A simple parameterized model of Earth's thermal history with the transition from layered to whole mantle convection
- 30 April 1995
- journal article
- research article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 131 (3-4) , 357-369
- https://doi.org/10.1016/0012-821x(95)00034-a
Abstract
No abstract availableThis publication has 24 references indexed in Scilit:
- Effects of chemical fractionation of heat-producing elements on mantle evolution inferred from a numerical model of coupled magmatism-mantle convection systemPhysics of the Earth and Planetary Interiors, 1994
- Model for Convective Cooling of Mantle with Phase Changes: Effects of Aspect Ratios and Initial Conditions.Journal of Physics of the Earth, 1994
- Melting of (Mg, Fe)SiO 3 -Perovskite to 625 Kilobars: Indication of a High Melting Temperature in the Lower MantleScience, 1993
- Instabilities from phase transitions and the timescales of mantle thermal evolutionGeophysical Research Letters, 1993
- Multiple phase transitions and the style of mantle convectionPhysics of the Earth and Planetary Interiors, 1992
- Melting of peridotite at uppermost lower-mantle conditionsNature, 1987
- Regionalized models for the thermal evolution of the EarthEarth and Planetary Science Letters, 1984
- On the thermal evolution of the earthEarth and Planetary Science Letters, 1980
- Speculations on the Thermal and Tectonic History of the EarthGeophysical Journal of the Royal Astronomical Society, 1975
- Finite amplitude convective cells and continental driftJournal of Fluid Mechanics, 1967