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Geodynamics of the Eravna Zone (Uda-Vitim Fold System of the Transbaikal Region): Geological and Geochronological Data

机译:Eravna区(跨贝加尔湖地区的Uda-Vitim褶皱系统)的地球动力学:地质和年代学数据

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摘要

The Uda-Vitim fold system (UVFS) comprises the inner areas of the western Transbaikal region extending from the lower reaches of the Selenga River to the Southern Muya Range. In the Vitim River upper reaches, it includes three lithotectonic zones: Eravna, Ikat-Bagdara, and Turka-Kurba (Fig. 1). In structural terms, all of them represent a system of tectonic blocks confined to the subsided upper part of the Angara-Vitim batholith that is largely composed of Late Paleozoic granitoids. A remarkable feature of the Uda-Vitim fold system is development of lithology-variable Middle and Upper Paleozoic rocks in its section.
机译:Uda-Vitim褶皱系统(UVFS)包括Transbaikal西部地区的内部区域,该区域从Selenga河的下游一直延伸到Muya山脉的南部。在维提姆河上游,它包括三个岩性构造带:Eravna,Ikat-Bagdara和Turka-Kurba(图1)。从结构上讲,所有这些都代表了一个构造块体系统,该结构块体被限制在安加拉-维蒂姆岩基的下陷上部,该基岩主要由晚古生代花岗岩组成。 Uda-Vitim褶皱系统的显着特征是其剖面中岩性可变的中上古生界岩石的发育。

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  • 来源
    《Doklady Earth Sciences》 |2010年第1期|p.1168-1171|共4页
  • 作者单位

    Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017 Russia;

    rnGeological Institute, Siberian Branch, Russian Academy of Sciences, ul. Sakh'yanovoi 6a, Ulan-Ude, 670042 Buryat Republic, Russia;

    rnGeological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017 Russia;

    rnGeological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017 Russia;

    rnKarpinskii All-Russia Research Institute of Geology (VSEGEI), Srednii pr. 74, St. Petersburg, 199106 Russia;

    rnInstitute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM), Russian Academy of Sciences, Staromonetnyi per. 35, Moscow, 119017 Russia;

    rnGeological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017 Russia;

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