Channel-form Structures

Channel-Form Structures is a sedimentary structure characterized by a three-dimensional, concave-upward geometry formed by the erosional and depositional processes within a confined flow pathway, distinguishing it from other sedimentary structures by its association with fluvial, tidal, or density-driven current systems and its role in indicating paleoflow direction and sediment transport mechanisms.

189

Publications

10.7K

Citations

680

Authors

311

Institutions

Publications per year

2017–2026

35

Variants

Channel-form Sedimentary Structures

Authors

680

  1. KP
    K.T. Pickering

    University College London, United Kingdom

    3 publications · 143 citations

    3

    h-index

  2. EH
    Emily H. Stanley

    University of Wisconsin–Madison, United States

    3 publications · 301 citations

    3

    h-index

  3. VR
    Victor R. Baker

    University of Arizona, United States

    3 publications · 139 citations

    3

    h-index

  4. BK
    Ben Kneller

    University of Aberdeen, United Kingdom

    3 publications · 238 citations

    3

    h-index

  5. TK
    Takayoshi Kuroda‐Sowa

    Kindai University, Japan

    2 publications · 223 citations

    2

    h-index

1–5 of 680

Venues

  1. Marine and Petroleum Geology

    8 publications · 411 citations

    8

    h-index

  2. Earth Surface Processes and Landforms

    7 publications · 347 citations

    7

    h-index

  3. Geomorphology

    6 publications · 280 citations

    6

    h-index

  4. Crystal Growth & Design

    6 publications · 255 citations

    6

    h-index

  5. Journal of Sedimentary Research

    JSR · 5 publications · 321 citations

    5

    h-index

1–5