| 小秦岭脉型金矿床容矿断裂及石英脉形成机制的探讨 |
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| 引用本文： | 邵世才,何绍勋,奚小双.小秦岭脉型金矿床容矿断裂及石英脉形成机制的探讨[J].地质找矿论丛,1993,8(2):26-33. |
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| 作者姓名： | 邵世才 何绍勋 奚小双 |
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| 作者单位： | 中南工业大学地质系，中南工业大学地质系，中南工业大学地质系 长沙，410083，长沙，410083，长沙，410083 |
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| 基金项目： | 国家自然科学基金(编号49172134) |
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| 摘 要： |
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| 关 键 词： | 金矿床 容矿断裂 石英脉 形成机制 |
| 收稿时间： | 1992/7/9 0:00:00 |
ERSEARCH ON MECHNANISM OF FORMATION OF THE ORE-HOSTED FRACTURES AND GOLD-BEARING QUARTZ VEINS AT XIAOQINLING AREA |
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| Shao Shicai,He Shaoxun and Xi Xiashuang.ERSEARCH ON MECHNANISM OF FORMATION OF THE ORE-HOSTED FRACTURES AND GOLD-BEARING QUARTZ VEINS AT XIAOQINLING AREA[J].Contributions to Geology and Mineral Resources Research,1993,8(2):26-33. |
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| Authors: | Shao Shicai He Shaoxun and Xi Xiashuang |
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| Institution: | Department of Geology, Central-south University of Technology;Department of Geology, Central-south University of Technology;Department of Geology, Central-south University of Technology |
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| Abstract: | A complete set of fault rocks from mylonite to cataclasite are present in the ore-hosted fractures at Xiaoqinling Au-ore area where microstructural phenomena are very common. The fractures are sinistral thrust-type ductile-brittle shear zones and formed by the hydrofracturing by the high fluid pressure. The cyclic crack of the fractures and cyclic sealing caused by the ore-forming fluids produced the multistage gold-bearing quartz veins. |
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