| 内蒙古好力宝斑岩型铜钼矿床流体特征和矿床成因 |
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| 引用本文： | 曲高勇,付丽娟,黄广环,王可勇,孙清飞,崔志磊.内蒙古好力宝斑岩型铜钼矿床流体特征和矿床成因[J].黄金,2021(1):7-14. |
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| 作者姓名： | 曲高勇 付丽娟 黄广环 王可勇 孙清飞 崔志磊 |
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| 作者单位： | 吉林大学地球科学学院;内蒙古山金地质矿产勘查有限公司;新疆大学地质与采矿工程学院;国土资源部东北亚矿产资源评价重点实验室 |
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| 基金项目： | 山东黄金集团有限公司科技项目(SD2018-6)。 |
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| 摘 要： | 好力宝矿床位于西拉木伦成矿带东部,为斑岩型铜钼矿床。矿体主要赋存于斜长花岗斑岩的角砾岩带中,与斜长花岗斑岩关系密切,成矿作用划分为3个阶段:石英-黄铜矿-黄铁矿-辉钼矿阶段(Ⅰ)、黄铁矿-方铅矿-闪锌矿-辉钼矿-石英脉阶段(Ⅱ)、石英-方解石-萤石阶段(Ⅲ)。流体包裹体测试结果表明:流体包裹体主要为气液两相包裹体(L型)、含CO 2包裹体(C型)和纯CO 2包裹体(PC型)。成矿Ⅰ阶段主要包括L型、C型和PC型流体包裹体,为典型的高温(集中在380.0℃~400.0℃)、中低盐度(集中在7.50%~8.50%)的CO2-NaCl-H2O体系;成矿Ⅱ阶段主要包括L型和C型流体包裹体,属于高温(集中在330.0℃~350.0℃)、低盐度(集中在4.25%~5.00%)的CO2-NaCl-H2O体系;成矿Ⅲ阶段仅包括L型流体包裹体,属于中低温(集中在280.0℃~300.0℃)、低盐度(集中在2.00%~2.75%)的NaCl-H2O体系。氢-氧同位素测试结果显示,δD V-SMOW为-115.8‰~-94.5‰,δ18O H2O为-8.32‰~0.28‰,暗示成矿流体主要来源于岩浆,含有少量大气降水。研究结果表明,该矿床成矿流体为中高温、中低盐度流体,流体不混溶促使金属矿物发生沉淀富集。
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| 关 键 词： | 流体包裹体 成矿阶段 氢-氧同位素 矿床成因 好力宝矿床 |
Ore-forming fluids characteristics and deposit genesis of Haolibao Porphyry Cu-Mo Deposit,Inner Mongolia |
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| Qu Gaoyong,Fu Lijuan,Huang Guanghuan,Wang Keyong,Sun Qingfei,Cui Zhilei.Ore-forming fluids characteristics and deposit genesis of Haolibao Porphyry Cu-Mo Deposit,Inner Mongolia[J].Gold,2021(1):7-14. |
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| Authors: | Qu Gaoyong Fu Lijuan Huang Guanghuan Wang Keyong Sun Qingfei Cui Zhilei |
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| Affiliation: | (College of Earth Sciences,Jilin University;Inner Mongolia Shandong Gold Geological Minerals Survey Co.,Ltd.;College of Geology and Mining Engineering,Xinjiang University;MNR Key Laboratory of Mineral Resources Evaluation in Northeast Asia) |
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| Abstract: | Haolibao Deposit,located in the east of Xilamulun metallogenic belt,is a porphyry Cu-Mo deposit.Ore bodies are mainly hosted in breccia zone of plagioclase granite porphyry,and are closely related to plagiogranite porphyry.The mineralization can be divided into 3 stages:quartz-chalcopyrite-pyrite-molybdenite stage(Ⅰ);pyrite-galena-sphalerite-molybdenite-quartz vein stage(Ⅱ);quartz-calcite-fluorite stage(Ⅲ).The results of fluid inclusions test show that the fluid inclusions are mainly gas-liquid two-phase inclusions(L type),CO2-containing inclusions(C type)and pure CO2 inclusions(PC type).StageⅠmainly includes L,C and PC type fluid inclusions,which are typical high temperature(380℃-400℃)and medium-low salinity(7.5%-8.5%)CO2-NaCl-H2O system;Stage Ⅱ mainly includes L and C type fluid inclusions,belonging to high temperature(330℃-350℃)and low salinity(4.25%-5.00%)CO2-NaCl-H2O system;Stage Ⅲ only includes L type fluid inclusions,belonging to the medium-low temperature(280℃-300℃)and low salinity(2.00%-2.75%)NaCl-H 2O system.The results of H-O isotope test is that δD V-SMOW is-115.8‰--94.5‰,δ18O H2O is-8.32‰-0.28‰,implying that the ore-forming fluid of the deposit is mainly from magma with a small amount of meteoric water.The results show that the ore-forming fluid of the deposit is of medium high temperature and low salinity,and the immiscibility of fluid promotes the precipitation and enrichment of metal minerals. |
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| Keywords: | fluid inclusion ore-forming stage mineralization stage H-O isotope deposit genesis Haolibao Deposit |
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