Loess Deposition
Loess Deposition is a sedimentary process within aeolian geomorphology and Quaternary geology consisting of the accumulation of fine-grained, silt-dominated mineral particles transported and deposited by wind, typically during glacial periods of the Pleistocene, distinguished from other aeolian deposits by its homogeneous, non-stratified structure, high porosity, and origin from glaciofluvial sources.
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Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China
Zhengtang Guo, William F Ruddiman, Qingzhen Hao et al. · Nature · 2002 · 1.8K citations
Dust transport and the question of desert loess formation
Haim Tsoar, Kenneth Pye · Sedimentology · 1987 · 720 citations
Magnetism of Chinese loess deposits
Friedrich Heller · Geophysical Journal International · 1984 · 530 citations · Full text
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Chinese Academy of Sciences
Beijing, China
49 h-index
356 publications
43.7K citations
Institute of Earth Environment
Xi'an, China
38 h-index
150 publications
12K citations
Institute of Geology and Geophysics
Beijing, China
29 h-index
111 publications
28K citations
Nanjing University
Nanjing, China
24 h-index
132 publications
6K citations

Centre National de la Recherche Scientifique
Paris, France
23 h-index
88 publications
7.3K citations
Lanzhou University
Lanzhou, China
22 h-index
125 publications
6K citations
University of Bayreuth
Bayreuth, Germany
22 h-index
39 publications
4.1K citations
University of Chinese Academy of Sciences
Beijing, China
20 h-index
54 publications
1.6K citations
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QR · 48 publications · 3.9K citations
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