Partitioning of Fe2+ and Mg2+ between olivine and garnet
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Reference23 articles.
1. Iron(II)-magnesium exchange equilibrium between olivine and calcium-free pyroxene over a temperature range 800°C to 1300°C;Matsui;Bull. Soc. Fr. Minéral. Cristallogr.,1974
2. The mineralogic distribution of iron in the upper mantle;Ahrens;Phys. Earth Planet. Inter.,1972
3. Petrology and petrogenesis of some garnetiferous peridotites;O'Hara;Trans. R. Soc. Edinburgh,1963
4. Distribution of elements between coexisting minerals and the nature of solid solution in garnet;Saxena;Am. Mineral.,1968
5. Study on the compositional dependence of the apparent partition coefficient of iron and magnesium between coexisting garnet and clinopyroxene solid solutions;Oka;Contrib. Mineral. Petrol.,1974
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3. Exchange of Fe2+and Mg2+Between Olivine and Clinopyroxene at 7.5 GPa and 1300°C;High-Pressure Research: Application to Earth and Planetary Sciences;2013-03-18
4. A recalibration of the garnet-olivine geothermometer and a new geobarometer for garnet peridotites and garnet-olivine-plagioclase-bearing granulites;Journal of Metamorphic Geology;2007-06
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