Volatile oversaturation during the evolution of silicic magma chambers as an eruption trigger
- 20 September 1984
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 89 (B10), 8237-8244
- https://doi.org/10.1029/jb089ib10p08237
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- Some Aspects of the Role of Water In Rock MeltsPublished by Geological Society of America ,2015
- An empirical Redlich-Kwong-type equation of state for water to 1,000 °C and 200 KbarBeiträge zur Mineralogie und Petrographie, 1982
- Gradients in silicic magma chambers: Implications for lithospheric magmatismJournal of Geophysical Research, 1981
- Horizontal and vertical zoning in the Peruvian Coastal BatholithJournal of the Geological Society, 1981
- Volcanism and the dynamics of open magma chambersNature, 1981
- Distribution of Quaternary rhyolite domes of the Coso Range, California: Implications for extent of the geothermal anomalyJournal of Geophysical Research, 1980
- Fluids in the evolution of granitic magmas: Consequences of finite CO2 solubilityGSA Bulletin, 1976
- Meteoric Water in MagmasScience, 1974
- Pyroclastic flows in JapanBulletin of Volcanology, 1963
- Petrology and Petrogenesis of the Quaternary Pumice Ash in the Taupo Area, New ZealandJournal of Petrology, 1963