Rapid magma ascent and generation of 230Th excesses in the lower crust at Puyehue–Cordón Caulle, Southern Volcanic Zone, Chile

[1]  J. Cembrano,et al.  Structural controls of volcanism in transversal chains: Resheared faults and neotectonics in the Cordón Caulle Puyehue area (40.5°S), Southern Andes , 2006 .

[2]  B. Marsh Dynamics of Magmatic Systems , 2006 .

[3]  L. Lara,et al.  Magmatic evolution of the Puyehue–Cordón Caulle Volcanic Complex (40° S), Southern Andean Volcanic Zone: From shield to unusual rhyolitic fissure volcanism , 2006 .

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

[5]  A. Lahsen,et al.  Morpho-structural evolution of the CordÓn Caulle geothermal region, Southern Volcanic Zone, Chile : Insights from gravity and 40Ar/39Ar dating , 2005 .

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

[7]  K. Cooper,et al.  226Ra/230Th excess generated in the lower crust: Implications for magma transport and storage time scales , 2005 .

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

[9]  L. Lara,et al.  Rhyodacitic fissure eruption in Southern Andes (Cordón Caulle; 40.5°S) after the 1960 (Mw:9.5) Chilean earthquake: a structural interpretation , 2004 .

[10]  N. Rogers,et al.  Rates and Timescales of Fractional Crystallization from 238U-230Th-226Ra Disequilibria in Trachyte Lavas from Longonot Volcano, Kenya , 2004 .

[11]  M. Dungan,et al.  Partial assimilative recycling of the mafic plutonic roots of arc volcanoes: An example from the Chilean Andes , 2004 .

[12]  J. V. Van Orman,et al.  The 226Ra enrichment in oceanic basalts: Evidence for melt‐cumulate diffusive interaction processes within the oceanic lithosphere , 2004 .

[13]  D. DePaolo,et al.  Steady-state 226Ra/230Th disequilibrium in mantle minerals: Implications for melt transport rates in island arcs , 2003 .

[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]  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 .

[18]  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 .

[19]  F. Pollitz,et al.  Earthquake–Volcano Interactions , 2002 .

[20]  F. Costa,et al.  Evolution of Holocene Dacite and Compositionally Zoned Magma, Volcán San Pedro, Southern Volcanic Zone, Chile , 2002 .

[21]  J. Chmeleff,et al.  Origin of 226Ra–230Th disequilibria in arc lavas from southern Chile and implications for magma transfer time , 2002 .

[22]  M. Reagan,et al.  Multiple subduction components in the mantle wedge: Evidence from eruptive centers in the Central Southern volcanic zone, Chile , 2002 .

[23]  Ren A. Thompson,et al.  Eruptive Stratigraphy of the Tatara–San Pedro Complex, 36°S, Southern Volcanic Zone, Chilean Andes: Reconstruction Method and Implications for Magma Evolution at Long-lived Arc Volcanic Centers , 2001 .

[24]  Hai Cheng,et al.  The half-lives of uranium-234 and thorium-230 , 2000 .

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

[26]  C. Hawkesworth,et al.  226Ra–230Th evidence for multiple dehydration events, rapid melt ascent and the time scales of differentiation beneath the Tonga–Kermadec island arc , 2000 .

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

[28]  J. Brophy,et al.  Sector-zoned augite megacrysts in Aleutian high alumina basalts: implications for the conditions of basalt crystallization and the generation of calc-alkaline series magmas , 1999 .

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

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

[31]  A. Davis,et al.  Ion Microprobe Study of Plagioclase-Basalt Partition Experiments at Natural Concentration Levels of Trace Elements , 1998 .

[32]  C. Hawkesworth,et al.  Constraints on flux rates and mantle dynamics beneath island arcs from Tonga–Kermadec lava geochemistry , 1997, Nature.

[33]  R. Macdonald,et al.  U-series isotopes and destructive plate margin magma genesis in the Lesser Antilles , 1996 .

[34]  M. Parada,et al.  Calbuco Volcano and minor eruptive centers distributed along the Liquiñe-Ofqui Fault Zone, Chile (41°–42° S): contrasting origin of andesitic and basaltic magma in the Southern Volcanic Zone of the Andes , 1995 .

[35]  M. Parada,et al.  Crustal xenoliths from Calbuco Volcano, Andean Southern Volcanic Zone: implications for crustal composition and magma-crust interaction , 1995 .

[36]  G. Wörner,et al.  Evolution of the Laacher See magma chamber: Evidence from SIMS and TIMS measurements of UTh disequilibria in minerals and glasses , 1994 .

[37]  M. Parada,et al.  A contribution to the petrogenesis of Osomo and Calbuco volcanoes, Southern Andes (41°00'-41°30'S): comparative study , 1992 .

[38]  M. Dungan,et al.  The Tatara–San Pedro Volcano, 36 °S, Chile: A Chemically Variable, Dominantly Mafic Magmatic System , 1992 .

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

[40]  P. Schuller,et al.  Uranium-thorium activities and disequilibrium in volcanic rocks from the Andes (33-46°S): petrogenetic constraints and environmental consequences , 1991 .

[41]  J. Morris,et al.  Uranium and 10Be enrichments by fluids in Andean arc magmas , 1990, Nature.

[42]  J. Morris,et al.  The subducted component in island arc lavas: constraints from Be isotopes and B–Be systematics , 1990, Nature.

[43]  R. Harmon,et al.  Crustal sources involved in continental arc magmatism: A case study of volcan Mocho-Choshuenco, southern Chile , 1989 .

[44]  H. M. Roa,et al.  Geochemical variations in Andean basaltic and silicic lavas from the Villarrica-Lanin volcanic chain (39.5° S): an evaluation of source heterogeneity, fractional crystallization and crustal assimilation , 1989 .

[45]  M. Dungan,et al.  The origin and evolution of magmas from the San Pedro-Pellado volcanic complex, S. Chile: multicomponent sources and open system evolution , 1988 .

[46]  M. Condomines,et al.  UThRa radioactive disequilibria and magmatic processes , 1988 .

[47]  W. Hildreth,et al.  Crustal contributions to arc magmatism in the Andes of Central Chile , 1988 .

[48]  D. C. Gerlach,et al.  Recent volcanism in the Puyehue Cordon-Caulle region , 1988 .

[49]  M. Dungan,et al.  Crust-magma interactions and the evolution of arc magmas: The San Pedro–Pellado volcanic complex, southern Chilean Andes , 1987 .

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

[51]  D. C. Gerlach,et al.  Multiple sources for basaltic arc rocks from the southern volcanic zone of the Andes (34°–41°S): Trace element and isotopic evidence for contributions from subducted oceanic crust, mantle, and continental crust , 1986 .

[52]  P. Francis,et al.  Regional O-, Sr-, and Pb-isotope relationships in late Cenozoic calc-alkaline lavas of the Andean Cordillera , 1984, Journal of the Geological Society.

[53]  R. Harmon,et al.  Combined Sr–O isotope relationships and petrogenesis of Andean volcanics of South America , 1983, Nature.

[54]  C. Allègre,et al.  Magmatic evolution of a volcano studied by 230Th-238U disequilibrium and trace elements systematics: The Etna case , 1982 .

[55]  K. Cooper,et al.  magma transport and storage time scales , 2005 .

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

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

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

[59]  F. Frey,et al.  Recent lavas from the Andean volcanic front (33 to 42°S); Interpretations of along-arc compositional variations , 1991 .

[60]  R. Drake,et al.  Geochronology of the Lake Region of south-central Chile (39°-42°S): Preliminary results , 1988 .