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Pritchard, M. E., de Silva, S. L., Michelfelder, G., Zandt, G., McNutt, S. R., Gottsmann, J., West, M. E., Blundy, J., Christensen, D. H., Finnegan, N. J., Minaya, E., Sparks, R. S. J., Sunagua, M., Unsworth, M. J., Alvizuri, C., Comeau, M. J., del Potro, R., Díaz, D., Diez, M., ... Ward, K. M. (2018). Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes. Geosphere, 14(3), 954-982. https://doi.org/10.1130/GES01578.1 Publisher's PDF, also known as Version of record License (if available): CC BY-NC Link to published version (if available): 10.1130/GES01578.1 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Geo Science World at https://doi.org/10.1130/GES01578.1 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Research Paper THEMED ISSUE: PLUTONS: Investigating the Relationship between Pluton Growth and Volcanism in the Central Andes GEOSPHERE Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes GEOSPHERE; v. 14, no. 3 M.E. Pritchard1,2, S.L. de Silva3, G. Michelfelder4, G. Zandt5, S.R. McNutt6, J. Gottsmann2, M.E. West7, J. Blundy2, D.H. -
Redalyc.Geochemistry, U-Pb SHRIMP Zircon Dating and Hf Isotopes of The
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Poma, Stella; Zappettini, Eduardo O.; Quenardelle, Sonia; Santos, João O.; Koukharsky, Magdalena; Belousova, Elena; McNaughton, Neil Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: petrogenesis and geodynamic implications Andean Geology, vol. 41, núm. 2, mayo, 2014, pp. 267-292 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173931252001 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Andean Geology 41 (2): 267-292. May, 2014 Andean Geology doi: 10.5027/andgeoV41n2-a01 formerly Revista Geológica de Chile www.andeangeology.cl Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: petrogenesis and geodynamic implications Stella Poma1, Eduardo O. Zappettini 2, Sonia Quenardelle 1, João O. Santos 3, † Magdalena Koukharsky 1, Elena Belousova 4, Neil McNaughton 3 1 Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires (IGEBA-CONICET), Universidad de Buenos Aires, Facultad de Ciencias Exactas y Naturales, Departamento de Ciencias Geológicas, Pabellón II-Ciudad Universitaria, Intendente Güiraldes 2160, C1428 EGA, Argentina. [email protected]; [email protected] 2 Servicio Geológico Minero Argentino (SEGEMAR), Avda. General Paz 5445, edificio 25, San Martín B1650WAB, Argentina. [email protected] 3 University of Western Australia, 35 Stirling Highway, Crawley WA 6009, Australia. -
Volcán Lascar
Volcán Lascar Región: Antofagasta Provincia: El Loa Comuna: San Pedro de Atacama Coordenadas: 21°22’S – 67°44’O Poblados más cercanos: Talabre – Camar – Socaire Tipo: Estratovolcán Altura: 5.592 m s.n.m. Diámetro basal: 8.9 km Área basal: 62.2 km2 Volumen estimado: 28.5 km3 Última actividad: 2015 Última erupción mayor: 1993 Volcán Lascar. Vista desde el norte Ranking de riesgo (Fotografía: Gabriela Jara, SERNAGEOMIN) 14 específico: Generalidades El volcán Láscar corresponde a un estratovolcán compuesto, elongado en dirección este-oeste, activo desde hace unos 240 ka y emplazado en el margen oeste de la planicie altiplánica. Está conformado por lavas andesíticas, que alcanzan más de 10 km de longitud, y por potentes lavas dacíticas que se extienden hasta 5 km, las que fueron emitidas desde los flancos NO a SO. La lava más reciente se estima en 7 mil años de antigüedad. En los alrededores del volcán se reconocen depósitos de flujo y caída piroclástica, además de numerosos cráteres de impacto asociados a la eyección de bombas durante erupciones plinianas y subplinianas. El principal evento eruptivo durante su evolución se denomina Ignimbrita Soncor, generado hace unos 27 ka al oeste del volcán y con un volumen estimado cercano a los 10 km3. En la cima de este volcán se observan seis cráteres, algunos anidados, y el central de estos se encuentra activo. Registro eruptivo Este volcán ha presentado alrededor de 30 erupciones explosivas desde el siglo XIX, lo que lo convierte en el volcán más activo del norte de Chile. Estos eventos han consistido típicamente en erupciones vulcanianas de corta duración, con emisión de ceniza fina y proyecciones balísticas en un radio de 5 km, donde el último evento de este tipo ocurrió el 30 de octubre del 2015. -
