In the Pearl River Basin, except for the Hongshui reach of the upper reaches of the Xijiang River, the grain size change, CIA and REE of the main stream of the Xijiang River from the upper reaches to the lower reaches all show obvious gradual changes, and the overall CIA is increasing from the upper reaches to the lower reaches. The CIA in the upper reaches of Hongshui River is in the range of moderate weathering, and the fine-grained sediments in the lower reaches have experienced stronger chemical weathering than those in the upper reaches
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