Quaternary River Evolution
Quaternary River Evolution is a fluvial geomorphology concept denoting the spatiotemporal transformation of river systems during the Quaternary period, distinguished by its focus on the dynamic interplay between climatic fluctuations, tectonic activity, base-level changes, and sediment fluxes in shaping fluvial landscapes over the past 2.58 million years.
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2017–2026
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Pre-Miocene birth of the Yangtze River
Hongbo Zheng, Peter D. Clift, Ping Wang et al. · Proceedings of the National Academy of Sciences · 2013 · 334 citations · Full text
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Chinese Academy of Sciences
Beijing, China
12 h-index
33 publications
2.7K citations
China Earthquake Administration
Beijing, China
9 h-index
22 publications
634 citations
Institute of Geology and Geophysics
Beijing, China
8 h-index
17 publications
1.2K citations
China University of Geosciences
Wuhan, China
8 h-index
36 publications
955 citations
United States Geological Survey
Reston, United States
8 h-index
13 publications
669 citations
Institute of Geology, China Earthquake Administration
Beijing, China
7 h-index
18 publications
476 citations

University of Wollongong
Wollongong, Australia
7 h-index
11 publications
515 citations

Durham University
Durham, United Kingdom
7 h-index
12 publications
353 citations
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