Holocene Alluviation
Holocene Alluviation is a geomorphological process denoting the deposition of sediments by flowing water during the Holocene epoch, distinguished from other alluvial processes by its strict temporal confinement to the post-Pleistocene period and its association with climatically and anthropogenically influenced fluvial systems.
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Fluvial landscapes of the Harappan civilization
Liviu Giosan, Peter D. Clift, Mark G. Macklin et al. · Proceedings of the National Academy of Sciences · 2012 · 327 citations · Full text
Chenglong Deng, Rixiang Zhu, Mike Jackson et al. · Physics and Chemistry of the Earth Part A Solid Earth and Geodesy · 2001 · 222 citations
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Centre National de la Recherche Scientifique
Paris, France
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119 publications
5.6K citations
United States Geological Survey
Reston, United States
20 h-index
42 publications
1.5K citations

Chinese Academy of Sciences
Beijing, China
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67 publications
2.3K citations
University College London
London, United Kingdom
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16 publications
1.5K citations

Consejo Nacional de Investigaciones Científicas y Técnicas
Buenos Aires, Argentina
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48 publications
1.5K citations

Newcastle University
Newcastle upon Tyne, United Kingdom
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19 publications
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Aberystwyth University
Aberystwyth, United Kingdom
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Institut de Recherche pour le Développement
Marseille, France
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