The limitations of melting on the reactivation of silicic mushes

Journal of Volcanology and Geothermal Research

Volumn 195, Issue 2-4, 2010, Pages 97-105

  Huber, C ^a   Bachmann, Olivier ^b   Dufek, Josef ^a  

^a GEORGIA INSTITUTE OF TECHNOLOGY   (United States)

^b UNIVERSITY OF WASHINGTON   (United States)

Author keywords

Crystallinity; Intrusion; Magma chamber; Melting; Mush

Indexed keywords

ANALYTICAL MODEL; ANALYTICAL SOLUTIONS; COUPLED PROCESS; CRYSTALLINITIES; HEAT CONDUCTION MODELS; HIGH CRYSTALLINITY; IGNIMBRITES; INTRUSION; KEY PROCESS; MAGMA BODIES; MAGMA CHAMBER; MELTING MODEL; ORDER OF MAGNITUDE; PHASE CHANGE; RHEOLOGICAL TRANSITION; SILICIC MAGMAS; TEMPERATURE BOUNDARY; TEXTURAL FEATURE; THERMAL REACTIVATION;

HEAT CONDUCTION; MATHEMATICAL MODELS;

MELTING;

CRYSTALLINITY; EXPLOSIVE VOLCANISM; HEAT TRANSFER; IGNEOUS INTRUSION; IGNIMBRITE; MAGMA CHAMBER; MELTING; NUMERICAL MODEL; PHASE TRANSITION; REACTIVATION; THERMAL CONVECTION; VOLCANIC ERUPTION;

EID: 77955271445     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2010.06.006     Document Type: Article

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