Unraveling the Peruvian Phase of the Central Andes: Stratigraphy, Sedimentology and Geochronology of the Salar De Atacama Basin (22°30-23°S), Northern Chile
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/271538622 Unraveling the Peruvian Phase of the Central Andes: Stratigraphy, sedimentology and geochronology of the Salar de Atacama Basin (22°30-23°S), northern Chile Article in Basin Research · March 2015 DOI: 10.1111/bre.12114 CITATIONS READS 5 127 4 authors: Sebastián Bascuñán Cesar Arriagada University of Chile University of Chile 4 PUBLICATIONS 5 CITATIONS 90 PUBLICATIONS 664 CITATIONS SEE PROFILE SEE PROFILE Jacobus Philippus Le Roux Katja Deckart University of Chile University of Chile 141 PUBLICATIONS 1,668 CITATIONS 28 PUBLICATIONS 610 CITATIONS SEE PROFILE SEE PROFILE All in-text references underlined in blue are linked to publications on ResearchGate, Available from: Jacobus Philippus Le Roux letting you access and read them immediately. Retrieved on: 09 August 2016 EAGE Basin Research (2015) 1–28, doi: 10.1111/bre.12114 Unraveling the Peruvian Phase of the Central Andes: stratigraphy, sedimentology and geochronology of the Salar de Atacama Basin (22°30–23°S), northern Chile Sebastia´ n Bascun˜ a´ n,* Ce´ sar Arriagada,* Jacobus Le Roux*,† and Katja Deckart* *Departamento de Geologıa, Universidad de Chile, Santiago, Chile †Centro de Excelencia en Geotermia de los Andes (CEGA), Universidad de Chile, Santiago, Chile ABSTRACT The Salar de Atacama Basin holds important information regarding the tectonic activity, sedimen- tary environments and their variations in northern Chile during Cretaceous times. About 4000 m of high-resolution stratigraphic columns of the Tonel, Purilactis and Barros Arana Formations reveal braided fluvial and alluvial facies, typical of arid to semi-arid environments, interrupted by scarce intervals with evaporitic, aeolian and lacustrine sedimentation, displaying an overall coarsening- upward trend. -
Sr–Pb Isotopes Signature of Lascar Volcano (Chile): Insight Into Contamination of Arc Magmas Ascending Through a Thick Continental Crust N
Sr–Pb isotopes signature of Lascar volcano (Chile): Insight into contamination of arc magmas ascending through a thick continental crust N. Sainlot, I. Vlastélic, F. Nauret, S. Moune, F. Aguilera To cite this version: N. Sainlot, I. Vlastélic, F. Nauret, S. Moune, F. Aguilera. Sr–Pb isotopes signature of Lascar volcano (Chile): Insight into contamination of arc magmas ascending through a thick continental crust. Journal of South American Earth Sciences, Elsevier, 2020, 101, pp.102599. 10.1016/j.jsames.2020.102599. hal-03004128 HAL Id: hal-03004128 https://hal.uca.fr/hal-03004128 Submitted on 13 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Copyright Manuscript File Sr-Pb isotopes signature of Lascar volcano (Chile): Insight into contamination of arc magmas ascending through a thick continental crust 1N. Sainlot, 1I. Vlastélic, 1F. Nauret, 1,2 S. Moune, 3,4,5 F. Aguilera 1 Université Clermont Auvergne, CNRS, IRD, OPGC, Laboratoire Magmas et Volcans, F-63000 Clermont-Ferrand, France 2 Observatoire volcanologique et sismologique de la Guadeloupe, Institut de Physique du Globe, Sorbonne Paris-Cité, CNRS UMR 7154, Université Paris Diderot, Paris, France 3 Núcleo de Investigación en Riesgo Volcánico - Ckelar Volcanes, Universidad Católica del Norte, Avenida Angamos 0610, Antofagasta, Chile 4 Departamento de Ciencias Geológicas, Universidad Católica del Norte, Avenida Angamos 0610, Antofagasta, Chile 5 Centro de Investigación para la Gestión Integrada del Riesgo de Desastres (CIGIDEN), Av. -
