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《Journal of Palaeogeography》 2012-06
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Geochemical characteristics of trace elements in limestone of the Neoproterozoic Wangshan Formation in northern Anhui Province

Chen Song1,2 Fu Xuehai1,3 Gui Herong2 Sun Linhua2 1 The School of Resource and Earth Science,China University of Mining and Technology,Xuzhou221116,Jiangsu 2 School of Earth Sciences and Engineering,Suzhou University,Suzhou234000,Anhui 3 College of Geology and Exploration Engineering,Xinjiang University,rümqi830046,Xinjiang  
To understand the geochemical characteristics of limestone from the Neoproterozoic Wangshan Formation and its geological background, petrological and trace elemental analyses had been carried out for the limestone collected from the Neoproterozoic Wangshan Formation in northern Anhui Province.The results showed that: the elements of U,Pb,Sr,Sm in the limestone are rich,while Nb,Pr,Zr,Hf are poor; the REE in limestone from the Wangshan Formation are characterized by the lower total REE(6.68~42.78 μg/g),light LREE depletion(NdSN/YbSN=0.65~0.91),slight fractionation between LREE and HREE,and various degree in positive La and Y anomaly.It can be inferred that the ancient seawater is anoxic and high salinity,and the palaeoclimate is drought by the information from U,Th,V,Sr/Ba and Sr/Cu,respectively.The limestone from the Wangshan Formation might be deposited in the continental arc environment indicated by diagrams of the La-Th-Sc and Th-Sc-Zr/10.
【Fund】: 国家自然科学基金项目(编号:40873015);; 安徽省教育厅自然科学项目(编号:KJ2011B177);; 宿州学院科研平台开放课题(编号:2011YKF22)共同资助
【CateGory Index】: P595
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