摘要
Based on borehole logging, sediment sampling and analysis, the authors systematically evaluated the REE distribution characteristics of the sediment from different boreholes in Yongding River catchment and Chaobai River catchment of Beijing Plain. The results show that ∑REE, LREE/HREE, (La/Sm)N, and (Gd/Yb)N of sediments have significant differences between Yongding River catchment and Chaobai River catchment. REE characteristics were generally controlled by grain size of sediments. The chondrite-normalized REE patterns show LREE enrichment and weak Eu negative anomaly. The (La/Yb)N of fine fraction is a good indicator for provenance identification.