MG‐perovskite/silicate melt and majorite garnet/silicate melt partition coefficients in the SYSTEM CaO ‐ MgO ‐ SiO2at high temperatures and pressures
- 25 March 1993
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 98 (E3) , 5427-5431
- https://doi.org/10.1029/92je02290
Abstract
No abstract availableKeywords
This publication has 17 references indexed in Scilit:
- Experimental determination of element partitioning between silicate perovskites, garnets and liquids: constraints on early differentiation of the mantlePublished by Elsevier ,2002
- The origin of the Moon and the single-impact hypothesis IIIPublished by Elsevier ,2002
- FORMATION OF THE EARTHAnnual Review of Earth and Planetary Sciences, 1990
- Partitioning “equilibrium”, temperature gradients, and constraints on Earth differentiationEarth and Planetary Science Letters, 1989
- Mass balance and phase density constraints on early differentiation of chondritic mantleEarth and Planetary Science Letters, 1988
- Constraints on element partition coefficients between MgSiO3 perovskite and liquid determined by direct measurementsEarth and Planetary Science Letters, 1988
- Melting of peridotite at uppermost lower-mantle conditionsNature, 1987
- Occurrence of Giant Impacts During the Growth of the Terrestrial PlanetsScience, 1985
- Noble gas contents of shergottites and implications for the Martian origin of SNC meteoritesGeochimica et Cosmochimica Acta, 1984
- The case for a martian origin of the shergottites: nitrogen and noble gases in EETA 79001Earth and Planetary Science Letters, 1984