Heat transport by variable viscosity convection II: pressure influence, non-Newtonian rheology and decaying heat sources
- 28 February 1985
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 37 (2-3), 183-205
- https://doi.org/10.1016/0031-9201(85)90051-2
Abstract
No abstract availableThis publication has 16 references indexed in Scilit:
- Heat transport by variable viscosity convection and implications for the Earth's thermal evolutionPhysics of the Earth and Planetary Interiors, 1984
- Steady state, secondary convection beneath lithospheric plates with temperature‐ and pressure‐dependent viscosityJournal of Geophysical Research, 1984
- Subducted slabs and the geoid: Constraints on mantle rheology and flowJournal of Geophysical Research, 1984
- Convection with pressure- and temperature-dependent non-Newtonian rheologyGeophysical Journal International, 1984
- Convection in a variable-viscosity fluid: Newtonian versus power-law rheologyEarth and Planetary Science Letters, 1983
- Material properties for mantle convection consistent with observed surface fieldsJournal of Geophysical Research, 1980
- Convection with decaying heat sources: constant viscosityGeophysical Journal International, 1980
- Convection, composition, and the thermal state of the lower mantleJournal of Geophysical Research, 1979
- Thermal convection with strongly temperature-dependent viscosityJournal of Fluid Mechanics, 1976
- Low-stress high-temperature creep in olivine single crystalsJournal of Geophysical Research, 1974