Eruption Conditions and Mechanism of A17 Orange Glass Eruption: Petrologyand Modeling Data

Details Eruption Conditions and Mechanism of A17 Orange Glass Eruption: Petrologyand Modeling Data Eruption Conditions and Mechanism of A17 Orange Glass Eruption: Petrologyand Modeling Data

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1322r&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1322

Computer Science

Scientific paper

The gas phase in the A17 orange glass magma is constrained by C-O-S
phase equilibria and the compositions of glass and phenorysts.
Equilibrium C-O gas generation by C-oxidation is at 4 km. Modeling
constrains the C necessary to achieve fragmentation of the orange glass
melt prior to eruption.

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