Coda Wave Attenuation
Coda Wave Attenuation is a seismic attenuation measurement method that quantifies the temporal decay rate of coda wave amplitudes following the direct seismic arrivals, distinguishing itself by its reliance on scattered waves trapped in the Earth’s heterogeneities to infer regional subsurface attenuation properties.
233
Publications
12.6K
Citations
495
Authors
212
Institutions
Publications per year
2017–2026
38
Parents
233
1–5 of 233
495
10
h-index
Istituto Nazionale di Geofisica e Vulcanologia, Italy
9 publications · 444 citations
9
h-index
8
h-index
8
h-index
7
h-index
1–5 of 495
212

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
14 h-index
28 publications
914 citations

Indian Institute of Technology Roorkee
Roorkee, India
13 h-index
31 publications
1.1K citations
National Geophysical Research Institute
Hyderabad, India
11 h-index
27 publications
878 citations

Centre National de la Recherche Scientifique
Paris, France
9 h-index
22 publications
1.2K citations

Universidad de Granada
Granada, Spain
9 h-index
23 publications
688 citations
Universitat Politècnica de Catalunya
Barcelona, Spain
8 h-index
16 publications
646 citations
International Institute of Earthquake Engineering and Seismology
Tehran, Iran
8 h-index
17 publications
647 citations

Saint Louis University
St Louis, United States
7 h-index
12 publications
850 citations
1–8 of 212
BSSA · 52 publications · 3K citations
31
h-index
GJI · 41 publications · 1.8K citations
26
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PAGEOPH · 22 publications · 637 citations
16
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JGR · 18 publications · 3.5K citations
15
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15 publications · 766 citations
15
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1–5