This paper explain the results and suggests that the upper part of the section is normal loess/paleosol series, while the lower part is redeposited loess and paleosols.
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- 结合该剖面的岩石磁学性质与该区域其他剖面以及洛川剖面的对比,本文的解释是该剖面上部为正常的黄土古土壤序列,而底部为再搬运沉积的黄土古土壤。