Quaternary loess deposit of China is brought by wind force from the origin area to the deposit area in the arid climate condition.
我国第四纪以来的风成黄土堆积是在干旱的气候条件下由风力作用带到其他地区堆积的沉积物质。
参考来源 - 长江三峡地区第四纪沉积物质来源及其沉积环境意义的探讨·2,447,543篇论文数据，部分数据来源于NoteExpress
The environmental changes inferred from the loess deposit are in well comparison with the lacustrine records.
黄土和湖泊沉积记录的环境变化过程具有可比性。
Most loess is considered to be an eolian deposit.
大多数黄土被认为是一种风成沉积。
The oldest aeolian deposit on terrace T2 is loess L1, corresponding to oxygen isotope time MIS2.
T2阶地上覆的最老风尘沉积是黄土l1，对应氧同位素期MIS 2。
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