Rift-relatedtransition from andesite to rhyolitevolcanism in thetaupovolcanic zone (New Zealand) controlled by crystal-melt dynamics in mush zones withvariable mineral assemblages

Journal of Petrology

Volumn 52, Issue 11, 2011, Pages 2243-2263

  Deering, C D ^a   Bachmann, O ^a   Dufek, J ^b   Gravley, D M ^c  

^a UNIVERSITY OF WASHINGTON   (United States)

^b GEORGIA INSTITUTE OF TECHNOLOGY   (United States)

^c UNIVERSITY OF CANTERBURY   (New Zealand)

Author keywords

Andesite; Arc volcanism; Crystal mush; Melt extraction; Rhyolite; Rifting

Indexed keywords

ANDESITE; CHEMICAL ALTERATION; CHEMICAL COMPOSITION; CRUSTAL EVOLUTION; CRYSTALLIZATION; DACITE; FRACTIONATION; IGNEOUS GEOCHEMISTRY; LOWER CRUST; MAGMA CHAMBER; MAGMATIC DIFFERENTIATION; MAGMATISM; MULTIPHASE FLOW; NUMERICAL MODEL; PHENOCRYST; PLAGIOCLASE; REACTION KINETICS; RHYOLITE; RIFT ZONE; VOLCANIC ERUPTION; VOLCANISM;

NEW ZEALAND; NORTH ISLAND; TAUPO VOLCANIC ZONE;

EID: 80755169433     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egr046     Document Type: Article

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