Anelasticity from seismic to tidal timescales: Theory and observations
- 1 February 2019
- journal article
- research article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 508, 18-29
Abstract
No abstract availableKeywords
Funding Information
- NSF (EAR-1464024)
- NASA (NNX17AE42G)
- Harvard Society of Fellows
This publication has 47 references indexed in Scilit:
- Steady-state laboratory flow laws alone fail to explain postseismic observationsEarth and Planetary Science Letters, 2010
- Frequency dependence of Q in Earth's upper mantle inferred from continuous spectra of body wavesGeophysical Research Letters, 2004
- Grain‐size‐sensitive seismic wave attenuation in polycrystalline olivineJournal of Geophysical Research, 2002
- Viscoelasticity of the titanate perovskites CaTiO3 and SrTiO3 at high temperaturePhysics of the Earth and Planetary Interiors, 1999
- Low‐frequency shear attenuation in polycrystalline olivine: Grain boundary diffusion and the physical significance of the Andrade model for viscoelastic rheologyJournal of Geophysical Research, 1998
- Grain Growth Rates of MgSiO 3 Perovskite and Periclase Under Lower Mantle ConditionsScience, 1996
- Sound velocity and elasticity of single‐crystal forsterite to 16 GPaJournal of Geophysical Research, 1996
- Defect microdynamics in minerals and solid‐state mechanisms of seismic wave attenuation and velocity dispersion in the mantleReviews of Geophysics, 1990
- The effects of transient rheology on the interpretation of lower mantle viscosityGeophysical Research Letters, 1985
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981