kudi

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kudikudi
  1. Geological characteristics of North Kudi structure belt , Western Kunlun and their geotectonic implications

    西昆仑库地北构造带两侧地质特征对比及其大地构造意义

  2. The geological characteristics and geotectonic setting of Kudi ophiolite in Western Kunlun Mountains

    西昆仑库地蛇绿岩的地质特征及其形成环境

  3. Geochemistry and tectonic significance of the diabases in Kudi , Western Kunlun

    西昆仑库地基性脉岩地球化学及构造意义

  4. Kudi ophiolite derived from light loss , non single upper mantle magma sources which were hybridized by continental crust composition .

    岩浆来源为弱亏损的、非单一的上地幔源,并受到了陆壳物质的混染;

  5. THE CHARACTERISTICS OF KUDI OPHIOLITE SUITE AND ITS TECTONIC SETTING and the Pb , V and Cr anomalies in the southern part of the province are the resultant fields of the early Palaeozoic rock formations and ophiolite suite .

    西昆仑山库地蛇绿岩的特征及其构造意义南部Pb、V、Cr异常反映早古生代地层与蛇绿岩套的混合地化场。

  6. Combining the characteristics of Kudi island arc granitoid , the authors also suggest that there had been a wide ocean lying to the south of Tarim basin during Sinian and Early Paleozoic , and this wide ocean was closed at the end of Silurian .

    结合库地岛弧花岗岩的特征,提出塔里木盆地南缘在震旦纪&早古生代时期存在一个广阔的大洋,这一大洋在志留纪末期关闭。