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《Acta Sedimentologica Sinica》 2007-04
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REE Characteristics and Its Geological Significance of the Permo-Carboniferous in Bohaiwan Basin

LI Jun1 SANG Shu-xun1 LIN Hui-xi2 CHEN Shi-yue 3 MIAO Yao 1 YANG Yong 1(1.School of Resource and Geoscience,China University of Mining and Technology,Xuzhou Jiangsu 221008;2.Geological Science Research Institute of Shengli oilfield Company Ltd.,SINOPEC,Dongying Shandong 257015;3.School of Earth and Information Science,China University of Petroleum,Dongying Shandong 257000)  
An ICP-MS method is used to determine the contents of rare earth elements of Carboniferous and Permian sedimentary rocks in Bohaiwan Basin.The average REE content of every sample is 290.39 μg/g,and it is obvious higher than the North American shale sample.The δEu is 0.42-0.83,and the average is 0.67,and the samples are lack of Eu.Most samples content nomal Ce,and δCe is 0.51-1.22,and the average is 0.97.The rare earth element patterns indicate that the LREE is rich and the HREE is lack,and the HREE patterns are flat.The lack of Ce indicates the ancient water of the upper Carboniferous is oxidable.According to the values of δEu and the REE content and its variation,the material source of Carboniferous and Permian in Bohaiwan Basin was from the Yinshan ancient continent and its province is granite.
【Fund】: 国家重点基础研究发展规划项目(2002CB211703)资助;; 国家油气专项(XQ-2004-03)资助
【CateGory Index】: P595;P534.46
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