| 陕西省桐峪金矿床成矿流体研究 |
| Received:September 14, 2012 Revised:February 05, 2013 点此下载全文 |
| 引用本文：XU YanMing,ZHOU ZongGui,YAO ShuZhen,CHEN Jun,XIONG SuoFei,ZHOU XiaoNing.2013.Ore-forming fluid studies of Tongyu gold deposit, Shaanxi Province[J].Mineral Deposits,32(5):1011~1025 |
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| Author Name | Affiliation | E-mail | | XU YanMing | Faculty of Earth Resource, China University of Geosciences, Wuhan 430074, Hubei, China
Hubei Geological Survey, Wuhan 430074, Hubei, China | | | ZHOU ZongGui | Faculty of Earth Resource, China University of Geosciences, Wuhan 430074, Hubei, China | zhouzg@cug.edu.cn | | YAO ShuZhen | Faculty of Earth Resource, China University of Geosciences, Wuhan 430074, Hubei, China | | | CHEN Jun | Faculty of Earth Resource, China University of Geosciences, Wuhan 430074, Hubei, China | | | XIONG SuoFei | Faculty of Earth Resource, China University of Geosciences, Wuhan 430074, Hubei, China | | | ZHOU XiaoNing | Faculty of Earth Resource, China University of Geosciences, Wuhan 430074, Hubei, China | |
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| 基金项目:本文得到全国危机矿山接替资源找矿综合研究项目《小秦岭地区金矿床成矿规律总结研究》(20089939)资助 |
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| 中文摘要:桐峪金矿床位于华北地台南缘小秦岭金矿带的西段。矿体多呈薄板状、脉状和透镜状产出。赋矿围岩为太古代太华群变质岩系。围岩蚀变主要有绢云母化、硅化、碳酸盐化等。文章对该矿床的流体包裹体进行了岩相学研究,并开展了显微测温、流体成分及氢、氧同位素测试,模拟估算了密度、压力、深度。结果表明,第Ⅰ、Ⅱ、Ⅲ阶段流体包裹体的均一温度、盐度分别为:280~360℃,3%~11%;190~330℃,3%~15%;150~290℃,1%~11%。包裹体液相成分中阳离子以Na+、K+、Ca2+为主,阴离子以Cl-为主,SO42-次之;气相成分以H2O、CO2和N2为主,含少量O2、CH4。流体为弱还原性。成矿温度属中(高)温,低盐度,成矿压力为78~220 MPa,成矿深度大约为3~8 km。包裹体水的δDV-SMOW值为-44.4‰~-81.8‰,δ18O水值为0.01‰~6.65‰。成矿流体成矿初期为岩浆水或者混有少量变质水的混合水,成矿后期有大气降水的混入。Au在成矿流体中主要是以Au(HS)2-的形式进行迁移,其次为Au2S(HS)22-。 |
| 中文关键词:地球化学 成矿流体 氢、氧同位素 桐峪金矿床 |
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| Ore-forming fluid studies of Tongyu gold deposit, Shaanxi Province |
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| Abstract:The Tongyu gold deposit, lying in southern North China platform, is tectonically located in western Xiao Qinling gold metallogenic belt. Ore bodies, hosted in metamorphic rocks of Achaean Taihua Group, occur as sheets, veins and lenses. Wall rock alteration is well developed in the gold deposit; there are carbonatization, sericitization, silicification, choritization etc. The authors approximately calculated the density, pressure, depth on the basis of studies of petrography and microscopic differential thermometry of fluid inclusions as well as components and H-O isotopic compositions of the fluids. Homogenization temperatures of fluid inclusions of the three stages are 280~360℃,190~330℃ and 150~290℃ respectively, with salinities of 3%~11%, 3%~15% and 1%~11%. The liquid part of the fluid inclusion mainly contains Na+, K+, Ca2+. Cl- is the anion of the highest value, and SO42- takes the second place. The gas phase composition primarily contains H2O, CO2 and N2, followed by a small amount of O2 and CH4. The fluid inclusions are characterized by slight reduction. Mineralization took place at intermediate temperature. Based on fluid inclusion studies,the authors consider that the ore-forming hydrothermal fluid is of low salinity. The ore-forming pressures are from 78 MPa to 220 MPa, suggesting that the depth ranges from 3 km to 8 km. (D values vary in the range of-44.4‰~-81.8‰, and δ18O(H2O) in the range of 0.01‰~6.65‰. The δD-δ18O isotopic diagrams show that the early stage was dominated by magmatic water or mixed magmatic water, whereas at the late stage there was some addition of atmospheric precipitation. The authors have reached the conclusion that Au in the ore-forming fluid mainly migrated in the form of Au (HS)2-, followed by Au2S (HS)22-. |
| keywords:geochemistry ore-forming fluid H-O isotope Tongyu gold deposit |
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