Pre-eruptive conditions of dacitic magma erupted during the 21.7ka Plinian event at Nevado de Toluca volcano, Central Mexico

Author:

Arce J.L.,Gardner J.E.,Macías J.L.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference47 articles.

1. Internally consistent solution models for Fe–Mg–Mn–Ti oxides: Fe–Ti oxides;Andersen;American Mineralogist,1988

2. QUILF: a PASCAL program to asses equilibria among Fe–Mg–Ti oxides, pyroxenes, olivine, and quartz;Andersen;Computers and Geosciences,1993

3. The 10.5 ka Plinian eruption of Nevado de Toluca volcano, Mexico: stratigraphy and hazard implications;Arce;Geological Society of America Bulletin,2003

4. The 12.1 ka Middle Toluca Pumice: a dacitic Plinian–subplinian eruption of Nevado de Toluca in Central Mexico;Arce;Journal of Volcanology and Geothermal Research,2005

5. A 2.5 ka history of dacitic magmatism at Nevado de Toluca, Mexico: petrological, 40Ar–39Ar dating, and experimental constraints on petrogenesis;Arce;Journal of Petrology,2006

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