A Unique Oxide-Bearing Clast in the Aubrite Allan Hills 84008: Evidence for Oxidation During Magmatic Processes

Details A Unique Oxide-Bearing Clast in the Aubrite Allan Hills 84008: Evidence for Oxidation During Magmatic Processes A Unique Oxide-Bearing Clast in the Aubrite Allan Hills 84008: Evidence for Oxidation During Magmatic Processes

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1347m&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1347

Physics

1

Scientific paper

A forsterite-sulfide clast in the ALH 84008 aubrite contains grains of
perovskite (CaTiO3) and geikielite (MgTiO3) and a
diopside-troilite-perovskite intergrowth. These oxides likely formed by
oxidation of reduced phases typically found in aubrites.

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