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    The viscosity of hydrous dacitic liquids: implications for the rheology of evolving silicic magmas

    The viscosity of a series of six synthetic dacitic liquids, containing up to 5.04 wt% dissolved water, was measured above the glass transition range by parallel-plate viscometry. The temperature of the 1011 Pa s ...

    Alan G. Whittington, Bridget M. Hellwig, Harald Behrens… in Bulletin of Volcanology (2009)