Discriminating assimilants and decoupling deep- vs. shallow-level crystal records at Mount Adams using 238U–230Th disequilibria and Os isotopes

[1]  W. Hildreth,et al.  Isotopic and trace element constraints on the petrogenesis of lavas from the Mount Adams volcanic field, Washington , 2009 .

[2]  D. Hoffmann,et al.  An Inter‐Laboratory Assessment of the Thorium Isotopic Composition of Synthetic and Rock Reference Materials , 2008 .

[3]  D. Hoffmann,et al.  An Inter-Laboratory Assessment of the Th Isotopic Composition of Synthetic and Rock Standards. , 2007 .

[4]  B. Jicha,et al.  Rapid magma ascent and generation of 230Th excesses in the lower crust at Puyehue–Cordón Caulle, Southern Volcanic Zone, Chile , 2006 .

[5]  S. Turner,et al.  Source versus differentiation controls on U-series disequilibria: Insights from Cotopaxi Volcano, Ecuador , 2006 .

[6]  R. Sparks,et al.  The Genesis of Intermediate and Silicic Magmas in Deep Crustal Hot Zones , 2006 .

[7]  J. Blundy,et al.  Rapid decompression-driven crystallization recorded by melt inclusions from Mount St Helens volcano , 2005 .

[8]  B. Jicha,et al.  Not so fast: Contrasting timescales of crystallization and magma storage beneath the Aleutian Island arc , 2005 .

[9]  P. Renne,et al.  The 40Ar/39Ar dating of core recovered by the Hawaii Scientific Drilling Project (phase 2), Hilo, Hawaii , 2005 .

[10]  W. Leeman,et al.  Petrologic constraints on the thermal structure of the Cascades arc , 2005 .

[11]  J. Blundy,et al.  The extent of U-series disequilibria produced during partial melting of the lower crust with implications for the formation of the Mount St. Helens dacites , 2004 .

[12]  G. Rolandi,et al.  Time scales of crystal residence and magma chamber volume from modelling of diffusion profiles in phenocrysts: Vesuvius 1944 , 2004 .

[13]  B. Singer,et al.  40Ar/39Ar and K-Ar chronology of Pleistocene glaciations in Patagonia , 2004 .

[14]  R. Edwards,et al.  Time-scales of Differentiation from Mafic Parents to Rhyolite in North American Continental Arcs , 2003 .

[15]  K. Cooper,et al.  Re-examination of crystal ages in recent Mount St. Helens lavas: Implications for magma reservoir processes , 2003 .

[16]  B. Dupré,et al.  U-TH-PA-RA study of the Kamchatka arc: new constraints on the genesis of arc lavas 1 Associate edito , 2003 .

[17]  F. Costa,et al.  Diffusion coupling between trace and major elements and a model for calculation of magma residence times using plagioclase , 2003 .

[18]  W. Hildreth,et al.  New osmium isotope evidence for intracrustal recycling of crustal domains with discrete ages , 2003 .

[19]  R. George,et al.  Melting processes and fluid and sediment transport rates along the Alaska-Aleutian arc from an integrated U-Th-Ra-Be isotope study , 2003 .

[20]  R. Edwards,et al.  (231Pa/235U)-(230Th/238U) of young mafic volcanic rocks from Nicaragua and Costa Rica and the influence of flux melting on U-series systematics of arc lavas , 2002 .

[21]  C. Johnson,et al.  Osmium isotope constraints on lower crustal recycling and pluton preservation at Lassen Volcanic Center, CA , 2002 .

[22]  T. Elliott,et al.  Crystallization history of rhyolites at Long Valley, California, inferred from combined U-series and Rb-Sr isotope systematics , 2002 .

[23]  G. Wörner,et al.  U-series evidence for crustal involvement and magma residence times in the petrogenesis of Parinacota volcano, Chile , 2000 .

[24]  R. Walker,et al.  Re-Os isotopic systematics of primitive lavas from the Lassen region of the Cascade arc, California , 2000 .

[25]  C. Hawkesworth,et al.  Timescales of destructive plate margin magmatism: new insights from Santorini, Aegean volcanic arc , 2000 .

[26]  C. Hawkesworth,et al.  Plagioclase residence times at two island arc volcanoes (Kameni Islands, Santorini, and Soufriere, St. Vincent) determined by Sr diffusion systematics , 1999 .

