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焦家金矿成矿流体垂向变化特征及对胶东金成矿过程的启示
The Vertical Variation Characteristics of Ore-forming Fluids of the Jiaojia Deposit: Implications for Mineralizing Processes of Gold Deposits in the Jiaodong Peninsula

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胡换龙 1,2,3   姜晓辉 1,4   梁改忠 1,2   杨奎锋 1,2   范宏瑞 1,2 *  
文摘 为探讨焦家金矿成矿流体的时空演化特性,在焦家金矿①号和③号矿体纵深450 m的剖面上采集矿化样品,对不同阶段、不同深度石英脉中流体包裹体进行显微测温以及成矿流体特征垂向对比研究。结果显示,成矿早阶段石英主要捕获H_2OCO_2型包裹体,其完全均一温度为271~ 359 ℃,盐度为6.0%~ 10.0% NaCl_(eqv),X_(CO_2)为0.1~ 0.15。主成矿阶段石英中捕获大量H_2O-CO_2型、H_2O型和CO_2型包裹体,它们的完全均一温度为198 ~ 315 ℃,盐度为6.5%~ 8.5% NaCl_(eqv)。成矿晚阶段石英中只发育H_2O单相和气液两相包裹体,其完全均一温度为102~ 188 ℃,盐度为0.2%~ 3.8% NaCl_(eqv)。研究显示,焦家金矿成矿流体与其他胶东金矿成矿流体特征与演化过程一致,且在纵深450 m剖面上保持不变。与前人研究成果对比发现,胶东金矿具有统一的流体来源,但成矿物质显示出更为复杂的来源,应有源于沉积地层的物质加入。
其他语种文摘 In order to explore the temporal and spatial evolution characteristics of the ore-forming fluid in the Jiaojia gold deposit,samples at various levels with depths of elevations varying from-167 to-600 m were taken from the No.① and ③ gold orebodies of the Jiaojia deposit. For undertaking the vertical contrast study of ore-forming fluid characteristics,the microthermometric study of fluid inclusions in quartz veins of different ore-stages from samples collected at different depths has been carried out. The results show that early ore-stage quartzs mainly captured H_2O-CO_2-type fluid inclusions that had their total homogenization temperatures of 271-359 ℃,salinities of 6.0%-10.0%NaCl_(eqv),and X_(CO_2) values of 0.1-0.15. The main ore-stage quartzs captured a large amounts of H_2O-CO_2,H_2O and CO_2 type fluid inclusions with their total homogenization temperatures of 198-315 ℃ and salinities of 6.5%-8.5% NaCl_(eqv). The late stage quartzs only captured H_2O type fluid inclusions that had the total homogenization temperatures of 102-188 ℃ and salinities of 0.2%-3.8%NaCl_(eqv). These microthermometric results suggest that the ore-forming fluid of the Jiaojia gold deposit has the consistent characteristics and evolution process with those of other gold deposits in the Jiaodong Peninsula,and the ore-forming fluid characteristics kept stable within the 450 m ranged vertical profile. Combining with results of previous and this studies,it is believed that gold deposits in the Jiaodong Peninsula should share the common ore-forming fluid source but could contain relatively complicated ore-forming material sources with the addition of various amounts of sedimentary strata-derived materials.
来源 矿物岩石地球化学通报 ,2021,40(6):1345-1356 【核心库】
DOI 10.19658/j.issn.1007-2802.2021.40.053
关键词 流体包裹体 ; 显微测温 ; 垂向对比 ; 焦家金矿 ; 胶东
地址

1. 中国科学院地质与地球物理研究所, 矿产资源研究中国科学院重点实验室, 北京, 100029  

2. 中国科学院大学地球科学学院, 北京, 100049  

3. 中国科学院地球化学研究所, 矿床地球化学国家重点实验室, 贵阳, 550081  

4. 核工业北京地质研究院, 北京, 100029

语种 中文
文献类型 研究性论文
ISSN 1007-2802
学科 地质学
基金 科技部重点研发计划重点专项 ;  国家自然科学基金
文献收藏号 CSCD:7121483

参考文献 共 51 共3页

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引证文献 1

1 李晓东 流体包裹体研究进展及其在矿床学中的应用 地质论评,2022,68(6):2305-2318
CSCD被引 3

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论文科学数据集

1. 湖南东北部万古-黄金洞金矿区流体包裹体地球化学数据(2020)

2. 湘东北横洞钴矿床白垩纪时期流体包裹体数据

数据来源:
国家青藏高原科学数据中心
PlumX Metrics
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