The influence of amphibole fractionation on the evolution of calc-alkaline andesite and dacite tephra from the central Aleutians, Alaska
- 1 October 1992
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 112 (1) , 101-118
Abstract
No abstract availableKeywords
This publication has 41 references indexed in Scilit:
- Ultramafic Xenoliths from Adagdak Volcano, Adak, Aleutian Islands, Alaska: Deformed Igneous Cumulates from the Moho of an Island ArcThe Journal of Geology, 1987
- Depths and water content of magma chambers in the Aleutian and Mariana island arcsGeology, 1987
- Post-caldera dacites from the Santorini volcanic complex, Aegean Sea, Greece: an example of the eruption of lavas of near-constant composition over a 2,200 year periodContributions to Mineralogy and Petrology, 1986
- Magmatic Evolution of Semisopochnoi Island, Alaska: Trace-Element and Isotopic ConstraintsThe Journal of Geology, 1985
- Volatile oversaturation during the evolution of silicic magma chambers as an eruption triggerJournal of Geophysical Research, 1984
- Ultramafic and Mafic Inclusions from Adak Island: Crystallization History, and Implications for the Nature of Primary Magmas and Crustal Evolution in the Aleutian ArcJournal of Petrology, 1984
- Amphibole fractionation in calc-alkaline magma genesisAmerican Journal of Science, 1976
- Crystallization and Fractionation Trends in the System Andesite-H2O-CO2-O2 at Pressures to 10 KbGeological Society of America Bulletin, 1973
- Amphibole stability in H2O-undersaturated calc-alkaline meltsEarth and Planetary Science Letters, 1972
- The iron-titanium oxides of salic volcanic rocks and their associated ferromagnesian silicatesContributions to Mineralogy and Petrology, 1966