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甘肃北山地区公婆泉铜矿区岩体年龄及其地质意义
引用本文:吕昶良,杨富强,罗家书,马文富,刘文勋,石伟民.甘肃北山地区公婆泉铜矿区岩体年龄及其地质意义[J].矿产与地质,2021(1):83-89.
作者姓名:吕昶良  杨富强  罗家书  马文富  刘文勋  石伟民
作者单位:广西壮族自治区地球物理勘察院;中国-东盟地学合作中心(南宁)
基金项目:广西壮族自治区地质矿产勘查开发局“广西关键矿产资源深部勘查人才小高地项目”(2020年度)资助。
摘    要:为更好地分析甘肃北山地区公婆泉铜矿的成矿时代及成矿过程,对公婆泉铜矿英安斑岩、花岗闪长斑岩进行了LA-ICP-MS锆石U-Pb定年。结果显示,英安斑岩形成于(431.0±8.8)Ma,而花岗闪长斑岩形成于(439.6±7.1)Ma。总结前人的研究成果,认为公婆泉铜矿存在至少两期成矿事件,早期为斑岩成矿,形成于440~430 Ma;晚期为热液叠加,与韧性剪切作用密切相关,形成于372~336 Ma。认为公婆泉—月牙山地体为岛弧带,公婆泉铜矿形成于岛弧环境。

关 键 词:公婆泉铜矿  英安斑岩  花岗闪长斑岩  甘肃北山

Isotopic age of rock mass in Gongpoquan mining area in Beishan of Gansu and its geological significance
LYU Changliang,YANG Fuqiang,LUO Jiashu,MA Wenfu,LIU Wenxun,SHI Weimin.Isotopic age of rock mass in Gongpoquan mining area in Beishan of Gansu and its geological significance[J].Mineral Resources and Geology,2021(1):83-89.
Authors:LYU Changliang  YANG Fuqiang  LUO Jiashu  MA Wenfu  LIU Wenxun  SHI Weimin
Institution:(Geophysical Survey Institute of Guangxi Zhuang Autonomous Region,Liuzhou 545005,Guangxi,China;China-ASEAN Geosciences Cooperation Center,Nanning 530023,Guangxi,China)
Abstract:In order to better understand the mineralization age and process of Gongpoquan copper deposit in Beishan area,Gansu,LA-ICP-MS zircon U-Pb dating analysis is caaried out for dacite porphyry and granodiorite porphyry in the mining area.The result indicates that the isotopic ages of dacite porphyry and granodiorite porphyry are(431.0±8.8)Ma and(439.6±7.1)Ma,respectively.According to the previous research result,it is considered that there are at least two mineralization stages in Gongpoquan Cu deposit.The first stage is characterized by porphyry mineralization at 440-430 Ma.The second stage is superimposed by the hydrothermal mineralization which is closely related to the ductile shear process at 372-336 Ma.It is further proposed that Gongpoquan-Yueyashan terrane is an island arc belt,and that Gongpoquan Cu deposit is formed in the island arc environment.
Keywords:Gongpoquan Cu deposit  dacite porphyry  granodiorite porphyry  Beishan of Gansu
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