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
136
1–5 of 136
455
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Institut National de Recherches Archéologiques Préventives, France
4 publications · 226 citations
4
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4
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1–5 of 455
190
Brown University
Providence, United States
8 h-index
13 publications
1.2K citations

Centre National de la Recherche Scientifique
Paris, France
7 h-index
25 publications
1.4K citations
Boston University
Boston, United States
7 h-index
10 publications
762 citations

Tarbiat Modares University
Tehran, Iran
5 h-index
10 publications
412 citations
Geological Survey of Canada
Ottawa, Canada
4 h-index
7 publications
322 citations
Université de Bordeaux
Bordeaux, France
4 h-index
8 publications
509 citations
Institut National de Recherches Archéologiques Préventives
Metz, France
4 h-index
8 publications
574 citations

Carleton University
Ottawa, Canada
4 h-index
7 publications
640 citations
1–8 of 190
9 publications · 457 citations
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7 publications · 403 citations
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6 publications · 302 citations
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5 publications · 292 citations
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5 publications · 400 citations
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