首页> 外文会议>Asia Current Research on Fluid Inclusion Fifth Meeting >HYDROTHERMAL METALLOGENY OF THE MIAOLING GOLD DEPOSIT IN SONGXIAN COUNTY, HENAN PROVINCE: STUDIES ON ORE GEOLOGY AND FLUID INCLUSIONS
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HYDROTHERMAL METALLOGENY OF THE MIAOLING GOLD DEPOSIT IN SONGXIAN COUNTY, HENAN PROVINCE: STUDIES ON ORE GEOLOGY AND FLUID INCLUSIONS

机译:河南省嵩县苗岭金矿床热液成矿作用:矿床地质与流体包裹体研究

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摘要

(1) Based on cross-cutting relationships betweenrnore veins, mineral assemblages,three mineralizationrnstages have been identified: pyrite-quartz stage,rnquartz-pyrite stage, quartz-carbonate stage.rn(2) Experiment results display that the ore-formingrnfluids in Miaoling gold deposit evolved fromrnCO_2-H_2O-NaCl magmatic hydrothermal system thatrnintermediate-low in temperature and salinitie andrncontaining CO_2 into H_2O-NaCl meteoric hydrothermalrnsystem that low in temperature and salinity,rnpoor in CO_2.
机译:(1)根据矿脉,矿床组合的横切关系,确定了三个矿化阶段:黄铁矿-石英阶段,石英-黄铁矿阶段,石英-碳酸盐阶段。(2)实验结果表明,苗岭成矿流体金矿床由温度低,盐度中等,含CO_2的CO_2-H_2O-NaCl岩浆热液系统演化成温度低,盐度低,CO_2低的H_2O-NaCl流星热液系统。

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  • 会议地点 Xian(CN)
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    School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China (157019112@qq.com);

    MRL Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China (yehuishou@163.com);

    School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China;

    School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China;

    School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China;

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