Point Bar Formation is a fluvial geomorphic process that constitutes a sedimentary deposit feature, distinguished by the lateral accretion of alluvium on the inner bend of a meandering river channel due to reduced flow velocity and enhanced deposition relative to the outer, erosional bank.
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A Simulation Model for Meandering Rivers
Tao Sun, Paul Meakin, Torstein Jøssang et al. · Water Resources Research · 1996 · 276 citations
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University of Calgary
Calgary, Canada
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University of Padua
Padua, Italy
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China University of Petroleum, Beijing
Beijing, China
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Research Institute of Petroleum Exploration and Development
Beijing, China
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University of Leeds
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China National Petroleum Corporation (China)
Beijing, China
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Binghamton University
Binghamton, United States
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