| 青岗坪金矿床地质特征及成因探讨 |
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| 引用本文： | 刘国营,刘国庆. 青岗坪金矿床地质特征及成因探讨[J]. 桂林工学院学报, 2009, 29(3): 323-326 |
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| 作者姓名： | 刘国营 刘国庆 |
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| 作者单位： | 1. 中国地质大学,地球科学与资源学院,北京,100083;河南省有色金属地质矿产局,第五地质大队,郑州,450016
2. 河南省有色金属地质矿产局,第五地质大队,郑州,450016 |
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| 摘 要： | 青岗坪金矿位于华北地块南缘熊耳山变质核杂岩中部,其矿化类型为构造蚀变岩型。熊耳山变质核杂岩之拆离断层和次级断裂是该区的主要控矿构造,矿体主要赋存在层间破碎带中部的强硅化蚀变岩和蚀变糜棱岩中,金品位平均为7.04×10-6;成矿流体的1δ8OH2O为2.7‰-6.6‰,δDH2O为-63.1‰--96.3‰,成矿流体主要来源于岩浆水;石英包体测温结果为347.5-370℃,矿床成因类型属于中高温热液金矿床。
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| 关 键 词： | 金矿床 地质特征 成因 青岗坪 河南 |
Geologic Characters and Genesis of Qinggangping Gold Deposit |
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| LIU Guo-ying,LIU Guo-qing. Geologic Characters and Genesis of Qinggangping Gold Deposit[J]. Journal of Guilin University of Technology, 2009, 29(3): 323-326 |
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| Authors: | LIU Guo-ying LIU Guo-qing |
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| Affiliation: | LIU Guo-ying1,2,LIU Guo-qing2(1.Department of Geoscience and Resources,China University of Geoscience,Beijing 100083,China,2.No.5 Geological Team,Henan Geology Bureau of Nonferrous Metals and Mineral Resources,Zhengzhou 450016,China) |
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| Abstract: | Qinggangping gold deposit lies in the Xiongershan metamorphic core complex which is in the south of North China.The mineralization type is structural alterations.The Xiongershan detachment-metamorphic core complex is the main ore-controll structure.Most gold ore-bodies locate within the fractured zone of the fault and the mylonite zone.Au concentration grade is 7.04×10-6.δ18 OH2O value of ore fluid ranges from 2.7‰ to 6.6‰,δDH2O value from-63.1‰ to-96.3‰,indicating that the ore fluid is dominantly magmatic water,with the component of fluid inclusion.The temperature of fluid inclusions ranges from 347.5 to 370 ℃.The deposit genetic type is attributed to meso-epithermal of gold deposit. |
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| Keywords: | gold deposit geological character genesis Qinggangping Henan |
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