A Disequilibrium Reactive Transport Model for Mantle Magmatism
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DOI: 10.1093/petrology/egaa067
Abstract: Besides standard thermo-mechanical conservation laws, a general description of mantle magmatism requires the simultaneous consideration of phase changes (e.g. from solid to liquid), chemical reactions (i.e. exchange of chemical components) and multiple dynamic phases (e.g.… read more here.
Keywords: mantle magmatism; trace; model; chemical ... See more keywords