| 永梅会与中下扬子地区的成矿条件对比 |
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| 引用本文： | 贺菊瑞.永梅会与中下扬子地区的成矿条件对比[J].资源调查与环境,1998(4). |
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| 作者姓名： | 贺菊瑞 |
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| 作者单位： | 南京地质矿产研究所!南京，210016 |
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| 摘 要： | 永海会地区的区域构造、含矿地层和建造、中生代火山侵入岩体特征、局部控矿构造以及成矿物质来源、硫氢氧同位素、铅同位素、年龄同位素等成矿信息，都与扬子区、萍乐区已知铜金矿集区有许多相似之处。通过对比表明，永海会地区具有极大的找矿前应景。
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| 关 键 词： | 成矿条件对比 晚古生代坳陷区 永海会地区 扬子区 萍乐区 |
THE COMPARISON OF THE ORE-FORMING CONDITION IN YONGDING-MEIXIAN-HUICHANG AND MIDDLE-LOWER YANGTZE AREA |
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| He Jurui.THE COMPARISON OF THE ORE-FORMING CONDITION IN YONGDING-MEIXIAN-HUICHANG AND MIDDLE-LOWER YANGTZE AREA[J].Resources Survey & Environment,1998(4). |
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| Authors: | He Jurui |
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| Abstract: | Yongding-Meixian-Huichang metallogenic area(Yongmeihui for short) is similar to the CuAu deposit concentrated area of Middle-Lower Yangtze and Ping-Le in the characteristics of regional structure, ore-bearing strata and formations, the Mesozoic volcano-instrusive rocks, localore-control structure, the source of the ore-forming, S-O-H-isotope, Ph-isotope, the ore-formingages and etc. Therefore, it is suggested that there is a great potential for the ore-search inYongmeihui metallogenic area. |
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| Keywords: | the comparision of the ore-forming condition late Paleozoic depression zone Yongmeihui Yangtze area Ping-Le area |
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