我国第四纪风成沉积物研究进展  

Research Progress of Quaternary Aeolian Sediments in China

作　　者：沈小晓 Shen Xiaoxiao(College of Land Resources,Xihua Normal University,Nanchong,Sichuan 637002,China)

机构地区：[1]西华师范大学国土资源学院,四川南充637002

出　　处：《绿色科技》2018年第16期235-236,共2页Journal of Green Science and Technology

摘　　要：指出了中国第四纪风成沉积物分布广泛,现在已经被广泛研究并取得丰硕成果的主要有北方黄土高原黄土、长江中下游下蜀黄土、成都平原的成都黏土、岷江上游干旱河谷土壤等。综述了学者对其物源、成因、形成年代等特征进行的广泛研究并取得的丰硕成果。China＇s Quaternary eolian sediments are widely distributed. Now there have been extensive researches and achieved fruitful results in loess plateau loess in the north, lower loess in the middle and lower reaches of the Yangtze River, Chengdu clay in the Chengdu Plain, and dry valley soil in the upper reaches of the Minjiang River. Scholars have conducted extensive research on their source, origin and age of formation and have achieved fruitful results.

关 键 词：第四系 风成沉积物 成因 物源 

分 类 号：P533[天文地球—古生物学与地层学]