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小秦岭脉型金矿床容矿断裂及石英脉形成机制的探讨
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
作者姓名:邵世才  何绍勋  奚小双
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
基金项目:国家自然科学基金(编号49172134)
摘    要:

关 键 词:金矿床 容矿断裂 石英脉 形成机制
收稿时间:1992-07-09

ERSEARCH ON MECHNANISM OF FORMATION OF THE ORE-HOSTED FRACTURES AND GOLD-BEARING QUARTZ VEINS AT XIAOQINLING AREA
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
Authors:Shao Shicai  He Shaoxun  Xi Xiashuang
Affiliation:Department of Geology, Central-south University of Technology;Department of Geology, Central-south University of Technology;Department of Geology, Central-south University of Technology
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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