Geochemical variations in the Central Southern Volcanic Zone, Chile (38–43°S): The role of fluids in generating arc magmas
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L. Lara | H. Wehrmann | I. Bindeman | K. Hoernle | J. Gill | G. Jacques | Heidi Wehrmann
[1] D. Garbe‐Schönberg,et al. Volatile (sulphur and chlorine), major, and trace element geochemistry of mafic to intermediate tephras from the Chilean Southern Volcanic Zone (33–43°S) , 2014, International Journal of Earth Sciences.
[2] D. Garbe‐Schönberg,et al. Insights from trace element geochemistry as to the roles of subduction zone geometry and subduction input on the chemistry of arc magmas , 2014, International Journal of Earth Sciences.
[3] D. Pyle,et al. Arc magma compositions controlled by linked thermal and chemical gradients above the subducting slab , 2013 .
[4] S. Kay,et al. Origin of Tertiary to Recent EM- and subduction-like chemical and isotopic signatures in Auca Mahuida region (37°–38°S) and other Patagonian plateau lavas , 2013, Contributions to Mineralogy and Petrology.
[5] D. Garbe‐Schönberg,et al. Across-arc geochemical variations in the Southern Volcanic Zone, Chile (34.5–38.0°S): Constraints on mantle wedge and slab input compositions , 2012 .
[6] W. Rabbel,et al. Seismicity near the slip maximum of the 1960 Mw 9.5 Valdivia earthquake (Chile): Plate interface lock and reactivation of the subducted Valdivia Fracture Zone , 2012 .
[7] W. Rabbel,et al. Seismic velocity structure of the slab and continental plate in the region of the 1960 Valdivia (Chile) slip maximum — Insights into fluid release and plate coupling , 2012 .
[8] D. Garbe‐Schönberg,et al. Along and across arc geochemical variations in NW Central America: Evidence for involvement of lithospheric pyroxenite , 2012 .
[9] K. Haase,et al. On- and off-axis chemical heterogeneities along the South Atlantic Mid-Ocean-Ridge (5–11°S): Shallow or deep recycling of ocean crust and/or intraplate volcanism? , 2011 .
[10] C. Langmuir,et al. Assimilation of the Plutonic Roots of the Andean Arc Controls Variations in U-series Disequilibria at Volcan Llaima, Chile , 2011 .
[11] G. Abers,et al. Subduction factory: 4. Depth-dependent flux of H2O from subducting slabs worldwide , 2011 .
[12] C. Mandeville,et al. Back-arc basalts from the Loncopue graben (Province of Neuquen, Argentina) , 2010 .
[13] A. Kent,et al. Origin of cross‐chain geochemical variation in Quaternary lavas from the northern Izu arc: Using a quantitative mass balance approach to identify mantle sources and mantle wedge processes , 2010 .
[14] G. Franz,et al. Complete recycling of a magmatic arc: evidence from chemical and isotopic composition of Quaternary trench sediments in Chile (36°–40°S) , 2010 .
[15] Takeyoshi Yoshida,et al. Arc Basalt Simulator version 2, a simulation for slab dehydration and fluid‐fluxed mantle melting for arc basalts: Modeling scheme and application , 2009 .
[16] I. Bindeman,et al. New insights into the origin of O–Hf–Os isotope signatures in arc lavas from Tonga–Kermadec , 2009 .
[17] J. Cembrano,et al. The link between volcanism and tectonics in the southern volcanic zone of the Chilean Andes: A review , 2009 .
[18] C. Amante,et al. ETOPO1 arc-minute global relief model : procedures, data sources and analysis , 2009 .
[19] S. Kutterolf,et al. Comparative mass balance of volcanic edifices at the Southern Volcanic Zone of the Andes between 33°S and 46°S , 2011 .
[20] E. Flueh,et al. Upper lithospheric structure of the subduction zone offshore of southern Arauco peninsula, Chile, at ∼38°S , 2008 .
