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庐山筲箕洼组与星子岩群年代地层关系及SHRIMP锆石U-Pb年龄的制约
  
关键词:Shaojiwa Formation  Xingzi Complex Group  zircon SHRIMP dating  Jiangnan orogen  northeastern Jiangxi
基金项目:中国地质调查局地质大调查项目“中国新元古代年代地层格架及其全球对比”(编号: 121201011120131);科技部科技基础性工作专项“中国地质志欧亚大陆大地构造图编制”(编号: 2011FY120100)
作者单位E-mail
高林志 中国地质科学院地质研究所 gaolzh@cags.net.cn 
黄志忠 江西省地质调查研究院  
丁孝忠 中国地质科学院地质研究所  
刘燕学 中国地质科学院地质研究所  
张传恒 中国地质大学(北京)  
王自强 中国地质大学(北京)  
庞健峰 中国地质科学院地质研究所  
韩坤英 中国地质科学院地质研究所  
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摘要:
The Geochronological Relationship between the Shaojiwa Formation and the Xingzi Complex Group in Northwestern Jiangxi and the Constraints on Zircon SHRIMP U-Pb Age
      Ages of (840±6) Ma (MSWD=1.3), (833±4) Ma (MSWD=1.4) and (831±3) Ma (MSWD =1.47) were obtained for spilite and rhyolite from the Shaojiwa Formation. The Xingzi Complex Group has the age of 206Pb/238U (825±5) Ma (MSWD =0.46). In combination of the SHRIMP U-Pb dating of the spilite and rhyolite of the Shaojiwa Formation in the Jiangnan oregen, the authors have determined for the first time that the Xingzi Complex Group is of Neoproterozoic period and lies below the Shaojiwa Formation. These isotopic data from the Shaojiwa Formation are very important for regional correlation of the strata of the corresponding period and tectonic evolution. The zircon U-Pb ages mentioned above determine that Neoproterozoic strata around the age of 820 Ma are developed in northwestern Jiangxi Province. These data contribute to the stratigraphic subdivision and correlation of the metamorphosed rocks in whole Jiangnan old land and help geologists investigate the geological background and ore-forming conditions of the Jiangnan Orogen.
GAO Lin-zhi,HUANG Zhi-zhong,DING Xiao-zhong,LIU Yan-xue,ZHANG Chuan-heng,WANG Zi-qiang,PANG Jian-feng,HAN Kun-ying.2012.The Geochronological Relationship between the Shaojiwa Formation and the Xingzi Complex Group in Northwestern Jiangxi and the Constraints on Zircon SHRIMP U-Pb Age[J].Acta Geoscientica Sinica,33(3):295-304.
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