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The viscosity of magma is one of the most critical parameters of the various magmatic processes, such as magma segregation, magma uprise, crystallization differentiation, magma degassing and the mode of volcanic eruptions. Natural magmas almost always contain some crystals,where the bulk viscosity is often estimated through simple equations such as the Einstein-Roscoe equation. Pinkerton and Stevenson, among others, reviewed the methods of correction to obtain the bulk viscosity for melt crystal systems and indicated that crystal size distribution and the aspect ratio of crystals, in addition to the proportion of crystalline matter, greatly affect the bulk rheological properties of agmas. Previous experimental studies of subliquidus viscometry on basaltic magmas mostly pay little attention to the composition and textures of the crystals and melts.