Point Bar Sedimentation

Point Bar Sedimentation is a fluvial depositional process in which lateral accretion of sediment occurs along the inner bend of a meandering river channel due to reduced flow velocity and centrifugal redistribution of bedload, forming a characteristic asymmetric, fining-upward sedimentary sequence.

49

Publications

3.4K

Citations

98

Authors

55

Institutions

Publications per year

2017–2026

9

Authors

98

  1. SM
    Stephen M. Hubbard

    University of Calgary, Canada

    5 publications · 284 citations

    5

    h-index

  2. JB
    John Bridge

    Binghamton University, United States

    4 publications · 405 citations

    4

    h-index

  3. MG
    Massimiliano Ghinassi

    University of Padua, Italy

    3 publications · 210 citations

    3

    h-index

  4. PR
    Paul R. Durkin

    University of Calgary, Canada

    3 publications · 106 citations

    3

    h-index

  5. YS
    Yi Su

    Institute of High Performance Computing, Singapore

    2 publications · 58 citations

    2

    h-index

1–5 of 98

Venues

  1. Sedimentology

    10 publications · 994 citations

    10

    h-index

  2. Sedimentary Geology

    5 publications · 904 citations

    5

    h-index

  3. Journal of Sedimentary Research

    JSR · 3 publications · 228 citations

    3

    h-index

  4. Canadian Journal of Earth Sciences

    3 publications · 157 citations

    3

    h-index

  5. Earth Surface Processes and Landforms

    2 publications · 109 citations

    2

    h-index

1–5