Origin of distinct silicic magma types from the Guachipelín Caldera, NW Costa Rica: Evidence for magma mixing and protracted subvolcanic residence

Journal of Volcanology and Geothermal Research

Volumn 165, Issue 3-4, 2007, Pages 103-126

  Deering, Chad D ^a   Vogel, Thomas A ^a   Patino, Lina C ^a   Alvarado, Guillermo E ^b  

^a MICHIGAN STATE UNIVERSITY   (United States)

^b INSTITUTO COSTARRICENSE DE ELECTRICIDAD   (Costa Rica)

Author keywords

arcs; Central America; Costa Rica; fractional crystallization; mixing; silicic magma

Indexed keywords

CRYSTALLIZATION; GEOCHEMISTRY; IGNEOUS ROCKS; PETROLOGY; TRACE ELEMENTS; VOLCANOES;

FRACTIONAL CRYSTALLIZATION; MAGMA MIXING; SILICIC MAGMA;

SILICA;

CALDERA; DACITE; FRACTIONAL CRYSTALLIZATION; ISLAND ARC; LARGE IGNEOUS PROVINCE; MAGMA; PLEISTOCENE; PYROCLASTIC DEPOSIT; RHYOLITE; VOLCANIC ERUPTION;

CENTRAL AMERICA; COSTA RICA; IZU-BONIN ARC; PACIFIC OCEAN;

EID: 34547729616     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2007.05.004     Document Type: Article

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