Chinese Loess Paleosol sediments were just controlled by both the factors of glacial interglacial and paleomonsoon climate.

中国黄土—古土壤堆积是全球冰期—间冰期气候变化与东亚古季风气候变化共同作用的结果。

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Micron grade magnetic minerals are less than 1%of total minerals in the loess paleosol sequences. To satisfy requirements of a lot of kind of measurement, it needs to enrich the magnetic minerals.

微米级磁性矿物在黄土-古土壤序列中含量不足1%，为了满足多种测试的需要，要尽可能地富集磁性矿物。

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Based on detailed rock magnetic analyses of loess-paleosol sequence at Chaona section in the central loess Plateau, a high-resolution environmental magnetic framework has been built up for last 1.

通过对黄土高原中部朝那剖面黄土-古土壤序列系统的岩石磁学分析，建立了1。

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