Olivine zoning and retrograde olivine-orthopyroxene-metal equilibration in H5 and H6 chondrites

Author:

Reisener R. J.,Goldstein J. I.,Petaev M. I.

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Reference36 articles.

1. Optimized standard state and solution properties of minerals: Model calibration for olivine, orthopyroxene, cordierite, garnet, and ilmenite in the system FeO-MgO-CaO-Al2O3-TiO2-SiO2;Berman;Contributions to Mineralogy and Petrology,1996

2. Intrinsic oxygen fugacity measurements on seven chondrites, a pallasite, and a tektite and the redox state of meteorite parent bodies;Brett;Geochimica et Cosmochimica Acta,1984

3. Rates and mechanisms of Fe-Mg interdiffusion in olivine at 980-1300 °C;Chakraborty;Journal of Geophysical Research,1997

4. Chase M. W. 1998. NIST-JANAF thermochemical tables, 4th ed. Journal of Physical and Chemical Reference, Monograph 9. 1951 p.

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