Causes of magmatic diversity

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Magmatic Processes : Physicochemical Principles

The viscosities of eight melt compositions in the System albite-H20-F20_1 have been determined at high pressure and temperature. Measurements were performed using the falling sphere method at 1000-1600°C and 2.5 to 22.5 kbar. Fluorine and water strongly decrease the viscosity of albite melt at all pressures and temperatures investigated. The viscosity of a fluorine-bearing albitic melt decrease...

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ژورنال

عنوان ژورنال: Nature

سال: 1988

ISSN: 0028-0836,1476-4687

DOI: 10.1038/333397a0