| 云南兰坪李子坪铅锌矿床的控矿构造、碳和氧同位素及稀土元素地球化学特征 |
| Received:April 16, 2014 Revised:June 29, 2015 点此下载全文 |
| 引用本文：HU MaoDe,ZHANG HongRui,JIA JinWu,LIU YuYuan.2015.Structural control, oxygen and carbon isotope, and REE geochemistry of Liziping Pb-Zn ore deposit, Lanping Basin, Yunnan Province[J].Mineral Deposits,34(5):1057~1071 |
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| Author Name | Affiliation | E-mail | | HU MaoDe | Institute of Geology, CAGS, Beijing 100037, China
China National Geological & Mining Corporation, Beijing 100029, China | | | ZHANG HongRui | Institute of Geology, CAGS, Beijing 100037, China | hongrui_1982@126.com | | JIA JinWu | Institute of Geology, CAGS, Beijing 100037, China
China National Geological & Mining Corporation, Beijing 100029, China | | | LIU YuYuan | China University of Geosciences, Beijing 100083, China | |
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| 基金项目:本文得到国家自然科学基金项目(编号:41472067,41403043,41320104004,41273050和41302067)、中国地质调查局项目(编号:1212011220908)和国际地学对比计划IGCP/SIDA-600项目联合资助 |
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| 中文摘要:李子坪铅锌矿床位于青藏高原东缘的兰坪盆地内,属于白秧坪矿集区的一部分,矿体主要受构造裂隙控制,构造对该矿床具有重要的控制作用。文章对该矿床进行了构造解析,并结合地球化学数据,讨论了该矿床的形成过程。研究表明,李子坪铅锌矿床主要发育3期构造变形:早期为近南北走向的褶皱构造,中期为西倾近似等间距的数条逆断层,晚期形成北西西向与北东东向的平移断层。矿体主要受晚期2组平移断层的控制。各类方解石的δ13CPDB值变化范围为-1.3‰～ -2.3‰,平均值-1.7‰;δ18OSMOW值范围为6.9‰～21.0‰,平均值14.8‰。所测各类方解石的∑REE均小于30×10-6,∑HREE无明显变化,而∑LREE具有较明显差异,δEu均小于1,显示中等铕的负异常,表明成矿流体存在一定的演化规律。热液矿物方解石中的碳来源于海相碳酸盐岩的溶解作用,氧同位素结果表明成矿流体有大气降水渗入。综合分析认为,李子坪矿床应该为碰撞造山作用下形成的、矿体赋存于构造裂隙破碎带中的铅锌矿床。 |
| 中文关键词:地质学 控矿构造 碳、氧稳定同位素 稀土元素 李子坪铅锌矿床 |
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| Structural control, oxygen and carbon isotope, and REE geochemistry of Liziping Pb-Zn ore deposit, Lanping Basin, Yunnan Province |
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| Abstract:Located in the Lanping basin of the eastern Himalayan Syntaxis, the Liziping Pb-Zn ore deposit belongs to the Baiyangping silver-copper polymetallic ore concentration area. Orebody is mainly controlled by structure fracture zones. Structure played an important controlling role in Liziping lead-zinc mineralization. The structural analysis of the ore deposit and the geochemical ore-forming fluid study contribute to understanding the formation process of the ore deposit. In this paper, based on catalog of the ore adit, the authors analyzed ore-controlling structure of the ore deposit in detail and, what is more, with the ore-forming fluid data, carried out the effective constraint on the ore-forming conditions. The results show that the Liziping ore deposit mainly experienced three periods of tectonic deformation. In the early time, the strata of Liziping ore deposit developed a nearly NS-trending fold structure. In the middle period, several westward dipping approximately evenly spaced thrust faults were formed in the rocks. In the last stage, NW-striding and SW-striking strike-slip faults were formed. Orebody was mainly controlled by the two groups of strike-slip faults of the last stage. Ore structure is massive, breccia, disseminated in form, δ13CPDB values of all kinds of calcite are -1.3‰～ -2.3‰, averaging -1.7‰. δ18OSMOW values vary in the range of 6.9‰～21.0‰, averaging14.8‰. ∑REE(×10-6)values of all kinds of calcite are lower than 30. ∑ HREE has no obvious change and ∑ LREE has obvious difference. δEu values are lower than 1, exhibiting a medium europium negative anomaly. δCe has no significant anomalies. These features indicate that the evolution of the ore-forming fluid obeyed certain evolution regularity. The research results show that the C from the ore-forming fluid in the Liziping Pb-Zn deposit was derived from marine carbonate solution, whereas meteoric waters constantly entered the ore-forming fluid through percolation. The ore-forming fluid was in the form of underground shallow circulating waters. In combination with previous study of the Sanjiang region, the Liziiping Pb-Zn ore deposit should be formed from collision orogenics, and its ore body occurred in the tectonic fracture zone. |
| keywords:geology ore-controlling structure carbon and oxygen stable isotoperare rare earth elements Liziping Pb-Zn deposit |
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