Modeling Io volcanism: Maximum volcanic temperatures, depths of melting and magma composition

Details Modeling Io volcanism: Maximum volcanic temperatures, depths of melting and magma composition Modeling Io volcanism: Maximum volcanic temperatures, depths of melting and magma composition

Apr 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984pggp.rept...14c&link_type=abstract

In NASA. Washington Repts. of Planetary Geol. Program p 14-16 (SEE N84-23431 13-91)

Mathematics

Heat Transmission, Io, Magma, Mathematical Models, Surface Temperature, Volcanoes, Finite Element Method, Heat Transfer, Modulus Of Elasticity, Plumes, Sulfur, Temperature Distribution

Scientific paper

Interim results of thermal and structural modeling of volcanism on Io were presented. The final results of the modeling are summarized. The basic analysis is an evaluation of the magma trigger mechanism for initiating and maintaining eruptions. Secondary aspects include models of the mechanical mode of magma emplacement, interactions with a sulphur-rich upper crust, and more speculative implications for Io's volcanism.

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