Applications of a simplified equation of state for the density of silicate hydrous magmas: The Volcán de Colima (Mexico) buoyancy-driven dome growth process. Similarities and differences with the Popocatépetl volcano domes

Journal of Volcanology and Geothermal Research

Volumn 205, Issue 1-2, 2011, Pages 17-29

  González Mellado, Alex Onar ^a   De la Cruz Reyna, Servando ^a   Navarro Ochoa, Carlos ^b  

^a UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO   (Mexico)

^b UNIVERSIDAD DE COLIMA   (Mexico)

Author keywords

Colima; Density; Dome growth; Equation of state; Popocat petl; Water contents

Indexed keywords

BUOYANT FORCES; COLIMA; COMPOSITIONAL DIFFERENCE; DISSOLVED WATER; EQUATION OF STATE; GAS PRODUCTIONS; GROWTH PROCESS; HOST ROCKS; ISOSTATIC COMPENSATION; LAVA DOME; ME-XICO; STRUCTURAL DIFFERENCES; TWENTIETH CENTURY; VOLCANIC EDIFICE;

BUOYANCY; DOMES; SILICATES; VOLCANOES; WATER CONTENT;

EQUATIONS OF STATE;

ANDESITE; BUOYANCY; DENSITY; DOME; EQUATION OF STATE; LAVA DOME; MAGMA; SILICATE; TWENTIETH CENTURY; WATER CONTENT;

COLIMA; COLIMA VOLCANO; MEXICO [NORTH AMERICA]; POPOCATEPETL; PUEBLA [MEXICO];

EID: 79960061926     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2011.03.009     Document Type: Article

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