ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
恒山-五台地区同位素年代学与地质事件演化系列的建立
  
关键词:isotopic age  geological event  Hengsban Complex  Wutai complex
基金项目:本课题得到北京大学重点测试基金的资助。
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牛向龙 北京大学教育部造山带与地壳演化重点实验室北京大学地球与空间科学学院北京100871 xlniuol@pku.org.cn 
李江海 北京大学教育部造山带与地壳演化重点实验室北京大学地球与空间科学学院北京100871  
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摘要:
Geochronology and Geological Event Sequences of Hengshan-Wutai Precambrian Complex
      Statistics of many new isotopic age data show that the peak value of Hengshan complex (2520 Ma) is some 20 Ma younger than that of Wutai complex (2540 Ma).This serves as the evidence that Hengshan complex might be the arc root of Wutai complex. Based on an integrated analysis of various geological records, the authors have divided the evolution of Wutai-Hengshan Precambrian complex into five stages. It is thus inferred that the central arogeny should have taken place between 2.55 and 2.50 Ga in North China craton.
NIU Xianglong,LI Jianghai.2005.Geochronology and Geological Event Sequences of Hengshan-Wutai Precambrian Complex[J].Acta Geoscientica Sinica,26(z1):115-117.
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