Mud Cracking

Mud Cracking is a geological phenomenon characterized by the formation of polygonal desiccation cracks on the surface of fine-grained sediments due to the evaporation of water, distinguishing it from other types of soil cracking by its occurrence in saturated, cohesive mud deposits under drying conditions.

70

Publications

3.7K

Citations

228

Authors

106

Institutions

Publications per year

2017–2026

25

Authors

228

  1. CV
    Chava Venkatesh

    Vignan's Foundation for Science, Technology & Research, India

    3 publications · 185 citations

    3

    h-index

  2. RN
    Ruben Nerella

    Vignan's Foundation for Science, Technology & Research, India

    3 publications · 185 citations

    3

    h-index

  3. LG
    Lucas Goehring

    Max Planck Institute for Dynamics and Self-Organization, Germany

    2 publications · 204 citations

    2

    h-index

  4. AC
    A.C.F. Cocks

    University of Oxford, United Kingdom

    2 publications · 90 citations

    2

    h-index

  5. EJ
    Edward J. Anthony

    Centre National de la Recherche Scientifique, France

    2 publications · 29 citations

    2

    h-index

1–5 of 228

Venues

  1. Journal of Sedimentary Research

    JSR · 8 publications · 278 citations

    8

    h-index

  2. Journal of Petroleum Science and Engineering

    4 publications · 75 citations

    4

    h-index

  3. Construction and Building Materials

    3 publications · 397 citations

    3

    h-index

  4. Sedimentology

    3 publications · 186 citations

    3

    h-index

  5. American Journal of Science

    2 publications · 56 citations

    2

    h-index

1–5