Contrasting punctuated zircon growth in two syn-erupted rhyolite magmas from Tarawera volcano: Insights to crystal diversity in magmatic systems

Earth and Planetary Science Letters

Volumn 301, Issue 3-4, 2011, Pages 511-520

  Storm, Sonja ^a   Shane, Phil ^a   Schmitt, Axel K ^b   Lindsay, Jan M ^a  

^a UNIVERSITY OF AUCKLAND   (New Zealand)

^b UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

Magma; Rhyolite; Tarawera; Uranium series disequilibrium; Zircon

Indexed keywords

BASALT INTRUSION; CONDUIT SYSTEMS; COOLING TIME; FRACTIONAL CRYSTALLIZATION; GROWTH HISTORY; HIGH SPATIAL RESOLUTION; M-SCALE; MAFIC INTRUSION; MAGMA; MAGMA FLOW; MAGMATIC SYSTEMS; MAGMATISMS; NEW ZEALAND; RHYOLITE; STARTING CONDITIONS; TARAWERA; THERMAL PERTURBATIONS; URANIUM SERIES DISEQUILIBRIUM; ZIRCON CRYSTALS;

CRYSTALLIZATION; DEPTH PROFILING; GRANITE; PARAFFIN WAXES; URANIUM; VOLCANOES; ZIRCON;

SILICATE MINERALS;

BASALT; CHEMICAL COMPOSITION; CRYSTALLIZATION; IGNEOUS INTRUSION; MAFIC ROCK; MAGMA; MAGMATISM; RHYOLITE; URANIUM; VOLCANIC ERUPTION; ZIRCON;

BAY OF PLENTY; MOUNT TARAWERA; NEW ZEALAND; NORTH ISLAND;

EID: 78650548815     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2010.11.034     Document Type: Article

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