Anelastic Attenuation
Anelastic Attenuation is a geophysical phenomenon within seismic attenuation characterized by the gradual dissipation of seismic wave energy due to non-elastic deformation processes in Earth materials, distinguished from elastic attenuation by its dependence on intrinsic material properties such as viscosity and relaxation mechanisms.
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Viscoelastic finite-difference modeling
Johan O. A. Robertsson, Joakim O. Blanch, William W. Symes · Geophysics · 1994 · 595 citations
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United States Geological Survey
Reston, United States
15 h-index
27 publications
4.1K citations

Saint Louis University
St Louis, United States
13 h-index
19 publications
885 citations
The University of Tokyo
Tokyo, Japan
10 h-index
21 publications
1.1K citations
University of Cambridge
Cambridge, United Kingdom
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38 publications
798 citations
Planetary Science Institute
Tucson, United States
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12 publications
1.3K citations

Western University
London, Canada
7 h-index
13 publications
748 citations
University of California, Berkeley
Berkeley, United States
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15 publications
2K citations
Curtin University
Perth, Australia
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20 publications
903 citations
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BSSA · 74 publications · 9.6K citations
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GJI · 50 publications · 2.5K citations
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JGR · 24 publications · 1.8K citations
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