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《Geological Journal of China Universities》 2004-02
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Sr and C Isotopic Correlation and the Age Boundary Determination for the Neoproterozoic in the Southern Liaoning and Northern Jiangsu—Northern Anhui Provinces

ZHENG Wen-wu 1,YANG Jie-dong 2,3 ,HONG Tian-qiu 1 TAO Xian-cong 2,WANG Zong-zhe 4 (1.Institute of the Resources and Environment Engineering,Hefei University of Technology,Hefei 230009,China;2.Center of Modern Analysis,Nanjing University,Nanjing 210093,China;3.State Key Laboratory for Mineral Deposits Research,Nanjing University,Nanjing 210093,China;4.Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing 210008,China)  
According to the methods of Sr and C isotopic stratigraphy,limestone samples were systematically collected from the Neoproterozoic successions in northern Jiangsu,northern Anhui and southern Liaoning Provinces. New findings,such as the physical sequences of the strata,the depositional ages,and the choice of the isotopic geochronologic data of the study area,were obtained by comparing the Sr and C isotope compositions with the evolution curves of the Sr and C isotopes for the Neoproterozoic and Cambrian seawater. The findings suggested that the Huainan Group,the Xihe Group and the Wuxingshan Group in the studied regions were all formed 900 Ma to 700 Ma ago,a period before the Nantuo ice period or the Sturtian ice period,and it is proved further that the Huainan Biota should be one important life explosion that belongs to the pre-Ediacaran period.
【Fund】: 国家自然科学基金资助项目 (编号 :4 9872 0 12 ;4 98730 0 4 )
【CateGory Index】: P597.2
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