Possible Causes for Late-Stage Reaction Textures Associated with Pyroxferroite and Metastable Pyroxenes in the Basaltic Martian Meteorites

Details Possible Causes for Late-Stage Reaction Textures Associated with Pyroxferroite and Metastable Pyroxenes in the Basaltic Martian Meteorites Possible Causes for Late-Stage Reaction Textures Associated with Pyroxferroite and Metastable Pyroxenes in the Basaltic Martian Meteorites

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1003a&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1003

Physics

1

Scientific paper

Fine-grained assemblages of fayalite + SiO2 +/- hedenbergite are
observed in Los Angeles, QUE 94201, and Shergotty. These textures are
likely from the breakdown of metastable pyroxenes and/or pyroxferroite
and modification by diffusional reequilibration.

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