[27]  B. Wood,et al.  The role of clinopyroxene in generating U-series disequilibrium during mantle melting , 1999 .

[28]  F. McDermott,et al.  A U-series study of lavas from Kamchatka and the Aleutians: constraints on source composition and melting processes , 1998 .

[29]  J. Knowles,et al.  Melting of a subducting oceanic crust from U–Th disequilibria in austral Andean lavas , 1998, Nature.

[30]  R. Walker,et al.  THE Re-Os ISOTOPE SYSTEM IN COSMOCHEMISTRY AND HIGH-TEMPERATURE GEOCHEMISTRY , 1998 .

[31]  Tom Parsons,et al.  A new view into the Cascadia subduction zone and volcanic arc: Implications for earthquake hazards along the Washington margin , 1998 .

[32]  T. Plank,et al.  Element transport from slab to volcanic front at the Mariana arc , 1997 .

[33]  W. Hildreth,et al.  Recent eruptions of Mount Adams, Washington Cascades, USA , 1997 .

[34]  L. Borg,et al.  The variable role of slab-derived fluids in the generation of a suite of primitive calc-alkaline lavas from the Southernmost Cascades, California , 1997 .

[35]  W. Hildreth,et al.  Primitive magmas at five Cascade volcanic fields; melts from hot, heterogeneous sub-arc mantle , 1997 .

[36]  R. Edwards,et al.  U-series isotope evidence for the origin of continental basalts , 1995 .

[37]  W. Hildreth,et al.  Potassium-argon geochronology of a basalt-andesite-dacite arc system: The Mount Adams volcanic field, Cascade Range of southern Washington , 1994 .

[38]  M. Murrell,et al.  Uranium series and beryllium isotope evidence for an extended history of subduction modification of the mantle below Nicaragua , 1994 .

[39]  A. Volpe.  238U−230Th−226Ra disequilibrium in young Mt. Shasta andesites and dacites , 1992 .

[40]  A. Volpe,et al.  238U230Th226Ra disequilibria in young Mount St. Helens rocks: time constraint for magma formation and crystallization , 1991 .

[41]  N. Rogers,et al.  Compositional Diversity of Late Cenozoic Basalts in a Transect Across the Southern Washington Cascades: Implications for Subduction Zone Magmatism , 1990 .

[42]  D. Sherrod,et al.  Quaternary extrusion rates of the Cascade Range, northwestern United States and southern British Columbia , 1990 .

[43]  R. Miller.  The Mesozoic Rimrock Lake inlier, southern Washington Cascades: Implications for the basement to the Columbia Embayment , 1989 .

[44]  T. Druitt,et al.  Compositional evolution of the zoned calcalkaline magma chamber of Mount Mazama, Crater Lake, Oregon , 1988 .

[45]  R. W. Le Maitre,et al.  A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram , 1986 .

[46]  R. Finkel,et al.  Petrogenesis and 230Th-238U disequilibrium at Mt. Shasta, California, and in the Cascades , 1986 .

[47]  K. Turekian,et al.  The uranium and thorium decay series nuclides in Mt. St. Helens effusives , 1982 .

[48]  R. Steiger,et al.  Subcommission on geochronology: Convention on the use of decay constants in geo- and cosmochronology , 1977 .

[49]  W. Hildreth.  Quaternary magmatism in the Cascades : geologic perspectives , 2007 .

[50]  B. Wood,et al.  Mineral-Melt Partitioning of Uranium, Thorium and Their Daughters , 2003 .

[51]  Pierre-J. Gauthier,et al.  Timescales of Magma Chamber Processes and Dating of Young Volcanic Rocks , 2003 .

[52]  B. Bourdon,et al.  Insights into Magma Genesis at Convergent Margins from U-series Isotopes , 2003 .

[53]  W. Hildreth,et al.  Geologic map of the Mount Adams volcanic field, Cascade Range of southern Washington , 1995 .

[54]  W. Mooney,et al.  Chapter 9: Regional crustal structure and tectonics of the Pacific Coastal States; California, Oregon, and Washington , 1989 .

[55]  P. A. Baedecker.  Methods for geochemical analysis , 1987 .

[56]  M. Clynne,et al.  The application of uranium-thorium systematics to rocks from the Lassen Dome Field, California , 1984 .