Evidence of a lower mantle shear velocity discontinuity in S and sS phases
- 7 December 1986
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 13 (13) , 1493-1496
- https://doi.org/10.1029/gl013i013p01493
Abstract
No abstract availableThis publication has 8 references indexed in Scilit:
- Seismological properties of D″ and the structure of a thermal boundary layerPhysics of the Earth and Planetary Interiors, 1986
- Evidence against a discontinuity at the top of D'Geophysical Journal International, 1985
- The P wave velocity structure near the base of the mantleJournal of Geophysical Research, 1985
- Mapping the lower mantle: Determination of lateral heterogeneity in P velocity up to degree and order 6Journal of Geophysical Research, 1984
- The dynamical structures of D″ and deep plumes in a non-Newtonian mantlePhysics of the Earth and Planetary Interiors, 1984
- A lower mantle S-wave triplication and the shear velocity structure of D''Geophysical Journal International, 1983
- Present seismic evidence for a boundary layer at the base of the mantleJournal of Geophysical Research, 1983
- Convection, composition, and the thermal state of the lower mantleJournal of Geophysical Research, 1979