Shear-Wave Anisotropy is a geophysical measurement technique that quantifies the directional dependence of shear-wave splitting in seismological data to infer the presence and orientation of anisotropic structures within the Earth's crust.
653
Publications
40.5K
Citations
1.5K
Authors
501
Institutions
Publications per year
2017–2026
103
Variants
Seismic Shear-wave Anisotropy
Parents
Publications
653
1–5 of 653
Authors
1.5K
- SC
26
h-index
- JM
24
h-index
- MD
23
h-index
- MK
22
h-index
- PG
16
h-index
1–5 of 1.5K
Institutions
501
University of Bristol
Bristol, United Kingdom
25 h-index
56 publications
2.6K citations
Centre National de la Recherche Scientifique
Paris, France
23 h-index
59 publications
4.3K citations
Yale University
New Haven, United States
23 h-index
54 publications
3.5K citations
Carnegie Institution for Science
Washington, United States
22 h-index
42 publications
6K citations
China Earthquake Administration
Beijing, China
21 h-index
79 publications
3K citations
British Geological Survey
Nottingham, United Kingdom
21 h-index
51 publications
3.9K citations
Victoria University of Wellington
Wellington, New Zealand
18 h-index
47 publications
3.3K citations
University of Leeds
Leeds, United Kingdom
17 h-index
31 publications
2.2K citations
1–8 of 501
Venues
- Geophysical Journal International
GJI · 106 publications · 8.2K citations
50
h-index
- Journal of Geophysical Research Atmospheres
JGR · 61 publications · 7.4K citations
45
h-index
- Geophysical Research Letters
107 publications · 5.2K citations
44
h-index
- Journal of Geophysical Research Solid Earth
42 publications · 1.4K citations
26
h-index
- Earth and Planetary Science Letters
29 publications · 1.8K citations
23
h-index
1–5