Evolution of tuff ring-dome complex: the case study of Cerro Pinto, eastern Trans-Mexican Volcanic Belt

Cerro Pinto is a Pleistocene rhyolite tuff ring-dome complex located in the eastern Trans-Mexican Volcanic Belt. The complex is composed of four tuff rings and four domes that were emplaced in three eruptive stages marked by changes in vent location and eruptive character. During Stage I, vent clear...

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Veröffentlicht in:	Bulletin of volcanology 2010-12, Vol.72 (10), p.1223-1240
Hauptverfasser:	Zimmer, Brian W., Riggs, Nancy R., Carrasco-Núñez, Gerardo
Format:	Artikel
Sprache:	eng
Schlagworte:	Calderas Crystalline rocks Earth and Environmental Science Earth Sciences Earth, ocean, space Engineering and environment geology. Geothermics Exact sciences and technology Explosions Geochemistry Geological hazards Geology Geophysics/Geodesy Igneous and metamorphic rocks petrology, volcanic processes, magmas Igneous rocks Magma Mineralogy Natural hazards: prediction, damages, etc Petrology Pleistocene Research Article Risk assessment Sedimentology Trace elements Volcanic belts Volcanic eruptions Volcanoes Volcanology
Online-Zugang:	Volltext
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