| 吉林荒沟山金矿床成矿流体特征 |
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| 引用本文： | 周向斌,李剑锋,王可勇,梁一鸿,张淼,韦烈民,王志高.吉林荒沟山金矿床成矿流体特征[J].地球科学,2016,41(1):121-130. |
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| 作者姓名： | 周向斌 李剑锋 王可勇 梁一鸿 张淼 韦烈民 王志高 |
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| 作者单位： | 1.吉林大学地球科学学院，吉林长春 130061 |
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| 基金项目： | 中国地质大学地质过程与矿产资源国家重点实验室开放课题基金项目GPMR201307辽宁师范大学校青年基金项目LS2015L016中国地质调查局地质调查项目1212011120156 |
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| 摘 要： | 荒沟山金矿床为吉南老岭金-多金属成矿带内较具代表性矿床之一，产于元古宇老岭群珍珠门组地层之中，受韧性剪切带构造控制.按地质特征、矿物组合及矿脉之间的穿切关系，将荒沟山金矿床热液成矿作用划分为Ⅰ黄铁矿-毒砂-石英阶段和Ⅱ晚期辉锑矿-乳白色石英两个阶段.系统的流体包裹体岩相学及显微测温研究表明:Ⅰ阶段石英中发育含CO2三相、碳质及气液两相3种类型的原生流体包裹体，成矿流体属不混溶的中低温、低盐度NaCl-H2O-CO2体系热液，在成矿过程中发生过不混溶作用而导致金等有用元素沉淀富集；Ⅱ阶段石英颗粒中主要发育气液两相包裹体，成矿流体属均匀的NaCl-H2O体系热液.碳、氢、氧同位素研究表明，Ⅰ阶段成矿流体主要来源于岩浆热液，Ⅱ阶段流体除继承早阶段的热液外，还有大气降水的混入；δD和δ13CV-PDB值分析结果证明两个成矿阶段流体均与地层发生过较强的水岩反应.矿床成因属于中温岩浆热液矿床.
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| 关 键 词： | 荒沟山金矿床 成矿流体 地球化学特征 矿床成因 吉林省东南部 |
| 收稿时间： | 2015-09-01 |
Geochemical Characteristics of Ore-Forming Fluid inHuanggoushan Gold Deposit,Jilin Province |
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| Abstract: | Occurred in Zhenzhumen Formation of Laoling Group of Proterozoic Era and controlled by ductile shear belt, the Huanggoushan gold deposit is one of the most representative deposits in Laoling gold-polymetallic metallogenic belt in southern Jilin Province. Based on the geological characteristics, mineral assemblage and the crosscutting relationship between different kinds of veins, the hydrothermal mineralization processes can be divided into two main stages, namely, stageⅠpyrite arsenopyrite quartz and stageⅡ later stibnite-milky quartz. Systematic study on petrography and microthermometry of fluid inclusions shows that quartz of Stage Ⅰcontains three types of primary fluid inclusions, which are CO2 bearing three phases, carbonic and aqueous two phases inclusions respectively, and the ore forming fluid is of medium to low temperature and low salinity NaCl-H2O-CO2 kind of solutions and immiscibility happened in the ore forming process, which led to the enrichment of gold etc; in quartz of Stage Ⅱ, there are aqueous two phases fluids only and ore forming fluid is of homogeneous NaCl-H2O kind of solutions. Isotopic studies of carbon, hydrogen and oxygen show that the ore forming fluids of mineralization Stage Ⅰ mainly derived from magmatic solutions, whereas fluids of mineralization stage Ⅱ mainly came from meteoric water in addition to the relicts of stage Ⅰ ore forming solutions. The values of δD and δ13CV-PDB reveal that the ore forming fluids of both mineralization Stage Ⅰ and Ⅱ all experienced strong rock water reaction. The genesis of the gold deposit is medium temperature magmatic hydrothermal deposit. |
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