Heat transfer of ascending cryomagma on Europa
摘要：
This study aims to link cryovolcanism at Europa's surface to the subsurface transport of cryomagmatic fluidsWe investigate heat transfer associated with cryomagma ascent on EuropaModels for heat transfer in diapirs, dikes, and pipe-like conduits are presentedIn some cases, fluids transported in tabular dikes or pipe-like conduits may reach the surface at temperatures exceeding 250KWarm ice may be brought to Europa's surface by diapirs that traverse preheated ascent paths
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DOI：
10.1016/j.jvolgeores.2016.03.018
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年份：
2016
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2018
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