Pressure Solution
Pressure Solution is a deformation mechanism in structural geology wherein minerals dissolve at grain contacts under differential stress, with the solute transported by pore fluids, distinguished from other brittle or ductile mechanisms by its dependence on chemical processes and stress-induced solubility gradients.
439
Publications
27.8K
Citations
810
Authors
342
Institutions
Publications per year
2017–2026
57
Variants
Dissolution CreepPressure Solution Creep
Parents
439
1–5 of 439
810
28
h-index
19
h-index
Centre National de la Recherche Scientifique, France
16 publications · 1.4K citations
15
h-index
12
h-index
10
h-index
1–5 of 810
342
Utrecht University
Utrecht, The Netherlands
29 h-index
39 publications
3.1K citations

Centre National de la Recherche Scientifique
Paris, France
22 h-index
29 publications
1.9K citations

Université Joseph Fourier
Grenoble, France
18 h-index
20 publications
1.7K citations

University of Oslo
Oslo, Norway
16 h-index
16 publications
1.2K citations

Pennsylvania State University
State College, United States
13 h-index
15 publications
1.2K citations
Shell (Netherlands)
The Hague, The Netherlands
11 h-index
11 publications
800 citations
Stanford University
Stanford, United States
10 h-index
10 publications
845 citations

University of Liverpool
Liverpool, United Kingdom
10 h-index
10 publications
748 citations
1–8 of 342
JGR · 44 publications · 3.9K citations
33
h-index
JSR · 33 publications · 1.8K citations
24
h-index
21 publications · 1.7K citations
18
h-index
23 publications · 1.3K citations
17
h-index
21 publications · 1.6K citations
17
h-index
1–5