| 广西新路和水岩坝钨锡矿田的控矿构造 |
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| 引用本文： | 欧阳成甫,陈大克,钱建平.广西新路和水岩坝钨锡矿田的控矿构造[J].桂林工学院学报,1993(4). |
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| 作者姓名： | 欧阳成甫 陈大克 钱建平 |
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| 作者单位： | 桂林冶会地质学院地质矿产勘查系
(欧阳成甫，陈大克)，桂林冶会地质学院地质矿产勘查系(钱建平) |
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| 摘 要： | 姑婆山花岗岩体西南接触带的新路和水岩坝钨锡矿田的控矿构造主要是侵位构造,包括侵位断裂、侵位褶皱穹起、侵位界面和侵位面理等。白面山式锡矿床,并不是以“过渡层”为矿源层成矿,而是以“过渡层”这种构造薄弱层产生犁式滑脱断裂,矿液通过侵位断裂上升沿之充填交代成矿。
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| 关 键 词： | 钨矿床 锡矿床 矿田构造 控矿构造 广西/侵位构造 |
THE ORE-CONTROL STRUCTURE OF THE W-Sn ORE FIELD IN XINLU AND SHUIYANBA, GUANGXI |
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| Ouyang Chenpu Chen Dake Qian Jianping.THE ORE-CONTROL STRUCTURE OF THE W-Sn ORE FIELD IN XINLU AND SHUIYANBA, GUANGXI[J].Journal of Guilin University of Technology,1993(4). |
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| Authors: | Ouyang Chenpu Chen Dake Qian Jianping |
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| Abstract: | The ore-control structure of Xinlu and Shuiyanba W-Sn ore-field, loating within the south-western contact zone of Guposhan granite, is mainly an emplacement structure, including emplacement faults, emplacement upfolds, emplacement bounderies and emplacement foliations, etc. The Beimianshan-type Sn ore deposit is not formed directly by the 'transitional layer', providing ore-forming resources but formed by mineralization liquor going upwards, filling and replacing the replacement fault, plow-like detachment fault, created by such weak layer as 'transitional layer'. |
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| Keywords: | W ore deposit Sn ore deposit mine-field structure ore-controlling structure Guangxi/emplacement structure |
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