Low-angle Faults
Low-Angle Faults is a structural geological construct denoting a fracture or shear zone in the Earth's crust where the dip angle relative to the horizontal is less than 30 degrees, distinguished from high-angle faults by its shallow inclination and commonly associated with large-scale crustal extension or compression in marine tectonic settings.
286
Publications
20.9K
Citations
790
Authors
295
Institutions
Publications per year
2017–2026
37
Variants
Low-angle Fault
Parents
286
1–5 of 286
790
Istituto Nazionale di Geofisica e Vulcanologia, Italy
9 publications · 1K citations
9
h-index
7
h-index
5
h-index
5
h-index
5
h-index
1–5 of 790
295

Centre National de la Recherche Scientifique
Paris, France
13 h-index
26 publications
1.6K citations
University of Perugia
Perugia, Italy
12 h-index
21 publications
2.2K citations
United States Geological Survey
Reston, United States
11 h-index
23 publications
1.4K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
11 h-index
18 publications
1.1K citations
Columbia University
New York, United States
11 h-index
18 publications
1.1K citations
University of Oxford
Oxford, United Kingdom
9 h-index
14 publications
2.8K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
9 h-index
39 publications
6K citations

Durham University
Durham, United Kingdom
8 h-index
13 publications
1.4K citations
1–8 of 295
26 publications · 2.9K citations
23
h-index
23 publications · 1.5K citations
19
h-index
JGS · 22 publications · 1.8K citations
18
h-index
19 publications · 1.7K citations
17
h-index
16 publications · 1.1K citations
15
h-index
1–5