Low-δ18O Rhyolites from Yellowstone: Magmatic Evolution Based on Analyses of Zircons and Individual Phenocrysts
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/petrology/article-pdf/42/8/1491/13136189/421491.PDF
Reference74 articles.
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3. Anderson, J. L., Ague, J. J. & Brandon, M. T. (1997). Regional tilt of the Mount Stuart Batholith, Washington, determined using aluminum-in-hornblende barometry; implications for northward translation of Baja British Columbia; discussion and reply. Geological Society of America Bulletin109, 1223–1227.
4. Bacon, C. R., Adami, L. H. & Lanphere, M. A. (1989). Direct evidence for the origin of low-δ18O silicic magmas: quenched samples of a magma chamber’s partially-fused granitoid walls, Crater Lake, Oregon. Earth and Planetary Science Letters96, 199–208.
5. Bacon, C. R., Persing, H. M., Wooden, J. L. & Ireland, T. R. (2000). Late Pleistocene granodiorite beneath Crater Lake caldera, Oregon, dated by ion microprobe. Geology28, 467–470.
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