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首页> 外文期刊>Doklady Earth Sciences >Th-U-Pb Age of Metamophism of the Vorontsovka Group Rocks, Voronezh Crystalline Massif, from Microbrobe Dating of Monazites
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Th-U-Pb Age of Metamophism of the Vorontsovka Group Rocks, Voronezh Crystalline Massif, from Microbrobe Dating of Monazites

机译:沃罗涅佐夫卡族岩石沃洛涅日结晶断层的变质作用的Th-U-Pb年龄,来自独居石的微贿赂约会

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摘要

The Paleoproterozoic metaterrigenous rocks of the Vorontsovka Group were studied. This series occupies a large area between the Precambrian crustal segments of the East European Craton, Sarmatia, and Volgo-Uralia. Based on the data of Th-U-Pb microprobe dating of monazites from the Vorontsovka Group, the age of zonal metamorphism is 2039 + 26 Ma for the staurolite zone, 2015 ± 14 Ma for the muscovite- sillimanite zone, and 2008 ± 20 for the sillimanite-K-spar-cordierite zone. These data imply subsynchro-nity of the regional metamorphism and penetration of collision S-type granites of the Bobrov Complex about 2020 Ma B.P.
机译:研究了沃龙佐夫卡群的古元古代变质岩。该系列在东欧克拉通,萨尔玛蒂亚和伏尔加河-乌拉利亚的前寒武纪地壳段之间占据很大的面积。根据沃龙佐夫卡族独居石的Th-U-Pb微探针测年数据,纬线变质年龄为星形变石带2039 + 26 Ma,白云母-硅线石带为2015±14 Ma,2008年为±20 Ma硅线石-钾-堇青石带。这些数据暗示了2020 Ma B.P.附近的Bobrov复合体的碰撞S型花岗岩的区域变质作用和渗透性。

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  • 来源
    《Doklady Earth Sciences》 |2012年第1期|p.568-573|共6页
  • 作者单位

    Voronezh State University, Voronezh, Russia;

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

    Voronezh State University, Voronezh, Russia;

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

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