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In this study Chengdu Red Earth (CRE) from the Chengdu Plain (CP), Sichuan province, was analyzed for its elemental (major and trace elements) and isotopic (Sm‐Nd) geochemistry and compared with Pleistocene loess and paleosol samples from the Chinese Loess Plateau (CLP) in Northern China. The geochemical composition of CRE is similar to north China loess, and also resembles the average UCC. This indicates...
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