ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
蓟县中元古代高于庄组凝灰岩锆石LA-MC-ICPMS U-Pb定年及其地质意义
  
关键词:tuff bed  Gaoyuzhuang Formation  LA-MC-ICPMS U-Pb dating  Calymmian System  Jixian  North China Craton
基金项目:中国地质调查局项目(编号: 12120113013900; 1212011120142);国家自然科学基金项目(编号: 41430210; 41272046);科技部科技基础性工作专项(编号: 2015FY310100)
作者单位E-mail
田辉 中国地质调查局天津地质矿产研究所 309702629@qq.com 
张健 中国地质调查局天津地质矿产研究所 huaikunli@sina.com 
李怀坤 中国地质调查局天津地质矿产研究所  
苏文博 中国地质大学(北京)地球科学与资源学院  
周红英 中国地质调查局天津地质矿产研究所  
杨立公 天津市蓟县中上元古界国家自然保护区管理中心  
相振群 中国地质调查局天津地质矿产研究所  
耿建珍 中国地质调查局天津地质矿产研究所  
刘欢 中国地质调查局天津地质矿产研究所  
朱士兴 中国地质调查局天津地质矿产研究所  
许振清 天津市蓟县中上元古界国家自然保护区管理中心  
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摘要:
Zircon LA-MC-ICPMS U-Pb Dating of Tuff from Mesoproterozoic Gaoyuzhuang Formation in Jixian County of North China and Its Geological Significance
      A 15 cm thick tuff intercalation in dolomite was recently discovered in the lower horizon of the third member (the Zhangjiayu Subformaiton) of the Gaoyuzhuang Formation in the Mesoproterozoic Jixian System at the Dongshuichang Village, Jixian County. A zircon U-Pb age of (1577±12) Ma for the tuff was obtained by means of LA-MC-ICPMS method, consequently for the first time providing precise and reliable chronological constraint on the depositional age of the Gaoyuzhuang Formation in the Jixian area and a new correlation marker for Mesoproterozoic strata in the whole Yanshan area of the northern North China Craton. At the same time, abundant macro-alga fossils represented by Parachuaria glabra Sun, the same as those discovered previously in the Mesoproterozoic Standard Section in the Dahongyu Valley, were also found in the dolomite beds directly overlying the newly-discovered tuff beds. Therefore, the newly-obtained tuff age can further provide constraint on the living time of the macro-alga Parachuaria glabra Sun in the Gaoyuzhuang Formation. Combined with the zircon U-Pb age (1560±5) Ma obtained previously for the tuff bed in the top horizon of the third member of the Gaoyuzhuang Formation in Yanqing County, northwestern Beijing, it can be concluded that the depositional age of the third member of the Gaoyuzhuang Formation is in the time span of 1580~1560 Ma, and the boundary between the Gaoyuzhuang Formation and the underlying Dahongyu Formation can be quite confidently placed at 1600 Ma that is equivalent to the lower boundary of the International Mesoproterozoic Calymmian System.
TIAN Hui,ZHANG Jian,LI Huai-kun,SU Wen-bo,ZHOU Hong-ying,YANG Li-gong,XIANG Zhen-qun,GENG Jian-zhen,LIU Huan,ZHU Shi-xing,XU Zhen-qing.2015.Zircon LA-MC-ICPMS U-Pb Dating of Tuff from Mesoproterozoic Gaoyuzhuang Formation in Jixian County of North China and Its Geological Significance[J].Acta Geoscientica Sinica,36(5):647-658.
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