody namical position of the lower (Strelitsa) stratum of the Losevo Series, which includes the contrast volcanism products, mineralogicalpetrographic, petrochemical, geochemical, and isotopic studies of the metamorphized acid rocks from the reference section have been carried out.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X14020172