Oceanic Transform Faults
Oceanic Transform Fault is a type of strike-slip fault that forms part of a transform plate boundary system in oceanic crust, distinguished by its orthogonal linkage of offset mid-ocean ridge segments and its role in accommodating lateral displacement between adjacent tectonic plates.
460
Publications
39.2K
Citations
1.1K
Authors
421
Institutions
Publications per year
2017–2026
73
Variants
Oceanic Transform Fault
460
Charles DeMets, Richard G. Gordon, Donald F. Argus et al. · Geophysical Journal International · 1990 · 3.7K citations · Full text
J. B. Minster, T. H. Jordan · Journal of Geophysical Research Atmospheres · 1978 · 2.3K citations · Full text
S. H. Kirby · Reviews of Geophysics · 1983 · 792 citations
1–5 of 460
1.1K
University of California, Santa Barbara, United States
11 publications · 1K citations
11
h-index
9
h-index
9
h-index
8
h-index
GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany
8 publications · 271 citations
8
h-index
1–5 of 1.1K
421
Woods Hole Oceanographic Institution
Falmouth, United States
26 h-index
67 publications
5.7K citations

Centre National de la Recherche Scientifique
Paris, France
21 h-index
78 publications
2.8K citations

Scripps Institution of Oceanography
La Jolla, United States
18 h-index
45 publications
5.1K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
15 h-index
35 publications
4.4K citations

Institut de physique du globe de Paris
Paris, France
15 h-index
36 publications
1.5K citations
University of California San Diego
San Diego, United States
14 h-index
27 publications
2.3K citations

GEOMAR Helmholtz Centre for Ocean Research Kiel
Kiel, Germany
14 h-index
50 publications
2K citations
Massachusetts Institute of Technology
Cambridge, United States
13 h-index
19 publications
2.1K citations
1–8 of 421
JGR · 87 publications · 10.4K citations
53
h-index
GJI · 29 publications · 6.6K citations
26
h-index
25 publications · 1.8K citations
21
h-index
25 publications · 993 citations
21
h-index
27 publications · 1.3K citations
20
h-index
1–5