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

✍ Scribed by John A Wolff; Steven D Balsley; Robert T Gregory


Book ID
114244215
Publisher
Elsevier Science
Year
2002
Tongue
English
Weight
641 KB
Volume
116
Category
Article
ISSN
0377-0273

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