| 河南小秦岭杨砦峪金矿床成矿流体特征 |
| Received:January 04, 2013 Revised:September 12, 2013 点此下载全文 |
| 引用本文：XIONG SuoFei,DING ZhenJu,YAO ShuZhen,XIONG Jie,HU XinLu,HE MouChun,TAN ManTang.2013.Characteristics of ore-forming fluid of Yangzhaiyu gold deposit in Xiaoqinling gold district, Henan Province[J].Mineral Deposits,32(6):1249~1261 |
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| Author Name | Affiliation | E-mail | | XIONG SuoFei | Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China | | | DING ZhenJu | Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China | | | YAO ShuZhen | Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China | szyao@cug.edu.cn | | XIONG Jie | Guangxi Land and Resources Planning Institute, Nanning 530022, Guangxi, China | | | HU XinLu | Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China | | | HE MouChun | Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China
State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences, Wuhan 430074, Hubei, China | | | TAN ManTang | Faculty of Earth Resources, 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（编号：20089939）”和中国地质大学（武汉）教学实验室开放基金（编号：SKJ2011112）共同资助 |
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| 中文摘要:河南省杨砦峪金矿床位于华北克拉通南缘，是小秦岭地区大型的石英脉型金矿床。据野外观察，成矿过程经历了4个阶段：Ⅰ黄铁矿-石英脉阶段；Ⅱ石英-黄铁矿阶段；Ⅲ石英-多金属硫化物阶段；Ⅳ石英-碳酸盐阶段。包裹体岩相学、显微测温以及激光拉曼显微探针研究显示，该矿床为CO2-H2O-NaCl±CH4流体体系，并且发生不混溶。从第Ⅰ成矿阶段到Ⅳ成矿阶段，流体包裹体的均一温度范围分别是307~407℃，270~320℃，225~272℃和166~226℃，呈现逐步降低的趋势；盐度w（NaCleq）平均值分别为7.3%，7.1%，9.0% 和6.4%。各阶段成矿压力为120~178 MPa，85~140 MPa，75~130 MPa和60~122 MPa，呈现逐渐降低的趋势。流体不混溶作用是导致杨砦峪矿质沉淀的重要原因，其诱因可能与控矿断裂由压扭转为张扭所导致的构造减压有关。 |
| 中文关键词:地球化学 流体包裹体 流体不混溶 杨砦峪金矿 小秦岭金矿田 |
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| Characteristics of ore-forming fluid of Yangzhaiyu gold deposit in Xiaoqinling gold district, Henan Province |
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| Abstract:Located in the southern margin of the North China Craton, the Yangzhaiyu gold deposit in Henan Province is one of numerous lode gold deposits in Xiaoqinling region. The ore-forming process can be divided into four stages, i.e., Ⅰpyrite-quartz vein stage, Ⅱ quartz-pyrite stage, Ⅲ quartz-polymetallic sulfides stage, and Ⅳ quartz-carbonate stage. Researches based on petrography, fluid inclusion tests and Laser Raman spectroscopic analysis suggest that ore-forming fluids are mainly composed of CO2-H2O-NaCl±CH4. There is an immiscible process in the fluid system. The homogenization temperatures of ore-forming fluids from stageⅠto stage Ⅳ are 307.0~406.8℃,270.3~319.6℃,225.4~272.1℃ and 166.3~226.3℃ respectively, with the corresponding average salinities being 7.25% NaCleqv,7.14% NaCleqv,8.97% NaCleqv and 6.39% NaCleqv. The trapping pressures of fluid inclusions are estimated to be 120~178 MPa, 85~140 MPa, 75~130 MPa and 60~122 MPa for each stage. Fluid immiscibility must have played an important role in ore genesis. The cause of fluid immiscibility might have been related to tectonic decompressing. |
| keywords:geochemistry fluid inclusions fluid immiscibility Yangzhaiyu gold deposit Xiaoqinling gold district |
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