| 甘肃阳坝铜多金属矿床流体包裹体及S、Pb同位素组成特征 |
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| 引用本文： | 苗雅娜,张宝林,苏艳平,刘瑞麟,李会中,毛剑锋.甘肃阳坝铜多金属矿床流体包裹体及S、Pb同位素组成特征[J].矿床地质,2019,38(1):29-47. |
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| 作者姓名： | 苗雅娜 张宝林 苏艳平 刘瑞麟 李会中 毛剑锋 |
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| 作者单位： | 中国科学院地质与地球物理研究所中国科学院矿产资源研究重点实验室,北京100029;中国科学院地球科学研究院,北京100029;中国科学院大学,北京100049;自然资源部成矿作用与资源评价重点实验室中国地质科学院矿产资源研究所,北京100037;北京大学造山带与地壳演化重点实验室,北京100871;甘肃阳坝铜业有限公司,甘肃康县,746511 |
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| 基金项目： | 中国科学院地质与地球物理研究所自主创新项目（编号：31351460）的资助 |
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| 摘 要： | 甘肃省阳坝铜多金属矿床位于碧口地体的东北部,矿体呈层状、似层状赋存于碧口群阳坝组细碧凝灰岩和凝灰质千枚岩的过渡部位,根据矿床地质特征,将成矿期划分为海底火山喷流沉积期和变质热液叠加改造期。基于对阳坝矿床详细的野外观察和矿相学的研究,通过对矿床流体包裹体和S、Pb同位素的研究,总结矿床的成矿流体性质和成矿物质来源,探讨成矿机制。研究表明,阳坝矿床海底火山喷流沉积期流体包裹体类型主要为水溶液包裹体,成矿流体均一温度为135～336℃,盐度w(NaCl_(eq))为0.70%～10.61%,密度为0.58～0.97g/cm~3;包裹体气相成分以H_2O为主,含少量的CO_2和N_2,属于中低温、低盐度的H_2O-NaCl流体体系,与典型VMS型矿床成矿流体特征相似;变质热液叠加改造期流体包裹体类型主要为水溶液包裹体、CO_2-H_2O包裹体和纯CO_2包裹体,成矿流体均一温度为179～384℃,盐度w(NaCl_(eq))为3.39%～14.78%,密度为0.61～0.99 g/cm~3,包裹体气相成分富含CO_2及少量N_2,属于中高温、低盐度的H_2O-CO_2-NaCl±N_2流体体系,与区域上造山型金矿成矿流体特征一致,均为来自深部的变质流体。喷流沉积期矿石硫化物的δ~(34)S为-7.5‰～3.4‰,均值为-0.46‰,成矿热液δ~(34)S_(∑S)值≈3.73‰,变质热液叠加改造期硫化物的δ~(34)S为-6.7‰～3.3‰,均值-0.575‰,均显示幔源硫的特征。喷流沉积期(~(206)Pb/~(204)Pb=17.505～18.008、~(207)Pb/~(204)Pb=15.521～15.558、~(208)Pb/~(204)Pb=37.494～37.851)与变质热液叠加改造期(~(206)Pb/~(204)Pb=17.293～17.947、~(207)Pb/~(204)Pb=15.498～15.542、~(208)Pb/~(204)Pb=37.388～37.640)的矿石硫化物的Pb同位素组成相近,认为2期矿石铅具有相同来源。通过与阳坝组火山岩、阳坝岩体的Pb同位素组成对比,并结合Pb同位素源区特征值、构造模式图解和△β-△γ成因分类图解分析,认为矿石铅来自上地壳和地幔的混合。阳坝铜多金属矿床属于海底火山喷流沉积-变质热液叠加改造型矿床。
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| 关 键 词： | 地质学 流体包裹体 S、Pb同位素 阳坝铜多金属矿床 碧口地体 |
| 收稿时间： | 2018/6/1 0:00:00 |
| 修稿时间： | 2018/12/9 0:00:00 |
Fluid inclusions and sulfur and lead isotopic composition of Yangba Cu-polymetallic deposit in Gansu Province |
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| MIAO YaN,ZHANG BaoLin,SU YanPing,LIU RuiLin,LI HuiZhong and MAO JianFeng.Fluid inclusions and sulfur and lead isotopic composition of Yangba Cu-polymetallic deposit in Gansu Province[J].Mineral Deposits,2019,38(1):29-47. |
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| Authors: | MIAO YaN ZHANG BaoLin SU YanPing LIU RuiLin LI HuiZhong and MAO JianFeng |
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| Institution: | Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Institute of Earth Science, Chinese Academy of Sciences, Beijing 100029, China;University of Chinese Academy of Sciences, Beijing 100049, China,Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Institute of Earth Science, Chinese Academy of Sciences, Beijing 100029, China;University of Chinese Academy of Sciences, Beijing 100049, China,Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Institute of Earth Science, Chinese Academy of Sciences, Beijing 100029, China;University of Chinese Academy of Sciences, Beijing 100049, China,MNR Key Laboratory of Metallogeny and MineralAssessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Key Laboratory of Orogen and Crust Evolution, Ministry of Education, Peking University, Beijing 100871, China,Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Institute of Earth Science, Chinese Academy of Sciences, Beijing 100029, China;University of Chinese Academy of Sciences, Beijing 100049, China and Gansu Yangba Copper Mining Co., Ltd., Kangxian 746511, Gansu, China |
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| Abstract: | |
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| Keywords: | geology fluid inclusions S-Pb isotopes Yangba copper polymetallic deposit Bikou Terrane |
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