Bianchi, M., Heit, B., Jakovlev, A., Yuan, X., Kay, SM
Originally published as: Bianchi, M., Heit, B., Jakovlev, A., Yuan, X., Kay, S.M., Sandvol, E., Alonso, R.N., Coira, B., Brown, L., Kind, R., Comte, D. (2013): Teleseismic tomography of the southern Puna plateau in Argentina and adjacent regions. ‐ Tectonophysics, 586, 65‐83 DOI: 10.1016/j.tecto.2012.11.016 *Manuscript Click here to download Manuscript: Bianchi-etal.doc Click here to view linked References Teleseismic tomography of the southern Puna plateau in Argentina and adjacent regions 1 2 3 M. Bianchi 1, B. Heit 1,*, A. Jakovlev 2, X. Yuan 1, S. M. Kay 3, E. Sandvol 4, R. N. Alonso 5, B. 4 5 6 Coira 6, R. Kind 1,7 7 8 9 1 Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, 14473 Potsdam, Germany 10 11 12 13 2 Institute of Geology, SB RAS, Novosibirsk, Russia 14 15 16 3 Cornell University, EAS, Snee Hall, Ithaca, NY, 14850. 17 18 19 4 Department of Geological Sciences, University of Missouri, Columbia MO 65211 20 21 22 23 5 Universidad Nacional de Salta, Buenos Aires 177, 4400-Salta, Argentina 24 25 26 6 CONICET, Instituto de Geología y Minería, Universidad Nacional de Jujuy, Avda. Bolivia 1661, 27 28 29 4600-San Salvador de Jujuy, Argentina 30 31 32 7 Freie Universität Berlin, Maltesserstr. 74-100, 12227 Berlin, Germany 33 34 35 36 * Corresponding author, [email protected]. 37 38 39 40 41 42 43 ABSTRACT 44 45 46 An array of 74 seismological stations was deployed in the Argentine Puna and adjacent regions for 47 48 a period of two years. -
Scale Deformation of Volcanic Centres in the Central Andes
letters to nature 14. Shannon, R. D. Revised effective ionic radii and systematic studies of interatomic distances in halides of 1–1.5 cm yr21 (Fig. 2). An area in southern Peru about 2.5 km and chalcogenides. Acta Crystallogr. A 32, 751–767 (1976). east of the volcano Hualca Hualca and 7 km north of the active 15. Hansen, M. (ed.) Constitution of Binary Alloys (McGraw-Hill, New York, 1958). 21 16. Emsley, J. (ed.) The Elements (Clarendon, Oxford, 1994). volcano Sabancaya is inflating with U LOS of about 2 cm yr . A third 21 17. Tanaka, H., Takahashi, I., Kimura, M. & Sobukawa, H. in Science and Technology in Catalysts 1994 (eds inflationary source (with ULOS ¼ 1cmyr ) is not associated with Izumi, Y., Arai, H. & Iwamoto, M.) 457–460 (Kodansya-Elsevier, Tokyo, 1994). a volcanic edifice. This third source is located 11.5 km south of 18. Tanaka, H., Tan, I., Uenishi, M., Kimura, M. & Dohmae, K. in Topics in Catalysts (eds Kruse, N., Frennet, A. & Bastin, J.-M.) Vols 16/17, 63–70 (Kluwer Academic, New York, 2001). Lastarria and 6.8 km north of Cordon del Azufre on the border between Chile and Argentina, and is hereafter called ‘Lazufre’. Supplementary Information accompanies the paper on Nature’s website Robledo caldera, in northwest Argentina, is subsiding with U (http://www.nature.com/nature). LOS of 2–2.5 cm yr21. Because the inferred sources are more than a few kilometres deep, any complexities in the source region are damped Acknowledgements such that the observed surface deformation pattern is smooth. -
AN OCCURRENCE of the ASSEMBLAOE, NATIVE SULFTIR- COVELLITE-"Cu5 6,Fe,S6.S"", AUCANQUILCHA, CHILE Aran H. Cr-Etr&L
THE AMERICAN MINERALOGIST, VOL. 55, MAY_JUNE, 1970 AN OCCURRENCE OF THE ASSEMBLAOE, NATIVE SULFTIR- COVELLITE-"Cu5 6,Fe,S6.s"",AUCANQUILCHA, CHILE AraN H. Cr-etr<, Deportmentof GeologicalSciences, Queen's U niaersity, Kingston, Ontario. AssrnA.cr A mineral with composition near to CusFeSo has been found associated with nzrtive sulfur and covellite in the volcanic sulfur deposit at Aucanquilcha. Microprobe, optical and X-ray powder diffraction data match closell'a previously reported occurrence at Nu- kundamu, Fiji. Comparison with equilibrium synthesis by Kullerud and others indir:ates formation in the temperature range 434-482"C. INrnonucrroN Electron probe microanalysis(L6vy, 1967; Sillitoe and Clark, lt69) of