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Constraining Mantle Anelasticity Using S wave Amplitudes

Organization Virginia Polytechnic Institute and State UniversityLocation BLACKSBURG, United StatesPosted 1 Jun 2025Deadline 31 May 2028
NSFUS FederalResearch GrantScience FoundationVA
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Earthquakes generate seismic waves that propagate through the interior of the Earth, with their amplitude gradually decaying as they travel. This reduction in amplitude, known as attenuation or anelasticity, provides crucial insights into the properties of the materials they travel through. By analyzing mantle anelasticity, we can determine key…

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Constraining Mantle Anelasticity Using S wave Amplitudes — Virginia Polytechnic Institute and State University | United | Dev Procure