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首页> 外文期刊>Doklady Earth Sciences >Petrogeochemical and Isotope Peculiarities of Supersubduction Terrigenous Deposits: The Example of Predivinsk Terrane of the Yenisei Ridge
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Petrogeochemical and Isotope Peculiarities of Supersubduction Terrigenous Deposits: The Example of Predivinsk Terrane of the Yenisei Ridge

机译:超俯冲陆源矿床的岩石地球化学和同位素特征:以叶尼塞山脊的普雷迪维斯克地层为例

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摘要

This study is aimed at revealing petrogeochemical and isotope specifics of terrigenous rocks occurring in close paragenetic association with island arc magmatic complexes from the example of Neoproterozoic complexes of the Predivinsk Terrane of the Yenisei Ridge. This terrane is located in the southwestern part of the ridge and composes the Sayany-Yenisei accretion-collisional belt. It consists of a number of tectonic plates overthrusted in the NE direction along the Priy-enisei (Predivinsk) thrust (Fig. 1) [1-4]. Two large tectonic blocks with different sets and compositions of rock associations (Western and Eastern) are distinguished within the terrane.
机译:这项研究的目的是从叶尼塞海岭普列迪夫斯克地貌的新元古代复合体实例中揭示与岛弧岩浆复合体密切共生的陆源岩石的岩石化学和同位素特征。该地层位于山脊的西南部,由Sayany-Yenisei增生-碰撞带组成。它由许多构造板块组成,这些构造板块沿普里-恩塞西(普雷维因斯克)推力(图1)在NE方向上被上推[1-4]。在地层中,可以区分出两个大型的构造块,它们具有不同的岩石组合和组成(西部和东部)。

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  • 来源
    《Doklady Earth Sciences》 |2013年第2期|1039-1041|共3页
  • 作者单位

    Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia;

    Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia;

    Geological Institute, Kola Science Center, Russian Academy of Sciences, Murmansk oblast, Apatity, Russia;

    Zavaritskii Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences, Yekaterinburg, Russia;

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