The origin of the depletions of V, Cr and Mn in the mantles of the Earth and Moon
- 30 December 2000
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 184 (1) , 95-107
- https://doi.org/10.1016/s0012-821x(00)00323-x
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Oxide‐metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's coreJournal of Geophysical Research, 1998
- The Origin of the Moon and the Single Impact Hypothesis V☆Icarus, 1997
- Prediction of siderophile element metal-silicate partition coefficients to 20 GPa and 2800°C: the effects of pressure, temperature, oxygen fugacity, and silicate and metallic melt compositionsPhysics 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
- Stability of clinopyroxene at pressure-temperature conditions of the transition regionPhysics of the Earth and Planetary Interiors, 1994
- High-Pressure and High-Temperature Experiments on Core-Mantle Segregation in the Accreting EarthScience, 1994
- Early Differentiation of the Earth and the Problem of Mantle Siderophile Elements: A New ApproachScience, 1991
- Partitioning of Cr, V, and Mn between mantles and cores of differentiated planetesimals: Implications for giant impact hypothesis of lunar originIcarus, 1991
- High-pressure geochemistry of Cr, V and Mn and implications for the origin of the MoonNature, 1990
- The Bakerian Lecture, 1983 - The Earth’s core: its composition, formation and bearing upon the origin of the EarthProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1984