Finite-frequency Effects
Finite-Frequency Effects is a seismic wave propagation phenomenon that accounts for the non-instantaneous sensitivity of seismic measurements to medium properties around the infinite-frequency ray path, incorporating wavefront healing, diffraction, and interference through a frequency-dependent sensitivity kernel.
321
Publications
18.6K
Citations
790
Authors
398
Institutions
Publications per year
2017–2026
51
Parents
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790
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398

Centre National de la Recherche Scientifique
Paris, France
15 h-index
49 publications
2.6K citations
Princeton University
Princeton, United States
13 h-index
29 publications
2.5K citations

Northeastern University
Shenyang, China
9 h-index
17 publications
1K citations
Utrecht University
Utrecht, The Netherlands
8 h-index
15 publications
971 citations
The University of Tokyo
Tokyo, Japan
6 h-index
20 publications
3.2K citations
Massachusetts Institute of Technology
Cambridge, United States
6 h-index
11 publications
580 citations
Planetary Science Institute
Tucson, United States
6 h-index
9 publications
315 citations

Delft University of Technology
Delft, The Netherlands
5 h-index
9 publications
834 citations
1–8 of 398
GJI · 56 publications · 3.3K citations
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PRB · 33 publications · 1.3K citations
19
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PRL · 18 publications · 2.5K citations
15
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PRB · 19 publications · 853 citations
14
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JGR · 8 publications · 577 citations
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