IO: MODELS OF VOLCANISM AND INTERIOR STRUCTURE (JUPITER, MOON, CALDERAS, HEAT FLOW, LACCOLITHS).
The silicate "magma trigger" model of volcanism on Io has been evaluated numerically with finite element methods by considering the one-dimensional heat transfer between hot silicate magma and initially cold sulfur. It is found that for the probable range of initial magma temperatures and...
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| Language: | en |
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The University of Arizona.
1983
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| Online Access: | http://hdl.handle.net/10150/187613 |