Articles | Volume 36, issue 5
https://doi.org/10.5194/ejm-36-721-2024
https://doi.org/10.5194/ejm-36-721-2024
Research article
 | 
09 Sep 2024
Research article |  | 09 Sep 2024

Magma storage conditions of Lascar andesites, central volcanic zone, Chile

André Stechern, Magdalena Blum-Oeste, Roman E. Botcharnikov, François Holtz, and Gerhard Wörner

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Cited articles

Almeev, R. R., Holtz, F., Koepke, J., and Parat, F.: Experimental calibration of the effect of H2O on plagioclase crystallization in basaltic melt at 200 MPa, Am. Mineral., 97, 1234–1240, 2012. 
Almeev, R. R., Holtz, F., Ariskin, A. A., and Kimura, J.-I.: Storage conditions of Bezymianny Volcano parental magmas: results of phase equilibria experiments at 100 and 700 MPa, Contrib. Mineral. Petr., 166, 1389–1414, 2013a. 
Almeev, R. R., Kimura, J.-I., Ariskin, A. A., and Ozerov, A. Y.: Decoding crystal fractionation in calc-alkaline magmas from the Bezymianny Volcano (Kamchatka, Russia) using mineral and bulk rock compositions, J. Volcanol. Geoth. Res., 263, 141–171, 2013b. 
Andersen, D. J.: New (and final!) models for the Ti-magnetite/ilmenite geothermometer and oxygen barometer, Abstracts of American Geophysical Union 1985 Spring Meeting, 1985. 
Andersen, D. J. and Lindsley, D. H.: Internally consistent solution models for Fe-Mg-Mn-Ti oxides; Fe-Ti oxides, Am. Mineral., 73, 714–726, 1988. 
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Short summary
Lascar volcano, located in northern Chile, is among the most active volcanoes of the Andes. Its activity culminated in the last major explosive eruption in April 1993. We carried out experiments at high temperatures (up to 1050 °C) and pressures (up to 5000 bar) in the lab, and we used a wide variety of geochemical methods to provide comprehensive constraints on the depth and temperature of the magma chamber beneath Lascar volcano.
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