| 曾宪科,刘旭,吕宇明,覃金宁,张宋芳,王慧媛，朱武泉,朱成生.常宁市灯坪地区铜铅锌成矿作用及其特征[J].南华大学学报(自然科学版),2012,26(3):47~53.[ZENG Xian-ke,LIU Xu,LV Yu-ming,QIN Jin-ning,ZHANG Song-fang,WANG Hui-yuan,ZHU Wu-quan,ZHU Cheng-sheng.Copper Lead Zinc Mineralization and Characteristics of Deng Ping Area ，Changning City[J].Journal of University of South China(Science and Technology),2012,26(3):47~53.] |
| 常宁市灯坪地区铜铅锌成矿作用及其特征 |
| Copper Lead Zinc Mineralization and Characteristics of Deng Ping Area ，Changning City |
| 投稿时间：2012-09-19 |
| DOI： |
| 中文关键词: 铜铅锌矿床 矿化特征 成矿作用 成矿机制 |
| 英文关键词:copper-lead-zinc deposits mineralization characteristics mineralization metallogenic mechanism |
| 基金项目: |
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| 中文摘要: |
| 灯坪地区铜铅锌矿化特征表明：其成矿地质作用具有“热液充填交代”、“氧化淋积—次生富集”、“动力变质分异”的明显特征，且热液充填交代成矿作用是本区最为主要的成矿作用.矿物及包裹体特征、碳氧同位素组成及矿脉与地层岩体微量、稀土元素对比值的相关分析表明，热液充填交代成矿作用中成矿物质主要来源于地层，热液水主要来源于大气降水，部分来源于地层和岩浆残余水. |
| 英文摘要: |
| The copper-lead-zinc mineralization characteristics of DengPing area indicated the metallogenic geological process have obvious features about hydrothermal filling and replacement,oxidation leaching area-secondary enrichment,and dynamic metamorphism differentiation.Heatliquid filling and replacement mineralization is the main mineralization in this area.The correlation analysis ratio of Mineral inclusions characteristics,carbon and oxygen isotopes and veins with the formation rock trace rare earth elements manifest that metallogenic material of hydrothermal filling and replacement mineralization are mainly from the stratum.Hydrothermal water mainly comes from the atmosphere precipitation,partly from the stratigraphy and magma residual water. |
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