[21] C. Heubeck,et al. Turbidites deposited on Southern Central Chilean seamounts: Evidence for energetic turbidity currents , 2008 .
[22] J. Hermann,et al. Sediment Melts at Sub-arc Depths: an Experimental Study , 2008 .
[23] W. Strauch,et al. Arc-parallel flow in the mantle wedge beneath Costa Rica and Nicaragua , 2008, Nature.
[24] J. Pearce. Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust , 2008 .
[25] I. Bindeman. Oxygen Isotopes in Mantle and Crustal Magmas as Revealed by Single Crystal Analysis , 2008 .
[26] E. Flueh,et al. Alteration of the subducting oceanic lithosphere at the southern central Chile trench–outer rise , 2007 .
[27] J. Bialas,et al. Passive and active seismological study of bending-related faulting and mantle serpentinization at the Middle America trench , 2007 .
[28] J. Blichert‐Toft,et al. Hafnium, neodymium, and strontium isotope and parent‐daughter element systematics in basalts from the plume‐ridge interaction system of the Salas y Gomez Seamount Chain and Easter Microplate , 2007 .
[29] S. Kay,et al. The Somuncura Large Igneous Province in Patagonia: Interaction of a Transient Mantle Thermal Anomaly with a Subducting Slab , 2007 .
[30] Z. Pécskay,et al. Preliminary K/Ar geochronology of the Crater Basalt volcanic field (CBVF), northern Patagonia , 2007 .
[31] 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 .
[32] K. Hoernle,et al. Origin and geochemical evolution of the Madeira-Tore Rise (eastern North Atlantic) , 2006 .
[33] Hans-Jürgen Götze,et al. Three‐dimensional density model of the Nazca plate and the Andean continental margin , 2006 .
[34] Katherine A. Kelley,et al. Mantle melting as a function of water content beneath back-arc basins , 2006 .
[35] M. D’Orazio,et al. Sub-recent volcanism in Northern Patagonia: A tectonomagmatic approach , 2006 .
[36] W. Weinrebe,et al. Tectonic Processes along the Chile Convergent Margin , 2006 .
[37] W. Weinrebe,et al. Relationship between bend‐faulting at trenches and intermediate‐depth seismicity , 2005 .
[38] D. Hilton,et al. The May 2003 eruption of Anatahan volcano, Mariana Islands: Geochemical evolution of a silicic island-arc volcano , 2005 .
[39] J. Eiler,et al. Oxygen isotope evidence for slab melting in modern and ancient subduction zones , 2005 .
[40] Michael J. Carr,et al. Oxygen isotope constraints on the sources of Central American arc lavas , 2005 .
[41] S. Hart,et al. Major and trace element composition of the depleted MORB mantle (DMM) , 2005 .
[42] F. Hauff,et al. Sr‐Nd isotope systematics in 14–28 Ma low‐temperature altered mid‐ocean ridge basalt from the Australian Antarctic Discordance, Ocean Drilling Program Leg 187 , 2005 .
[43] I. N. Bindemana,et al. Oxygen isotope evidence for slab melting in modern and ancient subduction zones , 2005 .
[44] C. Stern. Active Andean volcanism: its geologic and tectonic setting , 2004 .
[45] J. Naranjo,et al. Holocene tephrochronology of the southernmost part (42°30'-45°S) of the Andean Southern Volcanic Zone , 2004 .
[46] J. Naranjo,et al. Geochemistry of Nevado de Longaví Volcano (36.2°S): a compositionally atypical arc volcano in the Southern Volcanic Zone of the Andes , 2004 .
[47] S. Kay,et al. Magmatic sources, setting and causes of Eocene to Recent Patagonian plateau magmatism (36°S to 52°S latitude) , 2004 .
[48] P. Vásquez,et al. Distinguishing crustal recycling and juvenile additions at active continental margins: the Paleozoic to recent compositional evolution of the Chilean Pacific margin (36–41°S) ☆ , 2004 .
