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| 豫西南周庄铅锌银矿床地质和成矿流体地球化学 | |
| 引用本文： | 曹纪虎,向世红,薛春纪,张旭,李永峰,李丙奇,程文厚.豫西南周庄铅锌银矿床地质和成矿流体地球化学[J].地学前缘,2011,18(5):159-171. |
| 作者姓名： | 曹纪虎 向世红 薛春纪 张旭 李永峰 李丙奇 程文厚 |
| 作者单位： | 1. 地质过程与矿产资源国家重点实验室；中国地质大学（北京）地球科学与资源学院,北京100083 2. 地质过程与矿产资源国家重点实验室；中国地质大学（北京）地球科学与资源学院,北京100083／河南省有色金属地质矿产局,河南郑州450016 3. 河南省有色金属地质矿产局,河南郑州,450016 |
| 基金项目： | 国家自然科学基金项目(41072069,40772061); 地质过程与矿产资源国家重点实验室科学基金项目(GPMR0936); 河南省有色金属地质矿产局科技创新项目(YSDK2010-6); 河南省科技发展计划项目(2010-021) |
| 摘 要： | 豫西南周庄铅锌银矿床是最近在豫西南铅锌银矿集区新发现的一处矿产地。矿床形成于印支期造山后板内构造-岩浆地质环境,工业矿体主要是东秦岭二郎坪群中充填于垂直造山带走向的断裂构造中的石英-铅锌银硫化物矿脉,热液成矿作用经历了石英-黄铁矿、石英-铅锌银硫化物、石英-方解石等早、中、晚3个不同阶段。矿石中以石英为主的脉石矿物捕获... |
| 关 键 词： | 矿床地质 流体包裹体 H、O同位素 脉状铅锌银矿 周庄 豫西南 |
Ore geology and ore-forming fluid geochemistry of Zhouzhuang Ag-Pb-Zn deposit,southwestern Henan Province |
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| Cao Jihu,Xiang Shihong,Xue Chunji,Zhang Xu,Li Yongfeng,Li Bingqi,Cheng Wenhou .State Key Laboratory of Geological Processes , Mineral Resources,School of Earth Sciences , Resources,China University of Geosciences,Beijing ,China .Bureau of Non-ferrous Metals Geological , Mineral Resources,Zhengzhou ,China.Ore geology and ore-forming fluid geochemistry of Zhouzhuang Ag-Pb-Zn deposit,southwestern Henan Province[J].Earth Science Frontiers,2011,18(5):159-171. | |
| Authors: | Cao Jihu Xiang Shihong Xue Chunji Zhang Xu Li Yongfeng Li Bingqi Cheng Wenhou State Key Laboratory of Geological Processes Mineral Resources School of Earth Sciences Resources China University of Geosciences Beijing China Bureau of Non-ferrous Metals Geological Mineral Resources Zhengzhou China |
| Institution: | Cao Jihu1,Xiang Shihong1,2,Xue Chunji1,Zhang Xu2,Li Yongfeng2,Li Bingqi2,Cheng Wenhou2 1.State Key Laboratory of Geological Processes and Mineral Resources,School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083,China 2.Bureau of Non-ferrous Metals Geological and Mineral Resources,Zhengzhou 450016,China |
| Abstract: | The Zhouzhuang Ag-Pb-Zn ore deposit was recently discovered in the southwestern Henan Province where there are some other Ag-Pb-Zn ore deposits.It occurred in an inter-plate tectonic-magmatic geological environment after Indosinian orogeny.The ore-body is mainly in the Erlangping Group and the veins of quartz-(Ag-Pb-Zn) sulfides filled in the fault fractures whose strike-directions are perpendicular to the orogenic belt.The Ag-Pb-Zn hydrothermal mineralization shows three stages: the early stage is characte... |
| Keywords: | ore geology fluid inclusions O-and H-isotopes Ag-Pb-Zn ore veins Zhouzhuang Ag-Pb-Zn ore deposit southwestern Henan Province |
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