| 闽中丁家山铅锌矿床同位素地球化学及其地质意义 |
| Received:September 24, 2011 Revised:June 25, 2013 点此下载全文 |
| 引用本文：SHI DeFeng,ZHANG ShuGen,HAN ShiLi,XU ZhongFa.2013.Isotope geochemistry of Dingjiashan Pb-Zn deposit in central Fujian Province and its geological significance[J].Mineral Deposits,32(5):1003~1010 |
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| Author Name | Affiliation | | SHI DeFeng | School of Civil Engineering, Hunan University of Science and Technology, Xiangtan 411201, Hunan, China | | ZHANG ShuGen | MOE Key Laboratory of Metallogenic Prediction of Nonferrous Metals, School of Geosciences and Info-Physics, Central South University, Changsha 410083, Hunan, China | | HAN ShiLi | MOE Key Laboratory of Metallogenic Prediction of Nonferrous Metals, School of Geosciences and Info-Physics, Central South University, Changsha 410083, Hunan, China | | XU ZhongFa | East China Geological Survey(Group) Co. Ltd., Nanjing 210007, Jiangsu, China |
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| 中文摘要:通过铅、硫、铷、锶同位素地球化学特征的系统分析,对闽中丁家山铅锌矿床的成矿物质来源、成矿时代及矿床成因进行了深入研究。围岩全岩及矿石内方铅矿的Pb同位素变化范围较宽,方铅矿的206Pb/204Pb比值在18.182~18.605之间, 207Pb/204Pb比值在15.010~15.932之间,208Pb/204Pb比值在38.331~39.666之间,具有明显的壳-幔混合来源特征,可能由龙北溪组地层和燕山期重熔型花岗岩共同提供。黄铁矿、磁黄铁矿、闪锌矿、方铅矿的δ34S组成为-1.7‰~5.6‰,平均值为2.7‰,具有向正值偏移的塔式分布特征;系统δ34S初始值为3.97‰,深源硫特征明显,说明硫由燕山期重熔型花岗岩提供。成矿期的石英铷-锶等时线年龄为(146.15±3.95) Ma,成矿时间属燕山早期第三阶段。以上结果进一步证实,丁家山铅锌矿床为马面山群龙北溪组上段经区域变质的富钙质沉积岩与燕山期重熔型花岗岩发生接触交代作用,形成的矽卡岩型矿床。 |
| 中文关键词:地球化学 成矿物质来源 成矿时代 矽卡岩型矿床 丁家山铅锌矿 |
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| Isotope geochemistry of Dingjiashan Pb-Zn deposit in central Fujian Province and its geological significance |
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| Abstract:Based on a systematic study of Pb, S, Rb and Sr isotope geochemistry, this paper deals with the sources of ore-forming materials,metallogenic epoch and genetic type of the Dingjiashan Pb-Zn ore district in Fujian Province. The 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb ratios are 18.182~18.605, 15.010~15.932, and 38.331~39.666 respectively. The wide ranges of Pb isotopes indicate that Pb was derived from the mantle and the crust. Neoproterozoic Mamianshan Formation of Longbeixi Group and Yanshanian remelted granite might have jointly served as the sources. The δ34S values of pyrite, pyrrhotite, sphalerite, galena are-1.7‰~5.6‰, 2.7‰ on average, characterized by tower-shaped distribution shifting to the positive value. The δ34S initial value of the metallogenic system is 3.97‰, obviously suggesting deep-sourced sulfur characteristics. These data imply that sulfur was supplied by Yanshanian remelted granite. Rb-Sr isochron of quartz reveals that the ore-forming process occurred at (146.15±3.95) Ma, in late Jurassic period, belonging to the third stage of early Yanshanian. It is thus held that the Dingjiashan Pb-Zn ore district is a skarn ore deposit resulting from the contact metasomatism between the Yanshanian remelted granite and the regional metamorphosed calcareous rock in Longbeixi Formation of Mamianshan Group. |
| keywords:geochemistry source of ore-forming materials metallogenic epoch skarn type ore deposit Dingjiashan Pb-Zn ore district |
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