Gas saturation and evolution of volatile and light lithophile elements in the Bandelier magma chamber between two caldera-forming eruptions

Journal of Geophysical Research: Solid Earth

Volumn 101, Issue B11, 1996, Pages 25181-25196

  Stix, John ^a   Layne, Graham D ^b  

^a UNIVERSITÉ DE MONTRÉAL   (Canada)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CALDERA; GAS SATURATION; LIGHT ELEMENT; MAGMA CHAMBER; VOLATILE ELEMENT; VOLCANIC ERUPTION;

USA, NEW MEXICO;

EID: 0344930405     PISSN: 21699313     EISSN: 21699356     Source Type: Journal    
DOI: None     Document Type: Article

References (6)

1. 2 from Mount Etna, Nature, 351, 387-391, 1991.
2. 2, Cl, and gas in Plinian and ash-flow Bishop Rhyolite, Geology, 17, 221-225, 1989.
3. Candela, P.A., Toward a thermodynamic model for the halogens in magmatic systems: An application to melt-vapor-apatite equilibria, Chem. Geol., 57, 289-301, 1986.
4. 2O to 1000°C and 1500 bars, Geochim. Cosmochim. Acta, 51, 1965-1975, 1987.
5. Devine, J.D., H. Sigurdsson, A.N. Davis, and S. Self, Estimation of sulfur and chlorine yield to the atmosphere from volcanic eruptions and potential climatic effects, J. Geophys. Res., 89, 6309-6325, 1984.
6. 2O contents of silicic volcanic glasses. Am. Mineral., 80, 319-328, 1995.