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Differentiation of magmas, as argued by [Bowen (1928)][1] and tested and refined by petrologists over the subsequent 50 years (cf. [Carmichael, et al. 1974][2]; [Yoder, 1979][3]; [Cox, et al., 1979][4]; [Hargraves, 1980][5]), contributes to the chemical, mineralogical, and textural diversity of

Sticky issues arising from high-viscosity magma: Settling arguments on magmatic structures