[49] M. Dungan,et al. Partial assimilative recycling of the mafic plutonic roots of arc volcanoes: An example from the Chilean Andes , 2004 .
[50] Matthias Hort,et al. Serpentine and the subduction zone water cycle , 2004 .
[51] J. Valley,et al. Volcanic arc of Kamchatka: a province with high-δ18O magma sources and large-scale 18O/16O depletion of the upper crust , 2004 .
[52] J. Morgan,et al. Bending-related faulting and mantle serpentinization at the Middle America trench , 2003, Nature.
[53] Katherine A. Kelley,et al. Composition of altered oceanic crust at ODP Sites 801 and 1149 , 2003 .
[54] L. Rüpke,et al. Are the regional variations in Central American arc lavas due to differing basaltic versus peridotitic slab sources of fluids , 2002 .
[55] J. Blichert‐Toft,et al. Hafnium isotopes in basalts from the southern Mid‐Atlantic Ridge from 40°S to 55°S: Discovery and Shona plume–ridge interactions and the role of recycled sediments , 2002 .
[56] J. Chmeleff,et al. Origin of 226Ra–230Th disequilibria in arc lavas from southern Chile and implications for magma transfer time , 2002 .
[57] M. Reagan,et al. Multiple subduction components in the mantle wedge: Evidence from eruptive centers in the Central Southern volcanic zone, Chile , 2002 .
[58] K. Haase. Geochemical constraints on magma sources and mixing processes in Easter Microplate MORB (SE Pacific): a case study of plume-ridge interaction , 2002 .
[59] 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 .
[60] J. Blundy,et al. SIMS determination of trace element partition coefficients between garnet, clinopyroxene and hydrous basaltic liquids at 2–7.5 GPa and 1080–1200°C , 2000 .
[61] Detlef Angermann,et al. Space-geodetic estimation of the nazca-south america euler vector , 1999 .
[62] E. M. Klein,et al. Age constraints on crustal recycling to the mantle beneath the southern Chile Ridge: He‐Pb‐Sr‐Nd isotope systematics , 1999 .
[63] J. Schilling,et al. Plume‐ridge interactions of the Discovery and Shona mantle plumes with the southern Mid‐Atlantic Ridge (40°‐55°S) , 1999 .
[64] T. Dixon,et al. Space geodetic observations of nazca-south america convergence across the central andes , 1998, Science.
[65] G. Wasserburg,et al. Osmium isotopic compositions and Re–Os concentrations in sulfide globules from basaltic glasses , 1998 .
[66] F. Albarède,et al. “The Lu–Hf isotope geochemistry of chondrites and the evolution of the mantle–crust system”: [Earth Planet. Sci. Lett. 148 (1997) 243–258]1 , 1998 .
[67] T. Plank,et al. Element transport from slab to volcanic front at the Mariana arc , 1997 .
[68] S. Cande,et al. The Chile ridge: A tectonic framework , 1997 .
[69] S. Cande,et al. Southeast Pacific tectonic evolution from Early Oligocene to Present , 1997 .
[70] F. Albarède,et al. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system , 1997 .
[71] W. Bach,et al. Unusually large NbTa depletions in North Chile ridge basalts at 36°50′ to 38°56′S: major element, trace element, and isotopic data , 1996 .
[72] J. Schilling,et al. Mantle heterogeneities beneath the South Atlantic: a NdSrPb isotope study along the Mid-Atlantic Ridge (3°S–46°S) , 1996 .
[73] J. Cembrano,et al. Geochemistry and tectonics of the Chilean Southern Andes basaltic Quaternary volcanism (37-46°S) , 1995 .
[74] M. Kohn,et al. UWG-2, a garnet standard for oxygen isotope ratios: Strategies for high precision and accuracy with laser heating , 1995 .
[75] E. M. Klein,et al. Ocean-ridge basalts with convergent-margin geochemical affinities from the Chile Ridge , 1995, Nature.
