Crystal scale anatomy of a dying supervolcano: an isotope and geochronology study of individual phenocrysts from voluminous rhyolites of the Yellowstone caldera

[1]  R. Cas,et al.  A reconnaissance of U-Pb zircon ages in the Cerro Galan system, NW Argentina: Prolonged magma residence, crystal recycling, and crustal assimilation , 2011 .

[2]  Kathryn Erin Watts,et al.  Large-volume rhyolite genesis in caldera complexes of the Snake River Plain , 2011 .

[3]  J. Wooden,et al.  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 , 2010 .

[4]  I. Bindeman,et al.  Supereruptions of the Snake River Plain: Two-stage derivation of low-δ18O rhyolites from normal-δ18O crust as constrained by Archean xenoliths , 2010 .

[5]  J. Stix,et al.  Rapid extraction of discrete magma batches from a large differentiating magma chamber: the Central Plateau Member rhyolites, Yellowstone Caldera, Wyoming , 2010 .

[6]  F. Ramos,et al.  Thermochemical evolution of young rhyolites at Yellowstone: Evidence for a cooling but periodically replenished postcaldera magma reservoir , 2009 .

[7]  J. Stix,et al.  Magma Recharge and Crystal Mush Rejuvenation Associated with Early Post-collapse Upper Basin Member Rhyolites, Yellowstone Caldera, Wyoming , 2009 .

[8]  J. Valley,et al.  High precision SIMS oxygen isotope analysis and the effect of sample topography , 2009 .

[9]  A. Kent In-situ analysis of Pb isotope ratios using laser ablation MC-ICP-MS: Controls on precision and accuracy and comparison between Faraday cup and ion counting systems , 2008 .

[10]  D. Stockli,et al.  Eruption and magma crystallization ages of Las Tres Vírgenes (Baja California) constrained by combined 230Th/238U and (U–Th)/He dating of zircon , 2006 .

[11]  J. Dufek,et al.  Lower Crustal Magma Genesis and Preservation: a Stochastic Framework for the Evaluation of Basalt–Crust Interaction , 2005 .

[12]  J. Lowenstern,et al.  Late Pleistocene granodiorite source for recycled zircon and phenocrysts in rhyodacite lava at Crater Lake, Oregon [rapid communication] , 2005 .

[13]  J. Baker,et al.  Pb isotopic analysis of standards and samples using a 207Pb–204Pb double spike and thallium to correct for mass bias with a double-focusing MC-ICP-MS , 2004 .

[14]  M. Reid,et al.  Probing the Accumulation History of the Voluminous Toba Magma , 2004, Science.

[15]  M. Walters,et al.  The Geysers - Cobb Mountain Magma System, California (Part 1): U-Pb zircon ages of volcanic rocks, conditions of zircon crystallization and magma residence times , 2003 .

[16]  J. Valley Oxygen Isotopes in Zircon , 2003 .

[17]  M. Reid,et al.  Time scales of magma storage and differentiation of voluminous high-silica rhyolites at Yellowstone caldera, Wyoming , 2002 .

[18]  J. Valley,et al.  Oxygen isotope study of the Long Valley magma system, California: isotope thermometry and convection in large silicic magma bodies , 2002 .

[19]  J. Obradovich,et al.  Revised ages for tuffs of the Yellowstone Plateau volcanic field: Assignment of the Huckleberry Ridge Tuff to a new geomagnetic polarity event , 2002 .

[20]  J. Valley,et al.  Low-δ18O Rhyolites from Yellowstone: Magmatic Evolution Based on Analyses of Zircons and Individual Phenocrysts , 2001 .

[21]  J. Valley,et al.  Post-caldera volcanism: in situ measurement of U^Pb age and oxygen isotope ratio in Pleistocene zircons from Yellowstone caldera , 2001 .

[22]  J. Valley,et al.  Formation of low-δ18O rhyolites after caldera collapse at Yellowstone, Wyoming, USA , 2000 .

[23]  G. Mahood,et al.  40Ar39Ar geochronology of rhyolites erupted following collapse of the Yellowstone caldera, Yellowstone Plateau volcanic field: implications for crustal contamination , 1996 .

[24]  W. Griffin,et al.  THREE NATURAL ZIRCON STANDARDS FOR U‐TH‐PB, LU‐HF, TRACE ELEMENT AND REE ANALYSES , 1995 .

[25]  Mark S. Ghiorso,et al.  Chemical mass transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures , 1995 .

[26]  J. D. Miller,et al.  Precise U‐Pb ages of Duluth Complex and related mafic intrusions, northeastern Minnesota: Geochronological insights to physical, petrogenetic, paleomagnetic, and tectonomagmatic processes associated with the 1.1 Ga Midcontinent Rift System , 1993 .

[27]  Paul Karl Link,et al.  Regional Geology of Eastern Idaho and Western Wyoming , 1992 .

[28]  W. Hildreth,et al.  Isotopic and chemical evidence concerning the genesis and contamination of basaltic and rhyolitic magma beneath the Yellowstone Plateau Volcanic Field , 1991 .

[29]  H. Taylor Igneous rocks; II, Isotopic case studies of Circumpacific magmatism , 1986 .

[30]  W. Hildreth,et al.  Catastrophic isotopic modification of rhyolitic magma at times of caldera subsidence, Yellowstone Plateau Volcanic Field , 1984 .

[31]  T. M. Harrison,et al.  Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types , 1983 .

[32]  R. L. Christiansen,et al.  Lead and strontium isotopes and related trace elements as genetic tracers in the Upper Cenozoic rhyolite-basalt association of the Yellowstone Plateau volcanic field. , 1982 .

[33]  P. Lipman,et al.  Meteoric Water in Magmas , 1974, Science.

[34]  L. Morgan,et al.  OF THE INTERIOR U . S . GEOLOGICAL SURVEY THE TRACK OF THE YELLOWSTONE HOTSPOT : VOLCANISM , FAULTING , AND UPLIFT by , 2010 .

[35]  J. Valley,et al.  Origin and Evolution of Silicic Magmatism at Yellowstone Based on Ion Microprobe Analysis of Isotopically Zoned Zircons , 2008 .

[36]  K. Putirka,et al.  Minerals, inclusions and volcanic processes , 2008 .

[37]  K. Putirka Introduction to Minerals, Inclusions and Volcanic Processes , 2008 .

[38]  L. Muffler,et al.  Preliminary Assessment of Volcanic and Hydrothermal Hazards in Yellowstone National Park and Vicinity , 2007 .

[39]  J. Lowenstern,et al.  Magma Generation at a Large, Hyperactive Silicic Volcano (Taupo, New Zealand) Revealed by U–Th and U–Pb Systematics in Zircons , 2005 .

[40]  Robert L. Christiansen,et al.  The Quaternary and Pliocene Yellowstone plateau volcanic field of Wyoming, Idaho, and Montana , 2001 .

[41]  E. Watson,et al.  Dissolution, growth and survival of zircons during crustal fusion: kinetic principals, geological models and implications for isotopic inheritance , 1996, Earth and Environmental Science Transactions of the Royal Society of Edinburgh.

[42]  J. Obradovich Geochronology of the Late Cenozoic volcanism of Yellowstone National Park and adjoining areas, Wyoming and Idaho , 1992 .

[43]  H. Taylor,et al.  Stable isotopes in high temperature geological processes , 1986 .