Surface Wave Anisotropy is a geophysical observable within the broader class of seismic anisotropy phenomena, distinguished by its manifestation in the directional dependence of surface wave propagation velocities arising from azimuthally anisotropic crustal and upper mantle structures.
119
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2017–2026
25
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119
1–5 of 119
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270
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9
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3
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3
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155
Centre National de la Recherche Scientifique
Paris, France
9 h-index
18 publications
1.4K citations
Utrecht University
Utrecht, The Netherlands
8 h-index
13 publications
776 citations
Institut de physique du globe de Paris
Paris, France
8 h-index
13 publications
639 citations
Lamont-Doherty Earth Observatory
Sparkill, United States
5 h-index
11 publications
346 citations
Columbia University
New York, United States
5 h-index
11 publications
346 citations
University of Colorado Boulder
Boulder, United States
5 h-index
13 publications
412 citations
China Earthquake Administration
Beijing, China
5 h-index
7 publications
144 citations
Massachusetts Institute of Technology
Cambridge, United States
4 h-index
7 publications
699 citations
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- Geophysical Journal International
GJI · 20 publications · 923 citations
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- Physics of The Earth and Planetary Interiors
9 publications · 498 citations
9
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- Journal of Geophysical Research Atmospheres
JGR · 8 publications · 716 citations
8
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- Journal of Geophysical Research Solid Earth
8 publications · 348 citations
8
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- Geophysical Research Letters
7 publications · 418 citations
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