Body waves in a layered anelastic solid
- 1 October 1976
- journal article
- Published by Seismological Society of America (SSA) in Bulletin of the Seismological Society of America
- Vol. 66 (5) , 1539-1554
- https://doi.org/10.1785/bssa0660051539
Abstract
A formulation extending the Haskell-Thompson matrix method to include the effects of anelastic attenuation is presented. The formulation is exact in that no low-loss approximations are made. Consideration is given to nonparallel propagation and attenuation directions with corresponding velocity anisotropy. Examples are presented for models representing soils, the crust, and the core-mantle boundary.Keywords
This publication has 14 references indexed in Scilit:
- Energy and plane waves in linear viscoelastic mediaJournal of Geophysical Research, 1973
- The density distribution near the base of the mantle and near the earth's centerPhysics of the Earth and Planetary Interiors, 1972
- Seismic Source Descriptions of Underground Explosions and a Depth DiscriminateGeophysical Journal International, 1972
- Plane Waves in Linear Viscoelastic MediaGeophysical Journal International, 1971
- Reflection and Transmission of Oblique Plane Waves at a Plane Interface between Viscoelastic MediaThe Journal of the Acoustical Society of America, 1967
- Dispersive body wavesJournal of Geophysical Research, 1962
- Crustal reflection of planePandSVwavesJournal of Geophysical Research, 1962
- On the linear theory of viscoelasticityArchive for Rational Mechanics and Analysis, 1962
- The reflection and refraction of waves at an interface between viscoelastic materialsJournal of the Mechanics and Physics of Solids, 1962
- Crustal reflection of planeSHwavesJournal of Geophysical Research, 1960