Crystal scale anatomy of a dying supervolcano: an isotope and geochronology study of individual phenocrysts from voluminous rhyolites of the Yellowstone caldera
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-012-0724-x.pdf
Reference40 articles.
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3. Barth AP, Wooden JL (2010) Coupled elemental and isotopic analyses of polygenetic zircons from granitic rocks by ion microprobe, with implications for melt evolution and the sources of granitic magmas. Chem Geol 277:149–159
4. Bindeman IN, Valley JW (2000) The formation of low-δ18O rhyolites after caldera collapse at Yellowstone, Wyoming, USA. Geology 28:719–722
5. Bindeman IN, Valley JW (2001) Low-δ18O rhyolites from Yellowstone: Magmatic evolution based on analyses of zircons and individual phenocrysts. J Petrol 42:1491–1517
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