Oxygen isotope disequilibrium between quartz and sanidine from the Bandelier Tuff, New Mexico, consistent with a short residence time of phenocrysts in rhyolitic magma

Journal of Volcanology and Geothermal Research

Volumn 116, Issue 1-2, 2002, Pages 119-135

  Wolff, John A ^a   Balsley, Steven D ^b   Gregory, Robert T ^c  

^a WASHINGTON STATE UNIVERSITY   (United States)

^b SANDIA NATIONAL LABORATORIES   (United States)

^c SOUTHERN METHODIST UNIVERSITY   (United States)

Author keywords

Isotopic disequilibrium; Oxygen isotopes; Rhyolite; Valles caldera

Indexed keywords

FELDSPAR; FRACTIONATION; ISOTOPES; QUARTZ;

PHENOCRYSTS;

OXYGEN;

DISEQUILIBRIUM; OXYGEN ISOTOPE; PHENOCRYST; QUARTZ; RESIDENCE TIME; RHYOLITE; SANIDINE;

UNITED STATES;

EID: 0036646902     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0377-0273(02)00214-7     Document Type: Article

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