| 吉林延边闹枝金矿床地质特征及矿床成因 |
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| 引用本文： | 杨帅师,卿敏,郝通顺,王可勇,万多,朴星海,边红业.吉林延边闹枝金矿床地质特征及矿床成因[J].世界地质,2010,29(4):607-613. |
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| 作者姓名： | 杨帅师 卿敏 郝通顺 王可勇 万多 朴星海 边红业 |
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| 作者单位： | 1． 内蒙古自治区地质勘查基金管理中心，呼和浩特010000; 2． 中国地质大学地球科学与资源学院，北京100083; 3． 武警黄金地质研究所，河北廊坊065000; 4． 内蒙古第二地质矿产勘查开发院，内蒙古临河015000; 5． 吉林大学地球科学学院，长春130061; 6． 武警黄金第一总队，哈尔滨150086 |
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| 基金项目： | 武警黄金指挥部地质科研项目资助(HJ-08-07-2) |
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| 摘 要： | 闹枝金矿床地处延边—东宁金矿带西段,为一主体产于海西期花岗闪长岩体内的石英脉型矿床。矿床地质特征及含金石英脉内流体包裹体研究结果表明,该区含金石英脉中主要发育气液两相及少量的含子矿物三相、气相--富气相包裹体。气液两相包裹体均一温度为283.5℃～375.9℃,盐度为3.4～8.13 wt%NaCl;富气相包裹体均一温度为416.5℃～431.6℃;含NaCl子矿物三相流体包裹体均一温度为303.9℃～393.2℃,盐度为38.21～45.3 wt%NaCl。包裹体氢、氧同位素分析结果表明,成矿流体以岩浆热液为主,可能混有少量大气降水。矿床成因属中温岩浆热液金矿床。
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| 关 键 词： | 地质特征 矿床成因 闹枝金矿床 吉林 |
Geological characteristics and genesis of Naozhi gold deposit in Yanbian area,Jilin Province |
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| YANG Shuai-shi,QING Min,HAO Tong-shun,WANG Ke-yong,WAN Duo,PIAO Xing-hai,BIAN Hong-ye.Geological characteristics and genesis of Naozhi gold deposit in Yanbian area,Jilin Province[J].World Geology,2010,29(4):607-613. |
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| Authors: | YANG Shuai-shi QING Min HAO Tong-shun WANG Ke-yong WAN Duo PIAO Xing-hai BIAN Hong-ye |
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| Institution: | YANG Shuai-shi1,2,QING Min3,HAO Tong-shun4,WANG Ke-yong5,WAN Duo5,PIAO Xing-hai5,BIAN Hong-ye6 1.The Management Center of Exploration Fund of Inner Mongolia,Huhehaote 010000,Inner Mongolia,China,2.College of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,3.Geological Institute of Gold Detachment of Chinese People's Armed Police Force,Langfang 065000,Hebei,4.No.2 Exploration and Development Institute of Mineral Resources of Inner Mongolia,Linhe 015000,Inner Mongol... |
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| Abstract: | Naozhi gold deposit located in the western sector of Yanbian—Dongning gold metallogenic belt,is a quartz vein type deposit occurred in Hercynian granodiorite.The analysis results of geological characteristics and the fluid inclusions in auriferous quratz veins show that the main types of fluid inclusions developed in auriferous quartz vein are gas-liquid two-phase,and a little daughter mineral-bearing three-phase as well as vapor phase fluid inclusions.The homogenization temperature of gas-liquid two-phase fluid inclusions is 283.5 ℃~375.9 ℃,with salintity 3.4~8.13 wt%NaCl;the homogenization temperature of vapor phase fluid inclusions is 416.5 ℃~431.6 ℃;and the homogenization temperature of NaCl daughter mineral-bearing three-phase fluid inclusions is 303.9 ℃~393.2 ℃,with salinity 38.21~45.3 wt%NaCl.The oxygen and hydrogen isotopes of fluid inclusions indicate that the ore-forming solutions mainly derived from magmatic fluids which mixed with a small amount of meteoric water.The gold deposit belongs to medium temperature magmatic hydrothermal type in origin. |
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| Keywords: | geological characteristics deposit genesis of ore deposit Naozhi gold deposit Jilin |
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