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《Journal of Hefei University of Technology(Natural Science)》 2010-01
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Discovery of the Neo-Proterozoic siliceous limestone in northern Anhui Province and its geological significance

SUN Lin-hua1,GUI He-rong1,HE Zhen-yu2,CHEN Song1,MA Yan-ping1(1.Dept.of Geographical and Environmental Sciences,Suzhou University,Suzhou 234000,China;2.Dept.of Earth Sciences,Nanjing University,Nanjing 210093,China)  
Siliceous limestone has been found in the Niyuan Formation formed in Neo-Proterozoic in northern Anhui Province.It is mainly composed of calcite(90%) and quartz(10%),and distributed as white cumulate mass in the country rock that is composed of lime-dolomite and limestone.The siliceous limestone is characterized by high CaO(85.34%) and SiO2(13.61%) contents.The HREE and LREE are strictly fractionated and the total REE content is low.It is characterized by evident positive Eu and weak positive Ce anomalies,high Tb/Yb ratio and low Th/Sc ratio,high Ba and(Cu+Pb+Zn) contents and low Al/(Al+Fe+Mn) ratio,indicating that it is precipitated from the mixing of the hydrothermal solution and sea water.In view of previous work,it is considered that the tectonic background in the Neo-Proterozoic of the northern Anhui Province is a young back-arc basin,which was formed during the Grenville orogen in response to the convergence of the Rodinia super continent,rather than the positive continental margin during the breakup of the Rodinia super continent that was presented by previous study.
【Fund】: 安徽省高校优秀青年人才基金资助项目(2010SQRL190);; 宿州学院教授(博士)科研启动基金资助项目(2009jb04)
【CateGory Index】: P588;P542
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10 YANG Jie dong 1)2) , ZHENG Wen wu 2) , WANG Zong zhe 4) and TAO Xian cong 1) ( 1) Center of Modern Analysis, Nanjing University, Nanjing, 210093; 2) State Key Laboratory of Mineralizing Processes of Ore Deposits, Nanjing Unive;AGE DETERMINING OF THE UPPE PRECAMBRIAN SYSTEM OF NORTHERN JIANGSU-ANHUI BY USING Sr AND C ISOTOPES[J];Journal of Stratigraphy;2001-01
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