Chromium-Silicates, Feldspars and Highly Silicic Glasses Formed from Felsic Melts in Post-Depressurization Ferroan Ureilites, Especially LEW 88774

Details Chromium-Silicates, Feldspars and Highly Silicic Glasses Formed from Felsic Melts in Post-Depressurization Ferroan Ureilites, Especially LEW 88774 Chromium-Silicates, Feldspars and Highly Silicic Glasses Formed from Felsic Melts in Post-Depressurization Ferroan Ureilites, Especially LEW 88774

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.2400w&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.2400

Physics

3

Scientific paper

We describe the diverse suite of post-depressurization redox phases in
the LEW 88774 ureilite, and discuss the origin of these materials,
including the highly silicic (typically ~70 wt% SiO2) glasses that are
associated with Cr-spinels.

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