The low viscosities of F + H2O-bearing granitic melts and implications for melt extraction and transport
- 1 May 1995
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 132 (1-4) , 199-211
- https://doi.org/10.1016/0012-821x(95)00054-g
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Least squares fitting of a straight line with correlated errorsPublished by Elsevier ,2005
- The extraction of magma from the crust and mantlePublished by Elsevier ,2002
- The combined effect of F and H2O on interdiffusion between peralkaline dacitic and rhyolitic meltsContributions to Mineralogy and Petrology, 1994
- Estimation of diffusion coefficients during interdiffusion of geologic melts: Application of transition state theoryChemical Geology, 1992
- The effect of H2O and CO2 on the viscosity of sanidine liquid at high pressuresJournal of Geophysical Research, 1990
- The fluid dynamics of evolving magma chambersPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1984
- Properties of Some Common Igneous Rocks and Their Melts at High TemperaturesGSA Bulletin, 1973
- Viscosities of magmatic silicate liquids; an empirical method of predictionAmerican Journal of Science, 1972
- Comments on viscosity, crystal settling, and convection in granitic magmasAmerican Journal of Science, 1965
- Obsidian-H2O viscosities at 1000 and 2000 bars in the temperature range 700° to 900°CJournal of Geophysical Research, 1963