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Single grain Rb-Sr dating of euhedral and cataclastic pyrite from the Qiyugou gold deposit in western Henan, central China
作者姓名:HAN  YiGui  LI  XiangHui  ZHANG  ShiHong  ZHANG  YuanHou  CHEN  FuKun
作者单位:[1]State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China; [2]Laboratory for Radiogenic Isotope Geochemistry, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China [3]The College of Earth Sciences, Jilin University, Changchun 130061, China
基金项目:Supported jointly by the National Natural Science Foundation of China (Grant No.40032010-B) and the National Basic Research Program of China (Grant No.2006CB403505)
摘    要:The Rb-Sr isotopic dating of pyrite mineral from ore deposits can directly provide mineralization age. However, many geological factors may affect the Rb-Sr isotopic system,which baffles application of this method. Employing ultra-low procedural blank Rb-Sr method,we have dated pyrites separated from the No. 4 breccia pipe of the Qiyugou gold deposit,western Henan Province. Single grains of euhedral pyrite crystal with few microcracks yield an isochron age of 126 ± 11 Ma, which represents time of the main mineralization stage of the deposit. Pyrite grains of cataclastic type show nevertheless scattered Rb-Sr isotopic composition and no reasonable isochron can be defined. Crystal morphology and mineral inclusion studies reveal that Rb and Sr of pyrite mineral probably are preserved mainly in biotite, K-feldspar, and sericite mineral inclusions. The dating results likely suggest that cataclastic pyrite is not suitable for the Rb-Sr dating due to modification of the Rb-Sr isotopic system by later hydrothermal activity of fluid.

关 键 词:硫化铁矿  年代测定      形成时间
收稿时间:6 December 2006
修稿时间:2006-12-062007-04-13

Single grain Rb-Sr dating of euhedral and cataclastic pyrite from the Qiyugou gold deposit in western Henan,central China
HAN YiGui LI XiangHui ZHANG ShiHong ZHANG YuanHou CHEN FuKun.Single grain Rb-Sr dating of euhedral and cataclastic pyrite from the Qiyugou gold deposit in western Henan, central China[J].Chinese Science Bulletin,2007,52(13):1820-1826.
Authors:Han YiGui  Li XiangHui  Zhang ShiHong  Zhang YuanHou  Chen FuKun
Institution:(1) State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing, 100083, China;(2) Laboratory for Radiogenic Isotope Geochemistry, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China;(3) The College of Earth Sciences, Jilin University, Changchun, 130061, China
Abstract:The Rb-Sr isotopic dating of pyrite mineral from ore deposits can directly provide mineralization age. However, many geological factors may affect the Rb-Sr isotopic system, which baffles application of this method. Employing ultra-low procedural blank Rb-Sr method, we have dated pyrites separated from the No. 4 breccia pipe of the Qiyugou gold deposit, western Henan Province. Single grains of euhedral pyrite crystal with few micro-cracks yield an isochron age of 126 ± 11 Ma, which represents time of the main mineralization stage of the deposit. Pyrite grains of cataclastic type show nevertheless scattered Rb-Sr isotopic composition and no reasonable isochron can be defined. Crystal morphology and mineral inclusion studies reveal that Rb and Sr of pyrite mineral probably are preserved mainly in biotite, K-feldspar, and sericite mineral inclusions. The dating results likely suggest that cataclastic pyrite is not suitable for the Rb-Sr dating due to modification of the Rb-Sr isotopic system by later hydrothermal activity of fluid. Supported jointly by the National Natural Science Foundation of China (Grant No. 40032010-B) and the National Basic Research Program of China (Grant No. 2006CB403505)
Keywords:pyrite  Rb-Sr dating  single grain  ultra-low procedural blank  Qiyugou
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