Dissolution Creep
Dissolution Creep is a deformation mechanism in which mineral grains deform through the dissolution of material at grain contacts under stress, followed by diffusive or advective mass transfer and reprecipitation in pore spaces, distinguished from other creep processes by its dependence on chemical solubility and fluid-mediated mass transport.
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85
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2017–2026
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Centre National de la Recherche Scientifique
Paris, France
5 h-index
5 publications
189 citations
Indiana University Bloomington
Bloomington, United States
4 h-index
4 publications
276 citations
Ruhr University Bochum
Bochum, Germany
4 h-index
4 publications
253 citations
Johannes Gutenberg University Mainz
Mainz, Germany
2 h-index
2 publications
387 citations
Utrecht University
Utrecht, The Netherlands
2 h-index
2 publications
214 citations
University of Münster
Münster, Germany
2 h-index
2 publications
144 citations

Monash University
Melbourne, Australia
2 h-index
2 publications
94 citations
Institut des Sciences de la Terre d'Orléans
Orléans, France
2 h-index
2 publications
86 citations
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9 publications · 672 citations
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6 publications · 206 citations
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JGR · 2 publications · 90 citations
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