风成堆积

辽南的滨海黄土也是我国第四纪风成堆积的重要组成部分，它们是我国第四纪黄土沉积物中的一种独特类型。

Coastal loess in the south of liaoning is an important part of Aeolian accumulation and a unique type of the Quaternary loess deposition .

激光粒度仪测量风成堆积物粒度的实验研究

Study on Experiment of Particle Size of Aeolian Deposits From Laser Diffraction Size Analyzer

风成堆积中不同粒径主要化学元素分布规律的初步研究

A preliminary study on the main chemical elements distributions of the different particles in eolian deposition

安徽宣城地区中晚更新世风成堆积与环境变迁风成堆积中不同粒径主要化学元素分布规律的初步研究

Eolian deposit and environmental change of Middle-Late Pleistocene in xuancheng , anhui province south of the lower reaches of the Changjiang River a preliminary study on the main chemical elements distributions of the different particles in eolian deposition

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。

Quaternary loess deposit of China is brought by wind force from the origin area to the deposit area in the arid climate condition .

对早先确定的典型黄土剖面的磁性地层研究表明风成黄土的堆积开始于Matuyama的下界，约2.6Ma。

The classic loess sections cross CLP indicate that wind-blown loess deposition began close to the base of Matuyama ( 2.6Ma ) .