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Volumn 42, Issue 8, 2001, Pages 1491-1517

Low-δ18O Rhyolites from Yellowstone: Magmatic evolution based on analyses of zircons and individual phenocrysts

Author keywords

18O 16O; Caldera; Isotope disequilibria; Yellowstone; Zircon

Indexed keywords

ISOTOPIC COMPOSITION; MAGMATISM; OXYGEN; PHENOCRYST; RHYOLITE; ZIRCON;

EID: 0034906540     PISSN: 00223530     EISSN: None     Source Type: Journal    
DOI: 10.1093/petrology/42.8.1491     Document Type: Article
Times cited : (257)

References (74)
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    • Chemical mass-transfer in magmatic processes IV. A revised and internally consistent thermo-dynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressure
    • (1995) Contributions to Mineralogy and Petrology , vol.119 , pp. 197-212
    • Ghiorso, M.S.1    Sack, R.O.2
  • 43
    • 44949288493 scopus 로고
    • Second reply to the comments of R.S.J. Sparks H. E. Huppert, and C. J. N. Wilson on 'evidence for long-residence times of rhyolitic magma in the Long Valley magmatic system: The isotopic record in pre-caldera lavas of Glass Mountain
    • (1990) Earth and Planetary Science Letters , vol.99 , pp. 395-399
    • Mahood, G.A.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.