High-Ti Volcanic Glasses: Derivation from a Garnet-bearing Source Coupled with Assimilation of Late-Stage LMO Cumulates

Details High-Ti Volcanic Glasses: Derivation from a Garnet-bearing Source Coupled with Assimilation of Late-Stage LMO Cumulates High-Ti Volcanic Glasses: Derivation from a Garnet-bearing Source Coupled with Assimilation of Late-Stage LMO Cumulates

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.2086n&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.2086

Computer Science

1

Scientific paper

Compositions of volcanic glasses are modeled to investigate the presence
of garnet in their source regions.

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