[76] D. Lowry,et al. Oxygen isotope composition of mantle peridotite , 1994 .
[77] M. Kurz,et al. Isotope and trace element characteristics of a super-fast spreading ridge: East Pacific rise, 13-23°S , 1994 .
[78] H. Moreno,et al. Two magma types of the high-alumina basalt series of Osorno Volcano, Southern Andes (41°06'S)-Plagioclase dilution effect , 1993 .
[79] Peter A. Cawood,et al. Subalkaline andesite from Valu Fa Ridge, a back-arc spreading center in southern Lau Basin: petrogenesis, comparative chemistry, and tectonic implications , 1991 .
[80] J. Schilling,et al. 87Sr86Sr and REE variations along the Easter Microplate boundaries (south Pacific): Application of multivariate statistical analyses to ridge segmentation , 1991 .
[81] F. Frey,et al. Recent lavas from the Andean volcanic front (33 to 42°S); Interpretations of along-arc compositional variations , 1991 .
[82] J. Morris,et al. Uranium and 10Be enrichments by fluids in Andean arc magmas , 1990, Nature.
[83] C. Stern,et al. Trace-element and Sr, Nd, Pb, and O isotopic composition of Pliocene and Quaternary alkali basalts of the Patagonian Plateau lavas of southernmost South America , 1990 .
[84] J. Morris,et al. The subducted component in island arc lavas: constraints from Be isotopes and B–Be systematics , 1990, Nature.
[85] R. Harmon,et al. Crustal sources involved in continental arc magmatism: A case study of volcan Mocho-Choshuenco, southern Chile , 1989 .
[86] 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 .
[87] B. Hanan,et al. Easter microplate evolution: Pb isotope evidence , 1989 .
[88] W. McDonough,et al. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes , 1989, Geological Society, London, Special Publications.
[89] R. W. Le Maitre,et al. A Classification of igneous rocks and glossary of terms : recommendations of the International Union of Geological Sciences Subcommission on the Systematics of Igneous Rocks , 1989 .
[90] C. Stern,et al. Sr and Nd isotopic and trace element compositions of Quaternary volcanic centers of the Southern Andes , 1988 .
[91] D. C. Gerlach,et al. Recent volcanism in the Puyehue Cordon-Caulle region , 1988 .
[92] W. Hildreth,et al. Crustal contributions to arc magmatism in the Andes of Central Chile , 1988 .
[93] C. Hawkesworth,et al. The Pleistocene-Recent Tonga-Kermadec Arc Lavas: Interpretation of New Isotopic and Rare Earth Data in Terms of a Depleted Mantle Source Model , 1987 .
[94] A. Hofmann,et al. Isotope geochemistry of Pacific Mid‐Ocean Ridge Basalt , 1987 .
[95] E. Ito,et al. The O, Sr, Nd and Pb isotope geochemistry of MORB , 1987 .
[96] H. Newsom,et al. Siderophile and chalcophile element abundances in oceanic basalts, Pb isotope evolution and growth of the Earth's core , 1986 .
[97] A. Hofmann,et al. Nb and Pb in oceanic basalts: new constraints on mantle evolution , 1986 .
[98] B. Hanan,et al. Pb isotope evidence in the South Atlantic for migrating ridge—hotspot interactions , 1986, Nature.
[99] 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 .
[100] J. Macdougall,et al. Sr and Nd isotopes in basalts from the East Pacific Rise: significance for mantle heterogeneity , 1986 .
[101] 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.
[102] B. Hamelin,et al. Lead-strontium isotopic variations along the East Pacific Rise and the Mid-Atlantic Ridge: a comparative study , 1984 .
[103] D. C. Gerlach,et al. Geochemical Variations in Volcanic Rocks from Central-south Chile (33–42°S) , 1984 .
[104] J. Gill. Orogenic Andesites and Plate Tectonics , 1981 .
[105] S. Cande,et al. An active spreading center collides with a subduction zone: A geophysical survey of the Chile Margin triple junction , 1981 .