Origin of a silica-oversaturated quartz trachyte-rhyolite suite through combined crustal melting, magma mixing, and fractional crystallization: The Leyva Canyon volcano, Trans-Pecos Magmatic Province, Texas

Journal of Volcanology and Geothermal Research

Volumn 111, Issue 1-4, 2001, Pages 155-182

  White, John Charles ^a,b   Urbanczyk, Kevin M ^b  

^a BAYLOR UNIVERSITY   (United States)

^b SUL ROSS STATE UNIVERSITY   (United States)

Author keywords

Anatexis; Fractional crystallization; Magma mixing; Rhyolite; Trachyte; Trans Pecos Magmatic Province

Indexed keywords

CRYSTALLIZATION; MIXING; SILICON;

VOLCANICLASTIC ROCK;

VOLCANOES;

ANATEXIS; FRACTIONAL CRYSTALLIZATION; MAGMA; OLIGOCENE; RHYOLITE; TRACHYTE; VOLCANISM;

UNITED STATES;

EID: 0035518110     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0377-0273(01)00225-6     Document Type: Article

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