...暴 黄土堆积 [gap=1251]klimakan Desert,aeolian accumulation landform,atmospheric circulation,duststorm,loess accumulation ...
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新近堆积黄土 recently deposited loess
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Based on detailed field investigation, we choose Jiangyang village and Huxizhuang village two sections as typical of loess accumulation and paleoflood sediment in Fufeng and Wugong of Zhouyuan area.
本研究基于详细的野外考察,分别在周原地区的扶风县和武功县选择了典型黄土堆积的匠杨村剖面和夹有古洪水沉积物的浒西庄剖面。
参考来源 - 周原地区全新世河流古洪水沉积与风成黄土的对比研究·2,447,543篇论文数据，部分数据来源于NoteExpress
谷风产生的大片类黄土堆积与滑坡体共同参与泥石流的形成；
Under the influence of the gully wind, there is filled with lots of wind accumulated deposit which triggers the form of debris flow with landslides;
这一时期夏季风减弱，冬季风增强，风成黄土堆积，降水减少。
Summer monsoon was weaker and winter monsoon stronger. Precipitation decreased, and eolian dust deposition was accelerated.
这种相关性与顶部的黄土堆积刚好相反，反映了二者之间磁化率不同的变化机制。
This correlation is contrast to the loess deposits on top of profile, which shows the mechanism of magnetic response towards paleoclimate changes in lacustrine sediments is unlike that in loess.
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