Thermodynamics of SiO2–H2O fluid near the upper critical end point from quartz solubility measurements at 10 kbar
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Reference44 articles.
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3. Complete miscibility between silicate melts and hydrous fluids in the upper mantle: experimental evidence and geochemical implications;Bureau;Earth Planet. Sci. Lett.,1999
4. The role of H2O in silicate melts: II. Thermodynamic and phase relations in the system NaAlSi3O8–H2O to 10 kilobars, 700°–1100 °C;Burnham;Am. J. Sci.,1974
5. High–low quartz inversion: determinations to 35 kilobars;Cohen;J. Geophys. Res.,1967
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