Generation of mega‐plumes from the core‐mantle boundary in a compressible mantle with temperature‐dependent viscosity
- 1 June 1998
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 25 (11) , 1999-2002
- https://doi.org/10.1029/98gl01228
Abstract
No abstract availableThis publication has 17 references indexed in Scilit:
- Inferences of viscosity from the oceanic geoid: Indication of a low viscosity zone below the 660-km discontinuityEarth and Planetary Science Letters, 1997
- The excess temperature of plumes rising from the core‐mantle boundaryGeophysical Research Letters, 1996
- MELTING TEMPERATURE OF THE EARTH'S MANTLE AND CORE: Earth's Thermal StructureAnnual Review of Earth and Planetary Sciences, 1996
- Effects of strongly variable viscosity on three‐dimensional compressible convection in planetary mantlesJournal of Geophysical Research, 1996
- Penetration of plates and plumes through the mantle transition zoneEarth and Planetary Science Letters, 1995
- Mantle plume interaction with an endothermic phase changeJournal of Geophysical Research, 1995
- Effects of multiple phase transitions in a three‐dimensional spherical model of convection in Earth's mantleJournal of Geophysical Research, 1994
- Rheology of the Upper Mantle: A SynthesisScience, 1993
- The effects of adiabatic and viscous heatings on plumesGeophysical Research Letters, 1987
- Convection Plumes in the Lower MantleNature, 1971