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Basalt-andesite-rhyolite-H2O: Crystallization intervals with excess H2O and H2O-undersaturated liquidus surfaces to 35 kolbras, with implications for magma genesis

Magmatic ProcessVolcanologyEarth ScienceEngineeringMagmatismIgneous PetrogenesisMagma GenesisGeologyGeochemistryIgneous ProcessChemistryExcess H2oPetrologyMagmatic-hydrothermal SystemCrystallization IntervalsTectonics