Seismological properties of D″ and the structure of a thermal boundary layer
- 31 January 1986
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 41 (4), 225-239
- https://doi.org/10.1016/0031-9201(86)90002-6
Abstract
No abstract availableKeywords
This publication has 38 references indexed in Scilit:
- S velocities in D'' from diffracted SH-waves at the core boundaryGeophysical Journal International, 1984
- Seismic anisotropy -- the state of the art: IIGeophysical Journal International, 1984
- Present seismic evidence for a boundary layer at the base of the mantleJournal of Geophysical Research, 1983
- Thermodynamic parameters in the Earth as determined from seismic profilesGeophysical Journal International, 1981
- The effect of a second-order velocity discontinuity on elastic waves near their turning pointGeophysical Journal International, 1981
- A thermodynamically based equation of state for the lower mantleJournal of Geophysical Research, 1979
- P and S waves diffracted around the core and the velocity structure at the base of the mantleGeophysical Journal International, 1979
- On seismic-wave scattering by a rough core?mantle boundaryGeophysical Journal International, 1978
- Some elastic constant data on minerals relevant to geophysicsReviews of Geophysics, 1968
- Long-wave elastic anisotropy produced by horizontal layeringJournal of Geophysical Research, 1962