| 闪锌矿LA-ICP-MS微量元素组成对西藏纳如松多铅锌矿床成矿作用的制约 |
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| 引用本文： | 龚雪婧,杨竹森,庄亮亮,马旺.闪锌矿LA-ICP-MS微量元素组成对西藏纳如松多铅锌矿床成矿作用的制约[J].矿床地质,2019,38(6):1365-1378. |
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| 作者姓名： | 龚雪婧 杨竹森 庄亮亮 马旺 |
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| 作者单位： | 中国地质科学院,北京 100037;中国地质调查局—中国地质科学院地球深部探测中心,北京 100037;中国地质科学院矿产资源研究所 自然资源部成矿规律与资源评价重点实验室,北京,100037;中国地质科学院地质研究所,北京,100037 |
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| 基金项目： | 本文得到国家重点研发计划"深地资源勘查开采"重点专项（编号：2016YFC0600306）地质调查项目（编号：DD20179172）和国家自然科学基金（编号：41802097）的联合资助 |
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| 摘 要： | 西藏纳如松多铅锌矿床是冈底斯北侧Pb-Zn-Ag-Mo成矿带中规模最大且最为典型的与斑岩系统相关的铅锌矿床,发育有多种矿化样式。本次研究选取该矿床隐爆角砾岩型矿体中的闪锌矿开展LA-ICP-MS微量元素组成研究,发现其中Fe含量不高,不属于高温铁闪锌矿,以富集Cd、Mn、Co,而贫In、Ga、Ge、Se、Te为特征。闪锌矿In/Ga值、In/Ge值及Zn/Cd值指示纳如松多隐爆角砾岩型铅锌矿体形成于中低温环境,且属于热液型矿床的范畴。闪锌矿原位微量元素特征指示纳如松多铅锌矿床的形成主要受到来自于岩浆热液作用的影响和控制,成矿物质主要来自于深部斑岩岩浆系统。
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| 关 键 词： | 地球化学 闪锌矿 微量元素组成 LA-ICP-MS 铅锌矿床 西藏 |
| 收稿时间： | 2017/9/29 0:00:00 |
| 修稿时间： | 2019/9/29 0:00:00 |
Genesis of Narusongduo Pb-Zn deposit, Tibet: Constraint from in-situ LA-ICPMS analyses of minor and trace elements in sphalerite |
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| GONG XueJing,YANG ZhuSen,ZHUANG LiangLiang and MA Wang.Genesis of Narusongduo Pb-Zn deposit, Tibet: Constraint from in-situ LA-ICPMS analyses of minor and trace elements in sphalerite[J].Mineral Deposits,2019,38(6):1365-1378. |
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| Authors: | GONG XueJing YANG ZhuSen ZHUANG LiangLiang and MA Wang |
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| Institution: | Chinese Academy of Geological Sciences, Beijing 100037, China;SinoProbe Center, Chinese Academy of Geological Sciences and China Geological Survey, Beijing 100037, China,MNR Key Laboratory and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China,Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China and Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China |
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| Abstract: | The Narusongduo lead-zinc deposit is the largest and most typical Pb-Zn deposit in the Pb-Zn-Ag-Mo metallogenic belt on the northern side of Gangdise belt. It has multiple mineralization styles. In this study, trace elements in sphalerite of the cryptoexplosion breccia type orebody were analyzed by LA-ICP-MS, and the result shows that the Fe content of sphalerite is not high and hence sphalerite does not belong to Fe sphalerite. The sphalerite is characterized by enrichment of Cd, Mn and Co and poor concentrations of In, Ga, Ge, Se and Te. The In/Ga, In/Ge and Zn/Cd ratios indicate that the deposit is a kind of hydrothermal deposit formed in a middle-low temperature environment. The values and discriminant diagram of the characteristic elements in the analyzed sphalerite show that the formation of Narusongduo deposit was mainly controlled and influenced by magmatic hydrothermal activities and the ore-forming material dominantly came from the porphyry magma system. |
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| Keywords: | geochemistry sphalerite trace elements composition LA-ICP-MS Pb-Zn deposit Tibet |
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