Double-diffusive convection in partially molten silicate systems: Its role during magma production and in magma chambers
- 31 October 1985
- journal article
- Published by Elsevier in Journal of Volcanology and Geothermal Research
- Vol. 26 (1-2) , 1-24
- https://doi.org/10.1016/0377-0273(85)90044-7
Abstract
No abstract availableThis publication has 37 references indexed in Scilit:
- Magma migration beneath an ocean ridgePublished by Elsevier ,2002
- Petrology of Young Pacific SeamountsJournal of Geophysical Research, 1984
- Double-Diffusive Convection Due to Crystallization in MagmasAnnual Review of Earth and Planetary Sciences, 1984
- Gradients in silicic magma chambers: Implications for lithospheric magmatismJournal of Geophysical Research, 1981
- Double-diffusive convectionJournal of Fluid Mechanics, 1981
- Crystallization in a double‐diffusive systemJournal of Geophysical Research, 1980
- Convective and interfacial instabilities during unidirectional solidification of a binary alloyJournal of Crystal Growth, 1980
- Free convection about a vertical flat plate embedded in a porous medium with application to heat transfer from a dikeJournal of Geophysical Research, 1977
- Ultrabasic magmas and high-degree melting of the mantleContributions to Mineralogy and Petrology, 1977
- The crystallization of haplobasaltic, haplodioritic, and related magmasAmerican Journal of Science, 1915