Linked magma ocean solidification and atmospheric growth for Earth and Mars
Top Cited Papers
- 1 July 2008
- journal article
- research article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 271 (1-4) , 181-191
- https://doi.org/10.1016/j.epsl.2008.03.062
Abstract
No abstract availableKeywords
This publication has 64 references indexed in Scilit:
- Hydrogen partition coefficients between nominally anhydrous minerals and basaltic meltsGeophysical Research Letters, 2004
- Water transport into the deep mantle and formation of a hydrous transition zonePhysics of the Earth and Planetary Interiors, 2004
- Convective cooling of an initially stably stratified fluid with temperature‐dependent viscosity: Implications for the role of solid‐state convection in planetary evolutionJournal of Geophysical Research, 2004
- Formation, history and energetics of cores in the terrestrial planetsPublished by Elsevier ,2002
- Determining the composition of the EarthNature, 2002
- Thermal and chemical evolution of the terrestrial magma oceanPhysics of the Earth and Planetary Interiors, 1997
- Melting experiments on anhydrous peridotite KLB‐1: Compositions of magmas in the upper mantle and transition zoneJournal of Geophysical Research, 1996
- Olivine flotation and crystallization of a global magma oceanPhysics of the Earth and Planetary Interiors, 1992
- Meteorite Impact Ejecta: Dependence of Mass and Energy Lost on Planetary Escape VelocityScience, 1977
- Convection from the Earth’s surfaceProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1957