Terrestrial Sedimentation
Terrestrial Sedimentation is the process of deposition and accumulation of detrital materials transported and laid down by subaerial agents such as wind, water, or gravity on continental surfaces, distinguished from marine or lacustrine sedimentation by its exclusive occurrence in non-marine, land-based environments.
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228
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129
Institutions
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2017–2026
7
Variants
Continental Sedimentation
Parents
56
Loess Plateau storage of Northeastern Tibetan Plateau-derived Yellow River sediment
Junsheng Nie, Thomas Stevens, Martin Rittner et al. · Nature Communications · 2015 · 419 citations · Full text
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129

Centre National de la Recherche Scientifique
Paris, France
3 h-index
5 publications
324 citations
ETH Zurich
Zurich, Switzerland
3 h-index
13 publications
1.1K citations
Laboratoire de Géographie Physique
Thiais, France
2 h-index
2 publications
108 citations
The University of Texas at Austin
Austin, United States
2 h-index
3 publications
914 citations
University of Potsdam
Potsdam, Germany
2 h-index
2 publications
123 citations
University of New Mexico
Albuquerque, United States
2 h-index
3 publications
245 citations

Uppsala University
Uppsala, Sweden
2 h-index
7 publications
491 citations
University of California, Merced
Merced, United States
2 h-index
2 publications
519 citations
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3 publications · 620 citations
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JSR · 2 publications · 41 citations
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2 publications · 773 citations
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2 publications · 78 citations
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2 publications · 238 citations
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