| 郭树银,郭宾锋.河南王庄锑矿区矿床地质特征及找矿标志[J].矿产勘查,2015,6(4):391-396 |
| 河南王庄锑矿区矿床地质特征及找矿标志 |
| Geological characteristics and prospecting criteria of Wangzhuang antimony mineral deposits of Lushi County, Henan Province |
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| DOI： |
| 中文关键词: 锑矿床 地质特征 矿床成因 矿床类型 王庄 河南 |
| 英文关键词: antimony deposit, geological characteristics, ore deposit deposit genesis, ore deposit type, Wangzhuang, Henan |
| 基金项目:河南省地质矿产厅地质勘查及科研项目(编号:豫地字(1991)第 507 号文)资助。 |
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| 中文摘要: |
| 河南省王庄锑矿床地处华北地台和扬子地台两大构造单元的过渡地带,北秦岭褶皱带东段,区域构造线呈NNW-SEE向。成矿区划属朱阳关—夏馆银铅锌铜锑成矿带之五里川锑V级成矿亚带,区内岩浆活动频繁,构造变动剧烈,为一重要的构造—岩浆活动带。通过对区域地质特征、矿床地质特征、成矿物质来源、化探异常特征等研究,认为该区锑矿床严格受断裂带控制,成矿温度中—低温,矿床类型为热液充填型矿床。 |
| 英文摘要: |
| The Wangzhuang antimony deposit located in the eastern part of North Qinling fold belt, occurs in the transition zone of the two tectonic units between North China platform and Yangtze platform. The regional structure strikes NNW-SEE-trendign. The metallogenic district is classified into Wulichuan grade V antimony sub-metallogenic belt within Zhuyangguan-Xiaguan Ag-Pb-Zn-Cu-Sb metallogenic belt, which is one key tectonic and magmatic activity belt. Based on the study of regional geological characteristics, ore deposit characteristics, metallogenic material sources and geochemical anomaly, it is concluded that the antimony deposit is strictly controlled by faults in this area, and the ore-forming temperature is low - intermediate temperature, the deposit type belongs to hydrothermal filling tyoe deposit. |
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