Oriented Chromite-Diopside Symplectic Inclusions in Lunar Olivine from the "Luna-24": Hydrogenation-Dehydrogenation as a Mechanism of Simplectic Formation?

Details Oriented Chromite-Diopside Symplectic Inclusions in Lunar Olivine from the "Luna-24": Hydrogenation-Dehydrogenation as a Mechanism of Simplectic Formation? Oriented Chromite-Diopside Symplectic Inclusions in Lunar Olivine from the "Luna-24": Hydrogenation-Dehydrogenation as a Mechanism of Simplectic Formation?

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1068k&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1068

Computer Science

Scientific paper

Diopside-chromite symplectitic lamellae in olivine from the "Luna-24"
soil are studied with FIB/TEM and FE-EMPA and suggested to be formed by
two-step solid-state reaction involving exsolution, oxidation, cellular
decomposition, and dehydrogenation.

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