Magma ocean fractional crystallization and cumulate overturn in terrestrial planets: Implications for Mars
- 1 December 2003
- journal article
- Published by Wiley in Meteoritics & Planetary Science
- Vol. 38 (12), 1753-1771
- https://doi.org/10.1111/j.1945-5100.2003.tb00013.x
Abstract
No abstract availableKeywords
This publication has 73 references indexed in Scilit:
- Garnet–ilmenite–perovskite transitions in the system Mg4Si4O12–Mg3Al2Si3O12 at high pressures and high temperatures: phase equilibria, calorimetry and implications for mantle structurePhysics of the Earth and Planetary Interiors, 2002
- Determining the composition of the EarthNature, 2002
- Grain‐scale channelization of pores due to gradients in temperature or composition of intergranular fluid or meltJournal of Geophysical Research, 2002
- Thermal equation of state of magnesiowüstite (Mg0.6Fe0.4)OPhysics of the Earth and Planetary Interiors, 2002
- Implications of Mars Pathfinder Data for the Accretion History of the Terrestrial PlanetsScience, 1998
- Thermal and chemical evolution of the terrestrial magma oceanPhysics of the Earth and Planetary Interiors, 1997
- Rheology of crystal‐bearing silicate melts: An experimental study at high viscositiesJournal of Geophysical Research: Solid Earth, 1995
- Phase transition Clapeyron slopes and transition zone seismic discontinuity topographyJournal of Geophysical Research, 1994
- Physical state of the very early EarthLithos, 1993
- Olivine flotation and crystallization of a global magma oceanPhysics of the Earth and Planetary Interiors, 1992