| 河台金矿断层岩的地质地球化学特征及其与金矿化的关系 |
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| 引用本文： | 邱德同.河台金矿断层岩的地质地球化学特征及其与金矿化的关系[J].地质找矿论丛,1989(4):12-21. |
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| 作者姓名： | 邱德同 |
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| 作者单位： | 南京大学地球科学系 |
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| 摘 要： | 摘要本文论述了河台金矿区断层岩的类型及其地质和地球化学特征,探讨了糜棱岩带与金矿化的关系,指出剪切应变强度和石英动态重结晶发育程度与金矿化强度密切相关.
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| 关 键 词： | 断层岩 碎裂岩 糜棱岩 动态重结晶构造 |
GEOLOGICAL AND GEOCHEMICAL FEATURES OF THE FAULT ROCRS AND THEIR RELATIONSHIP WITH GOLD MINERALIZATITON IN HETAI GOLD DEPOSIT |
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| Qiu Detong.GEOLOGICAL AND GEOCHEMICAL FEATURES OF THE FAULT ROCRS AND THEIR RELATIONSHIP WITH GOLD MINERALIZATITON IN HETAI GOLD DEPOSIT[J].Contributions to Geology and Mineral Resources Research,1989(4):12-21. |
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| Authors: | Qiu Detong |
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| Institution: | Geoscience department of Nanjing university |
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| Abstract: | The author deals with the types of fault rocks and their geological and geochemical feature in Hetai gold district; the relationship between mylonite belt and gold mineralization. The author also indicates the shear strain strength and dynamical recrystallization degree of quartz are closely to related gold mineralization intensity |
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