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作 者:赵兴展 邓小华 张静[1] 祝新友[3] 何西恒 舒磊 Zhao Xingzhan;Deng Xiaohua;Zhang Jing;Zhu Xinyou;He Xiheng;Shu Lei(School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing,100083,China;Hami Redstone Mining Co.,Ltd.,Hami,Xinjiang,839000,China;Beijing Institute of Mineral Geology Co.,Ltd.,Beijing,100012,China;MNR Key Laboratory of Gold Mineralization Process and Resource Utilization,Shandong Institute of Geological Sciences,Jinan,Shandong,250013,China)
机构地区:[1]中国地质大学(北京)地球科学与资源学院,北京100083 [2]哈密红石矿业有限公司,新疆哈密839000 [3]北京矿产地质研究院有限责任公司,北京100012 [4]自然资源部金矿成矿
出 处:《新疆地质》2022年第1期20-26,共7页Xinjiang Geology
基 金:新疆高层次人才引进工程全职创新人才经费(新人社函〔2019〕39号);国家重点研发计划东天山卡拉塔格-黄山铜镍多金属矿带深部资源预测(2018YFC0604006)联合资助。
摘 要:矿床石英脉中发育3种类型的流体包裹体:C型、PC型及W型包裹体。测温结果显示:早阶段C型包裹体均一温度为340℃~480℃,盐度为6.1%~9.1%NaCl_(eqv);中阶段3种类型的包裹体均发育,均一温度为220℃~460℃,盐度5%~15.2%NaCl_(eqv);晚阶段只发育“W”型包裹体,均一温度为140℃~300℃,盐度为1.1%~8.1%NaCl_(eqv)。萨热阔布金矿床受阿巴宫断裂构造控制,整体呈脉状产于韧性剪切带内,流体以中-低温、低盐度、富CO_(2)为特征,与造山型矿床的流体特征十分相似,因此认为萨热阔布金矿为造山型金矿床。Three types of fluid inclusions are developed in the quartz veins of the deposit:C-type,PC-type and W-type inclusions.The temperature measurement results show that the homogenization temperature of C-type inclusions in the early stage is 340℃~480℃,and the salinity is 6.1%~9.1%NaCl_(eqv);the three types of inclusions in the middle stage are all developed,and the homogenization temperature is 220℃~460℃,and the salinity is 5~15.2 NaCl_(eqv);only W-shaped inclusions developed in the late stage,the homogenization temperature is 140℃~300℃,the salinity is 1.1~8.1NaCl_(eqv),the Sarekuobu gold deposit is controlled by the Abagong fault structure,and the whole vein is produced in ductile shear.In the cut zone,the fluid is characterized by medium-low temperature,low salinity,and rich CO_(2),which is very similar to the fluid characteristics of orogenic deposits.Therefore,the Sarekuobu gold deposit is an orogenic gold deposit.
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