naturally-occurring,supergene idaite has cast considerabledoub1. on the equation (Frenzel, 1959) of this not uncommon sulfi.de with the phaseof generalformula Cur r,Fe,Se.s,1 (Yund, 1963), which has h,een synthesizedby Merwin and Lombard (1937), Roseboomand Kullerud (1958),and Yund and Kullerud (1966).Idaite has been shown to have the compositionCurFeSa, or Cu3FeS4-,1orrd there is as yet no evidence of solid solution in nature between this and more copper-rich comF,osi- tions.The well-establishedX-ray powder data"(a:3.772 A; c:11.1U A; Yund, 1963) for hexagonal Cus.s,Fe"Se.r, are only with difficulty recon- ciled with thoseof natural idaite (Frenzel,1959, 1963), and L6vy (I\167) has suggestedthat Frenzel'soriginal powder data may be adequately fitted to a stannite-type,tetragonal cell. A differencein crystal struclure between thesephases is supported by the dissimilar reflectivity disper- sion profi.lesof natural idaite (L6vy, 1967; Sillitoe and Clark, 1969) and the synthetic "Cu5FeS6"of Merwin and l-ombard (1937; inLlvy, 1967). -
Burns Et Al 2015.Pdf
Earth and Planetary Science Letters 422 (2015) 75–86 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Recording the transition from flare-up to steady-state arc magmatism at the Purico–Chascon volcanic complex, northern Chile ∗ Dale H. Burns a, ,1, Shanaka L. de Silva a, Frank Tepley III a, Axel K. Schmitt b, Matthew W. Loewen a a College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97731, USA b Department of Earth, Planetary, and Space Sciences, University of California at Los Angeles, Los Angeles, CA 90095, USA a r t i c l e i n f o a b s t r a c t Article history: The long-term evolution of continental magmatic arcs is episodic, where a few transient events of high Received 6 December 2014 magmatic flux or flare-ups punctuate the low-flux magmatism or “steady state” that makes up most Received in revised form 31 March 2015 of the arc history. How this duality manifests in terms of differences in crustal architecture, magma Accepted 1 April 2015 dynamics and chemistry, and the time scale over which transitions occur is poorly known. Herein Available online 22 April 2015 we use multiscale geochemical and isotopic characteristics coupled with geothermobarometry at the Editor: T. Mather Purico–Chascon Volcanic Complex (PCVC) in the Central Andes to identify a transition from flare-up to ∼ Keywords: steady state arc magmatism over 800 kyr during which significant changes in upper crustal magmatic Central Andes dynamics are recorded. continental arc evolution The PCVC is one of the youngest volcanic centers related to a 10–1 Ma ignimbrite flare-up in the ignimbrite flare-up Altiplano–Puna Volcanic Complex of the Central Andes. -
Three-Dimensional Resistivity Image of the Magmatic System Beneath
PUBLICATIONS Geophysical Research Letters RESEARCH LETTER Three-dimensional resistivity image of the magmatic system 10.1002/2015GL064426 beneath Lastarria volcano and evidence for magmatic Key Points: intrusion in the back arc (northern Chile) • Electrical resistivity images of the Lastrarria volcano Daniel Díaz1,2, Wiebke Heise3, and Fernando Zamudio1 • The magmatic source is located to the south of Lastarria volcano 1Departamento de Geofísica, Universidad de Chile, Santiago, Chile, 2Centro de Excelencia en Geotermia de Los Andes, • Deep conductor in the back arc 3 suggests magmatic intrusion Santiago, Chile, GNS Science, Lower Hutt, New Zealand Supporting Information: Abstract Lazufre volcanic center, located in the central Andes, is recently undergoing an episode of uplift, • Readme conforming one of the most extensive deforming volcanic systems worldwide, but its magmatic system and • Text S1 • Figure S1 its connection with the observed uplift are still poorly studied. Here we image the electrical resistivity structure • Figure S2 using the magnetotelluric method in the surroundings of the Lastarria volcano, one of the most important • Figure S3 features in the Lazufre area, to understand the nature of the magmatic plumbing, the associated fumarolic • Figure S4 activity, and the large-scale surface deformation. Results from 3-D modeling show a conductive zone at 6 km Correspondence to: depth south of the Lastarria volcano interpreted as the magmatic heat source which is connected to a shallower D. Díaz, conductor beneath the volcano, showing the pathways of volcanic gasses and heated fluid. A large-scale [email protected] conductive area coinciding with the area of uplift points at a magma intrusion at midcrustal depth. -
