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Liquidus phase relations on the join diopside-forsterite-anorthite from 1 atm to 20 kbar: Their bearing on the generation and crystallization of basaltic magma

Magmatic ProcessVolcanologyEngineeringPhysicsMagmatismIgneous PetrogenesisApplied PhysicsGeologyCrustal MeltingLiquidus Phase RelationsGeochemistryExperimental PetrologyCrystallographyPetrologyBasaltic MagmaTectonics