Clinoform Development

Clinoform Development is a stratigraphic process in deltaic sedimentation characterized by the progressive seaward progradation, aggradation, and lateral spreading of sedimentary deposits that form a distinctive clinoform geometry defined by a convex-upward bedslope transitioning from subaerial to subaqueous environments.

61

Publications

4.4K

Citations

190

Authors

119

Institutions

Publications per year

2017–2026

20

Authors

190

  1. RJ
    Ronald J. Steel

    The University of Texas at Austin, United States

    9 publications · 558 citations

    9

    h-index

  2. CO
    Cornel Olariu

    The University of Texas at Austin, United States

    4 publications · 155 citations

    4

    h-index

  3. AS
    A. S. Ogston

    University of Washington, United States

    4 publications · 328 citations

    4

    h-index

  4. DM
    David M. Hodgson

    University of Leeds, United Kingdom

    3 publications · 136 citations

    3

    h-index

  5. SS
    Stephen S. Flint

    University of Liverpool, United Kingdom

    3 publications · 136 citations

    3

    h-index

1–5 of 190

Venues

  1. Basin Research

    16 publications · 771 citations

    15

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  2. Marine Geology

    5 publications · 683 citations

    5

    h-index

  3. Continental Shelf Research

    4 publications · 846 citations

    4

    h-index

  4. Journal of Sedimentary Research

    JSR · 4 publications · 335 citations

    4

    h-index

  5. Sedimentology

    4 publications · 135 citations

    4

    h-index

1–5