Ascent and Eruption of Magmas on Io: Application to Pele

Details Ascent and Eruption of Magmas on Io: Application to Pele Ascent and Eruption of Magmas on Io: Application to Pele

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1555c&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1555

Physics

1

Scientific paper

We model eruptions at the Pele vent on Io as being due to discrete
buoyant dikes (volumes ~30 million cubic m) rising from a deep reservoir
under crustal structural control and absorbing near-surface SO2 to feed
short-lived (~1 hr long) events.

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