Steady-state volcanism, paleoeffusion rates, and magma system volume inferred from plagioclase crystal size distributions in mafic lavas: Dome Mountain, Nevada
Open Access
- 1 November 1995
- journal article
- research article
- Published by Elsevier in Journal of Volcanology and Geothermal Research
- Vol. 68 (4) , 273-296
- https://doi.org/10.1016/0377-0273(95)00003-5
Abstract
No abstract availableThis publication has 36 references indexed in Scilit:
- Conjugate solidification and melting in multicomponent open and closed systemsInternational Journal of Heat and Mass Transfer, 1992
- Dusty and honeycomb plagioclase: indicators of processes in the Uchino stratified magma chamber, Izu Peninsula, JapanJournal of Volcanology and Geothermal Research, 1992
- Crystal size distribution systematics and the determination of magma storage times: The 1959 eruption of Kilauea volcano, HawaiiJournal of Volcanology and Geothermal Research, 1990
- Crystallization of Mount St. Helens 1980?1986 dacite: A quantitative textural approachBulletin of Volcanology, 1988
- Changes in magma composition at Arenal volcano, Costa Rica, 1968?1985: Real-time monitoring of open-system differentiationBulletin of Volcanology, 1987
- On the distribution and separation of crystals in convecting magmaJournal of Volcanology and Geothermal Research, 1985
- Geophysical evidence for the locations, shapes and sizes, and internal structures of magma chambers beneath regions of Quaternary volcanismPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1984
- Thermal Evolution of Plutons: A Parameterized ApproachScience, 1980
- On the heat and mass transfer from an ascending magmaEarth and Planetary Science Letters, 1978
- Nucleation and growth of plagioclase, Makaopuhi and Alae lava lakes, Kilauea Volcano, HawaiiGSA Bulletin, 1977