Fe2+ partitioning between the M1 and M2 sites in silicate crystals in some stony and stony-iron meteorites studied using X-ray diffraction and Mössbauer spectroscopy
A. A. Maksimova, E. V. Petrova, А. В. Чукин, М. И. Оштрах
Topics & Concepts
MeteoriteOlivineMössbauer spectroscopySilicateChemistryDiffractionAnalytical Chemistry (journal)MineralogyCrystallographyPhysicsAstrobiologyOpticsOrganic chemistryChromatographyAstro and Planetary ScienceHigh-pressure geophysics and materialsPlanetary Science and Exploration