| 广西云开地区新华铅锌(银)矿床白云母Ar-Ar年代学及其成矿动力学背景 |
| Received:August 02, 2016 Revised:June 26, 2017 点此下载全文 |
| 引用本文：ZHANG XuBo,WANG MinFang,PI DaoHui,LIU Kun,GUO XiaoNan,WANG YanBo.2017.Ar-Ar geochronology of muscovite and metallogenic geodynamics of the Xinhua Pb-Zn(Ag) deposit in Yunkai area, Guangxi[J].Mineral Deposits,36(4):979~991 |
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| Author Name | Affiliation | E-mail | | ZHANG XuBo | Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China | | | WANG MinFang | Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China | wang-minfang@163.com | | PI DaoHui | Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China | | | LIU Kun | Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China | | | GUO XiaoNan | No.2 Geological Survey of Henan Province, Zhengzhou 450000, Henan, China | | | WANG YanBo | Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China | |
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| 基金项目:本文得到中央高校基本科研业务费专项资金（编号：CUG120702）、国家自然科学基金面上项目（批准号：41272097）、中国地质大学（武汉）教学实验室开放基金项目（编号：SKJ2015010、SKJ2015017）联合资助 |
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| 中文摘要:新华铅锌（银）矿床位于钦杭成矿带南端云开地区的六万大山隆起区，是以铅锌为主的含银热液脉型多金属矿床。矿体赋存在含堇青石黑云母花岗岩中，主要呈脉状和透镜状产出。文章利用激光阶段加热技术对与矿化密切共生的白云母进行Ar-Ar年龄测定。结果表明，新华铅锌（银）多金属矿床的40Ar/39Ar坪年龄为（165.3±1.6） Ma（MSWD=0.38），反等时线年龄为（165.2±1.6） Ma（MSWD=0.42），等时线年龄和坪年龄一致，代表了白云母的冷却年龄和矿床的形成年龄，表明该矿床的形成与云开地区燕山早期的岩浆活动有关，这与区域成矿事件相吻合。结合前人对华南地区地球动力学背景的研究成果，初步认为新华铅锌（银）矿床形成于中-晚侏罗世碰撞板块边缘再次活化，岩石圈伸展的构造背景。 |
| 中文关键词:地球化学 40Ar/39Ar年代学 白云母 新华矿床 成矿动力学 云开地区 |
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| Ar-Ar geochronology of muscovite and metallogenic geodynamics of the Xinhua Pb-Zn(Ag) deposit in Yunkai area, Guangxi |
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| Abstract:The Xinhua Pb-Zn-(Ag) deposit,located in the Liuwandashan granite uplift zone of western Yunkai area which constitutes a part of the southern section of the Qinzhou Bay-Hangzhou Bay (QBHB) metallagenic belt in south China, is a hydrothermal vein type polymetallic deposit. Orebodies exist in the fault zone of the cordierite biotite granite, in the veinlike and lenticular forms. This paper presents precise 40Ar/39Ar ages of muscovite related to the mineralization by laser incremental 40Ar/39Ar analysis. Muscovite yielded a well-defined 40Ar/39Ar plateau age of (165.3±1.6) Ma (MSWD=0.38) and inverse age of (165.2±1.6) Ma (MSWD=0.42). These ages can represent the formation age of the deposit and suggest that the Xinhua deposit is related to the magmatic activities of Yanshanian period, which is in conformity with things of the regional metallogenic events. Combined with the previous studies of the geodynamic settings of South China, the authors consider that the Xinhua deposit was most likely formed in a setting of lithospheric extension because of plate boundary reactivation in the mid-late Jurassic period. |
| keywords:geochemistry 40Ar/39Ar geochronology muscovite Xinhua deposit metallogenic geodynamics Yunkai area |
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