Numerical models of a dense layer at the base of the mantle and implications for the geodynamics of D″
- 10 May 2000
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 105 (B5) , 11101-11114
- https://doi.org/10.1029/1999jb900450
Abstract
No abstract availableKeywords
This publication has 61 references indexed in Scilit:
- Growing the Earth's D″ layer: Effect of density variations at the core‐mantle boundaryGeophysical Research Letters, 1997
- Three regimes of mantle convection with non‐Newtonian viscosity and stagnant lid convection on the terrestrial planetsGeophysical Research Letters, 1997
- Implications of a metal‐bearing chemical boundary layer in D″ for mantle dynamicsGeophysical Research Letters, 1996
- Correlation analysis between subduction in the last 180 Myr and lateral seismic structure of the lower mantle: geodynamical implicationsGeophysical Research Letters, 1995
- On the possibility of anisotropy in the D″ layer as inferred from the polarization of diffracted S wavesPhysics of the Earth and Planetary Interiors, 1994
- Conman: vectorizing a finite element code for incompressible two-dimensional convection in the Earth's mantlePhysics of the Earth and Planetary Interiors, 1990
- The core shadow zone boundary and lateral variations of the P velocity structure of the lowermost mantlePhysics of the Earth and Planetary Interiors, 1989
- Interaction of mantle dregs with convection: Lateral heterogeneity at the core‐mantle boundaryGeophysical Research Letters, 1986
- Seismological properties of D″ and the structure of a thermal boundary layerPhysics of the Earth and Planetary Interiors, 1986
- The thermal boundary-layer interpretation of D″ and its role as a plume sourcePhysics of the Earth and Planetary Interiors, 1983