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Crustal melting to produce granite magmas requires a tremendous amount of energy. In principle, there are three main mechanisms of heating that can extensively melt a fertile crust: radiogenic heat caused by the decay of 40 K, 230 Th, 235 U and 238 U; increased subcrustal heat flux caused by the upwelling of deeper, therefore hotter, mantle materials; advection of heat...
Assimilation of foreign material into a granitic magma body entails mixing between two end-member components: the initially solid assimilant, and the original magma, whose composition is mostly represented by a granitic liquid. In this study, we assess the interactions between a haplogranite liquid made to the composition of the minimum at 200MPa H 2 O (Ab 38.23 Or 28.72 Qtz...
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