| 郴州市玛瑙山铁锰多金属矿床地质特征 |
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| 引用本文： | 曾昭健.郴州市玛瑙山铁锰多金属矿床地质特征[J].湖南地质,1997(3). |
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| 作者姓名： | 曾昭健 |
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| 作者单位： | 湖南省湘南地质勘察院 |
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| 基金项目： | 湖南地质矿产局地质勘查项目 |
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| 摘 要： | 玛瑙山铁锰多金属矿床产于棋梓桥组底部层位中，矿体呈似层状。除铁、锰、铅外，伴生有银、铟。由泥盆纪沉积期成岩成矿作用和燕山期岩浆热液叠加成矿作用所形成的沉积改造—岩浆热液叠加型铁锰多金属矿床。
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| 关 键 词： | 铁锰多金属矿床 特征 玛瑙山 |
Geological Feature of Manaoshan Fe Mn Polymetallic Ore Deposit in Chenzhou City |
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| Zeng ZhaojianGeological Exploration Institute of South Hunan.Geological Feature of Manaoshan Fe Mn Polymetallic Ore Deposit in Chenzhou City[J].Hunan Geology,1997(3). |
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| Authors: | Zeng ZhaojianGeological Exploration Institute of South Hunan |
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| Institution: | Zeng ZhaojianGeological Exploration Institute of South Hunan |
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| Abstract: | Manaoshan Fe Mn polymetallic ore deposit occurs in the bottom of Qiziqiao formation.The orebody looks beded.Iron,manganese and lead are the major minerals,accompanying silver and indium.Its forming experienced two stages,the first stage is diagenetic mineralization in Devonian and the second stage is magmatic hydrothermal superimposed miner alization in Yanshaian. |
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| Keywords: | Fe Mn polymetallic ore deposit feature Manaoshan |
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