Thermal Contraction Cracking

Thermal Contraction Cracking is a geological deformation process in which tensile fractures form on planetary surfaces due to the volumetric shrinkage of materials undergoing cooling, distinguishing it from other fracturing mechanisms by its dependence on thermal stress cycles in the absence of tectonic or impact forcing.

136

Publications

6.7K

Citations

455

Authors

190

Institutions

Publications per year

2017–2026

28

Authors

455

  1. JW
    J. W. Head

    Brown University, United States

    7 publications · 629 citations

    7

    h-index

  2. JS
    J. S. Levy

    The University of Texas at Austin, United States

    6 publications · 583 citations

    6

    h-index

  3. DR
    D. R. Marchant

    Boston University, United States

    6 publications · 389 citations

    6

    h-index

  4. PB
    Pascal Bertran

    Institut National de Recherches Archéologiques Préventives, France

    4 publications · 226 citations

    4

    h-index

  5. SM
    Seyed Mojtaba Sadrameli

    Tarbiat Modares University, Iran

    4 publications · 276 citations

    4

    h-index

1–5 of 455

Venues

  1. Fuel

    9 publications · 457 citations

    9

    h-index

  2. Permafrost and Periglacial Processes

    7 publications · 403 citations

    7

    h-index

  3. Journal of Analytical and Applied Pyrolysis

    6 publications · 302 citations

    6

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  4. Fuel Processing Technology

    5 publications · 292 citations

    5

    h-index

  5. Canadian Journal of Earth Sciences

    5 publications · 400 citations

    5

    h-index

1–5