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cryomagmas

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Journal Article
Published: 01 December 2013
European Journal of Mineralogy (2013) 25 (5): 735–743.
... at the conditions of cryomagma reservoirs within the icy crust of the Europa satellite and, by using these data, to simulate processes affecting the reservoirs such as the vapour formation and eruption to the surface ( Head & Wilson, 2003 ). In order to do this, the following conditions are assumed: 1...
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Bulk total densities,  β , (symbols) and liquid densities,  ρ , (solid line...
Published: 01 December 2013
Fig. 8 Bulk total densities, β , (symbols) and liquid densities, ρ , (solid lines, from Vance, 2007 ) of cryomagmas vs . depth within Europás crust, for each experiment, M1–5, at several conditions of MgSO 4 concentration and temperature.
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(Left): Sketch of the model of <span class="search-highlight">cryomagma</span> degasification in which the bubble...
Published: 01 December 2013
Fig. 9 (Left): Sketch of the model of cryomagma degasification in which the bubble and fragmentation depths, which can produce an explosive eruption, are predicted. (Right), Image PIA00294 from the Galileo mission where cryoclastic deposits around Belus Linea can be seen.
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Depth within Europa (calculated with  Equation 7 ) as a function of the sol...
Published: 01 December 2013
Fig. 7 Depth within Europa (calculated with Equation 7 ) as a function of the solubility data of CO 2 in mass fraction, S PT, for different cryomagmas, M1–M5. Vertical line represents the initial concentration of CO 2 , x iCO 2 = 0.03. From this figure the bubble pressures ( P B
Journal Article
Published: 01 April 2009
Mineralogical Magazine (2009) 73 (2): 167–191.
... = 10 1 Pa s) Bg φ = 0.0555 5.9 × 10 -7 φ = 0.7405 2.1 × 10 -6 Rhyolite (η 0 = 10 5 Pa s) φ = 0.0555 5.9 × 10 -11 φ = 0.0745 2.1 × 10 -10 Cryomagma (η 0 = 10 -1 Pa s) φ = 0.0555 3.5 × 10 -5 φ = 0.7405 1.29 × 10 -4 The particle migration effects...
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