Actualización Plan Director De Infraestructura Mop
REPÚBLICA DE CHILE MINISTERIO DE OBRAS PÚBLICAS DIRECCIÓN DE PLANEAMIENTO ACTUALIZACIÓN PLAN DIRECTOR DE INFRAESTRUCTURA MOP Informe Final Región de Antofagasta Chile, Noviembre de 2009 INECON, Ingenieros y Economistas Consultores S.A. ÍNDICE 1. CARACTERÍSTICAS DE LA REGIÓN DE ANTOFAGASTA ............................ 1 1.1. Características generales. ............................................................................. 1 1.2. Características económicas. .......................................................................... 1 1.3. Características de la población. ..................................................................... 2 1.4. Gasto histórico en infraestructura por parte del MOP. ...................................... 2 2. IMAGEN OBJETIVO DE LA REGIÓN DE ANTOFAGASTA ............................ 3 2.1. Diagnósticos, objetivos estratégicos y visiones pertinentes. .............................. 3 2.1.1. Estrategia de Desarrollo Regional (EDR) ................................................... 3 2.1.2. Visión 2020- Talleres MOP ..................................................................... 4 2.1.3. Reconocimiento Territorial ...................................................................... 4 2.2. Oportunidades y restricciones de la región. ..................................................... 5 2.2.1. Oportunidades ...................................................................................... 5 2.2.2. Restricciones ....................................................................................... -
The Role of Crustal and Eruptive Processes Versus Source Variations in Controlling the Oxidation State of Iron in Central Andean Magmas ∗ Stephanie B
Earth and Planetary Science Letters 440 (2016) 92–104 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl The role of crustal and eruptive processes versus source variations in controlling the oxidation state of iron in Central Andean magmas ∗ Stephanie B. Grocke a,b, , Elizabeth Cottrell a, Shanaka de Silva b, Katherine A. Kelley c a Smithsonian Institution, National Museum of Natural History, Washington, DC 20560, USA b College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA c Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 20882, USA a r t i c l e i n f o a b s t r a c t Article history: The composition of the continental crust is closely tied to subduction zone magmatism. Elevated oxygen Received 8 July 2015 fugacity ( f O2) plays a central role in fostering crystallization of oxide minerals and thereby aids in Received in revised form 21 January 2016 generating the calc-alkaline trend of iron depletion that characterizes the continents. Along continental Accepted 24 January 2016 margins, arc magmas erupt through continental crust and often undergo extensive differentiation that Available online 22 February 2016 may modify magmatic f O2. The importance of the subducting slab and mantle wedge relative to Editor: T.A. Mather the effects of this differentiation on the f O2 recorded by continental arc magmas remains relatively Keywords: unconstrained. Here, we focus on the effect of differentiation on magmatic f O2 using a suite of 14 Central Andean volcanic zone samples from the Central Volcanic Zone (CVZ) of the Andes where the continental crust is atypically thick crustal assimilation (60–80 km).