| 新资断裂带的构造地球化学特征 |
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| 引用本文： | 康自立,吴伟成.新资断裂带的构造地球化学特征[J].铀矿地质,1991,7(3):137-145. |
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| 作者姓名： | 康自立 吴伟成 |
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| 摘 要： |
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| 关 键 词： | 断裂带 构造地球化学 铀矿床 |
THE TECTONO-GEOCHEMICAL CHARACTERISTICS OF XINZI FRACTURE ZONE |
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| Kang Zili,Wu Weicheng,Zhu Minqiang.THE TECTONO-GEOCHEMICAL CHARACTERISTICS OF XINZI FRACTURE ZONE[J].Uranium Geology,1991,7(3):137-145. |
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| Authors: | Kang Zili Wu Weicheng Zhu Minqiang |
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| Institution: | Kang Zili;Wu Weicheng;Zhu Minqiang |
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| Abstract: | Xinzi fracture zone is a trunk fracture zone for metallogenesis in a certain uranium ore field. Based on dissection of structural deformation regularity and research on tec- tono-geochemical action of fault caused by the tectonic deformation, this paper preliminarily reveals the relation between the faulting and the variation of chemical compositions of rocks in the fault zone, and the mineralization process of minerogenetic elements such as uranium to be mobilized, migrated and conecntrated under the effect of structural dy- namics. |
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| Keywords: | Xinzi fracture zone Tectono-geochemistry Uranium deposit |
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