Upper Mantle Attenuation
Upper Mantle Attenuation is a geophysical phenomenon within seismic attenuation that specifically characterizes the dissipation of seismic wave energy due to anelastic processes in the Earth's upper mantle, distinguished from attenuation in other mantle layers by its dependence on temperature, composition, and partial melt in the depth range approximately 50 to 660 kilometers.
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Lateral inhomogeneities of the upper mantle
Markus Båth · Tectonophysics · 1965 · 537 citations
L. Knopoff · Reviews of Geophysics · 1964 · 431 citations
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Institut de physique du globe de Paris
Paris, France
23 h-index
49 publications
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Australian National University
Canberra, Australia
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51 publications
6.2K citations

Centre National de la Recherche Scientifique
Paris, France
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54 publications
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Planetary Science Institute
Tucson, United States
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Lamont-Doherty Earth Observatory
Sparkill, United States
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California Institute of Technology
Pasadena, United States
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29 publications
2K citations
China Earthquake Administration
Beijing, China
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55 publications
2.8K citations
Massachusetts Institute of Technology
Cambridge, United States
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JGR · 75 publications · 8.9K citations
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GJI · 48 publications · 2.6K citations
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