kudi
- 网络库迪
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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
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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
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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
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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;
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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。
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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。