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The viscosities of a series of granitic (sensu lato) melts have been determined in the range of 10 3  to 10 12  Pa·s. The anhydrous melt compositions are based on the addition of 10, 20, 50, and 75 wt% of the anorthite component (CaAl 2 Si 2 O 8 ) to a haplogranitic melt (HPG8) whose composition lies near the 2 kbar water-saturated minimum melt composition in the system NaAlSi 3 O 8 -KAlSi 3 O 8 -SiO 2 . Melts with 10 and 20 wt% normative anorthite were subjected to high-pressure hydration syntheses using a piston-cylinder apparatus to generate water contents up to 2 wt%. Viscosities were determined for the anhydrous melts using the concentric cylinder method in the viscosity range of 10 2  to 10 5  Pa·s, and for both anhydrous and hydrated melts in the range of 10 9  to 10 12  Pa·s.

Viscosities of granitic (sensu lato) melts: Influence of the anorthite component