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作 者:XU Fangjian CHEN Shiyue QIU Longwei CAO Yingchang 徐方建;陈世悦;邱隆伟;操应长(School of Geosciences,China University of Petroleum,Qingdao 266555,China;Key Laboratory of Shandong Province for Reservoir Geology,China University of Petroleum,Dongying 257061,China)
机构地区:[1]School of Geosciences,China University of Petroleum,Qingdao 266555,China [2]Key Laboratory of Shandong Province for Reservoir Geology,China University of Petroleum,Dongying 257061,China
出 处:《Journal of Rare Earths》2012年第1期94-96,共3页稀土学报(英文版)
基 金:Project supported by the National Natural Science Foundation of China (41106040);Shandong Provincial Natural Science Foundation,China(ZR2010DL009);Fundamental Research Fund for the Central Universities (10CX04004A);the Doctoral Fund of China University of Petroleum (Y0901036)
摘 要:Several REE data sets were collected in Core DD2 and EC2005 in the inner shelf of East China Sea,Core Y127 in the northern Okinawa Trough,Core NT1,C9247 and C92169 in the south Yellow Sea to check the applicability of the δEuN-ΣREEs model for quantita-tively distinguishing sediments from the Yangtze River and the Yellow River.By comparison,several sediments in cores DD2,EC2005,Y127 are generally in accordance with this model.The cores NT1,C9247 and C92169,which have been influenced by the Yangtze River and the Yellow River together,however,were inconsistent with the δEuN-ΣREEs model.The δEuN-ΣREEs plot and its corresponding regression equation,which could be used to distinguish sediments "intuitively and quantitatively" from the Yangtze River,and the Yellow River should be reconsidered or reassessed.Several REE data sets were collected in Core DD2 and EC2005 in the inner shelf of East China Sea,Core Y127 in the northern Okinawa Trough,Core NT1,C9247 and C92169 in the south Yellow Sea to check the applicability of the δEuN-ΣREEs model for quantita-tively distinguishing sediments from the Yangtze River and the Yellow River.By comparison,several sediments in cores DD2,EC2005,Y127 are generally in accordance with this model.The cores NT1,C9247 and C92169,which have been influenced by the Yangtze River and the Yellow River together,however,were inconsistent with the δEuN-ΣREEs model.The δEuN-ΣREEs plot and its corresponding regression equation,which could be used to distinguish sediments "intuitively and quantitatively" from the Yangtze River,and the Yellow River should be reconsidered or reassessed.
关 键 词:rare earths sediment provenance Yangtze River Yellow River
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