The thermal boundary-layer interpretation of D″ and its role as a plume source
- 1 August 1983
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 33 (1) , 45-55
- https://doi.org/10.1016/0031-9201(83)90006-7
Abstract
No abstract availableKeywords
This publication has 31 references indexed in Scilit:
- The dynamical and thermal structure of deep mantle plumesPhysics of the Earth and Planetary Interiors, 1983
- The effects of a strongly temperature-dependent viscosity on slow flow past a hot sphereJournal of Fluid Mechanics, 1982
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981
- Mantle plumes and the thermal stability of the D″ layerGeophysical Research Letters, 1980
- The cooling Earth: A reappraisalPhysics of the Earth and Planetary Interiors, 1980
- Second-order elasticity theory: Explanation for the high poisson's ratio of the inner corePhysics of the Earth and Planetary Interiors, 1980
- Core cooling by subsolidus mantle convectionPhysics of the Earth and Planetary Interiors, 1979
- Thermal regime of the Earth's corePhysics of the Earth and Planetary Interiors, 1973
- The creep strength of the Earth's mantleReviews of Geophysics, 1970
- Finite amplitude convective cells and continental driftJournal of Fluid Mechanics, 1967