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.

806

Publications

34.5K

Citations

2.8K

Authors

1.1K

Institutions

Publications per year

2017–2026

116

Authors

2.8K

  1. MG
    Mark G. Macklin

    Aberystwyth University, United Kingdom

    14 publications · 1.1K citations

    14

    h-index

  2. CC
    Chun Chang Huang

    Shaanxi Normal University, China

    8 publications · 273 citations

    8

    h-index

  3. JA
    John A. Matthews

    Swansea University, United Kingdom

    8 publications · 322 citations

    8

    h-index

  4. JJ
    John J. Clague

    Simon Fraser University, Canada

    7 publications · 218 citations

    7

    h-index

  5. JP
    Jiangli Pang

    Shaanxi Normal University, China

    7 publications · 230 citations

    7

    h-index

1–5 of 2.8K

Venues

  1. Quaternary Science Reviews

    55 publications · 3.8K citations

    36

    h-index

  2. Quaternary International

    73 publications · 2.6K citations

    30

    h-index

  3. Palaeogeography Palaeoclimatology Palaeoecology

    43 publications · 2.8K citations

    29

    h-index

  4. Geomorphology

    33 publications · 1.5K citations

    23

    h-index

  5. Marine Geology

    26 publications · 965 citations

    21

    h-index

1–5