nic gases exsolved from magmas (Symonds et al. 1994). Thus, Ionian volcanic gases exsolved from magmas during eruption may also chemically ## We use thermochemical equilibrium calculations to show equilibrate (see below). that SO is expected in volcanic gases erupted on Io, and derive We modeled
Volcanic Origin of Disulfur Monoxide (S2O) on Io
β Scribed by Mikhail Yu. Zolotov; Bruce Fegley Jr.
- Publisher
- Elsevier Science
- Year
- 1998
- Tongue
- English
- Weight
- 486 KB
- Volume
- 133
- Category
- Article
- ISSN
- 0019-1035
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We used thermochemical equilibrium calculations in the O-S-Na-K-Cl-H system to model the speciation of volcanic gases emitted from high-temperature (1000-2000 K) silicate magmas on Io. The effects of temperature, pressure, and bulk composition of the gases are explored. The bulk compositions are bas
Io, the innermost Galilean satellite of Jupiter, is a fascinating world. Data taken by Voyager and Galileo instruments have established that it is by far the most volcanic body in the Solar System and suggest that the nature of this volcanism could radically differ from volcanism on Earth. We report