Oblique Faulting
Oblique Faulting is a type of lithospheric deformation characterized by fault displacement that occurs at an angle to both the dip and strike directions of the fault plane, involving simultaneous normal or reverse and strike-slip shear components, thereby distinguishing it from purely dip-slip or strike-slip faulting mechanisms.
105
Publications
8.8K
Citations
365
Authors
169
Institutions
Publications per year
2017–2026
19
Variants
Oblique-slip Faulting
Parents
105
The Mechanics of Oblique Slip Faulting
M. H. P. Bott · Geological Magazine · 1959 · 1.2K citations
1–5 of 105
365
3
h-index
3
h-index
2
h-index
2
h-index
2
h-index
1–5 of 365
169
United States Geological Survey
Reston, United States
10 h-index
34 publications
1.2K citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
13 publications
1.8K citations
Planetary Science Institute
Tucson, United States
4 h-index
9 publications
3.1K citations
Stanford University
Stanford, United States
4 h-index
5 publications
301 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
3 h-index
4 publications
313 citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
3 h-index
14 publications
412 citations

Institut de physique du globe de Paris
Paris, France
3 h-index
6 publications
1.5K citations

Uppsala University
Uppsala, Sweden
3 h-index
3 publications
128 citations
1–8 of 169
9 publications · 591 citations
9
h-index
7 publications · 400 citations
7
h-index
6 publications · 604 citations
6
h-index
6 publications · 194 citations
6
h-index
JGR · 6 publications · 1.4K citations
6
h-index
1–5