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Programme Monday, March 24
23rd LAK, 2014, Heidelberg Programme 13 Programme Monday, March 24 INF 252, Hörsäle Chemie 18:00– CONFERENCE DESK OPENING 21:00 18:00– ICEBREAKER PARTY 22:00 * Sponsored by DFG travel grants 14 Programme 23rd LAK, 2014, Heidelberg Tuesday I, March 25 INF 252, Hörsaal Ost INF 252, Hörsaal West 09:30 Welcome Christina Ifrim and Wolfgang Stinnesbeck DAAD-Fördermöglichkeiten für Geowissenschaftler aus/nach Lateinamerika Sybilla Tinnap, DAAD, Bonn Talk 141: Funding Opportunities for Scientific and Technological Cooperation: The Role of the Project Management Agency European and International Cooperation International Bureau of the Bmbf Inge Lamberz de Bayas, Internationales Büro, Bundesministerium für Bildung und Forschung, Bonn International Cooperation in DFG-Programmes – Earth Sciences in Latin America Dietrich Halm, DFG, Bonn 11:00 COFFEE BREAK and POSTER SESSION Session 1: The southernmost dinosurs in Latin Session 2: Water America and their environment Chair: Heinrich Adolf Horn Chair: Marcelo Leppe 11:20 Talk 205: Late Cretaceous Terrestrial Biota from Las Talk 132: Nutrient fluxes in the groundwater affecting Chinas-Cerro Guido Complex, Magallanes Region, the northern mangrove coast of the peninsula Yucatán Southern Chile: A Key Area for the Antarctic-South (México) American Biogeography Lisa Krienen, Thomas Rüde, Eduardo Graniel Castro and Antonio Marcelo Leppe, Wolfgang Stinnesbeck, Eberhard Frey, Héctor Cardona Benavides Mansilla, Manfred Vogt, Edwin Gonzalez, Leslie Manriquez, Katherine Cisternas, Maritza Mihoc and Toshiro Jujihara -
Investigation of the Effects of Nazca-South America
Investigation of the Effects of Nazca-South America Plate Collision along the Peruvian-Chilean Active Continental Margin through Teleseismic Receiver Function Analysis Item Type text; Electronic Dissertation Authors Bishop, Brandon Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 10/10/2021 22:07:29 Link to Item http://hdl.handle.net/10150/627698 INVESTIGATION OF THE EFFECTS OF NAZCA-SOUTH AMERICA PLATE COLLISION ALONG THE PERUVIAN-CHILEAN ACTIVE CONTINENTAL MARGIN THROUGH TELESEISMIC RECEIVER FUNCTION ANALYSIS by Brandon T. Bishop __________________________ Copyright © Brandon T. Bishop 2018 A Dissertation Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College THE UNIVERSITY OF ARIZONA 2018 STATEMENT BY AUTHOR This dissertation has been submitted in partial fulfillment of the requirements for an advanced degree at the University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this dissertation are allowable without special permission, provided that an accurate acknowledgement of the source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his or her judgment the proposed use of the material is in the interests of scholarship. -
Event History of the Santiago Area (Chile): the Sedimentological Archive of Lago Lo Encañado
Event History of the Santiago area (Chile): the sedimentological archive of Lago Lo Encañado Thomas Pille 1 2 Acknowledgements Om te beginnen zou ik graag mijn promotor, Prof. Dr. Marc De Batist, bedanken voor dit interessante onderwerp en voor de tijd die u hierin gestoken hebt, voor de snelle verbeteringen en de veelbetekende tips en commentaren. Ook Maarten, mijn begeleider, verdient een welgemeende bedanking. Terwijl je het dit jaar zelf heel druk had (een doctoraat dat afgemaakt moest worden, je eerste kindje, een nieuw onderzoeksproject) vond je toch altijd de tijd om mij bij te staan. Vooral je enthousiasme en je doorzettingsvermogen zullen me bijblijven. Voor ieder klein vraagje waarmee ik kwam waren we een paar uur bezig, en vertrok ik niet enkel met een antwoord, maar ook met een hoofd vol extra ideeën. Philipp, obwohl ich ursprünglich nicht dein Thesis-Student war, hast du in der Abwesenheit von Maarten sehr viel Zeit in mein Project investiert. Was mir vor allem gefallen hat war das du bei einer Frage nicht einfach die Antwort gegeben hast, sondern auch versucht hast mir das Prinzip dahinter zu erklären. Vielen Dank für al deine Hilfe, und für eine schöne Reise nach Brest. Ich wünsche dir alles Gute bei deiner Doktorarbeit. I would also like to thank the rest of the RCMG staff, especially to Thomas, Mario, Willem, Oscar, Stan, Katrien and Koen. You were always there to help me if needed, or for a chat during a coffee break. The RCMG is a fantastic working environment. Mijn familie heeft er dit jaar (en eigenlijk doorheen mijn 5-jarige universitaire carrier) altijd voor mij gestaan. -
A Pliocene Mega-Tsunami Deposit and Associated Features in the Ranquil Formation, Southern Chile ⁎ J.P
A Pliocene mega-tsunami deposit and associated features in the Ranquil Formation, southern Chile ⁎ J.P. Le Roux a, , Sven N. Nielsen b,1, Helga Kemnitz b, Álvaro Henriquez a a Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Casilla 13518, Correo 21, Santiago, Chile b GeoForschungsZentrum Potsdam, Section 3.1, Telegrafenberg, 14473 Potsdam, Germany Abstract An exceptionally large tsunami affected the coastline of southern Chile during the Pliocene. Its backflow eroded coarse beach and coastal dune sediments and redistributed them over the continental shelf and slope. Sandstone dykes and sills injected from the base of the resulting hyperconcentrated flow into underlying cohesive muds, assisted in plucking up large blocks of the latter and incorporating them into the flow. Locally, the rip-up intraclasts were fragmented further by smaller-scale injections to form a distinct breccia of angular to rounded mudstone clasts within a medium to coarse sandstone matrix. Sandstone sills in places mimic normal sedimentary beds, complete with structures resembling inverse gradation, planar laminae, as well as ripple and trough cross-lamination. These were probably formed by internal sediment flow and shear stress as the semi-liquefied sand was forcefully injected into cracks. In borehole cores, such sills can easily be misinterpreted as normal sedimentary beds, which can have important implications for hydrocarbon exploration. Keywords: Tsunami; Sandstone dykes; Debris flow; Mimic sedimentary structures; Eltanin impact; Hydrocarbon reservoirs 1. Introduction associated sedimentological features including large rip-up clasts and well rounded basement boulders incorporated in- The west coast of South America has a narrow shelf and to the debris, as well as sand injection from the base of the steep continental slope into a deep subduction trench. -
Pore-Water in Marine Sediments Associated to Gas Hydrate Dissociation Offshore Lebu, Chile. Carolina Cárcamo1,2, Iván Vargas-C
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-362 Manuscript under review for journal Hydrol. Earth Syst. Sci. Discussion started: 29 August 2018 c Author(s) 2018. CC BY 4.0 License. 1 Pore-water in marine sediments associated to gas hydrate dissociation 2 offshore Lebu, Chile. 3 4 Carolina Cárcamo1,2, Iván Vargas-Cordero1, Francisco Fernandoy1, Umberta 5 Tinivella3, Diego López-Acevedo4, Joaquim P. Bento5, Lucía Villar-Muñoz6, Nicole 6 Foucher1, Marion San Juan1, Alessandra Rivero1 7 8 1 Universidad Andres Bello, Facultad de Ingeniería, Quillota 980, Viña del Mar, Chile 9 2 Centro de Investigación Marina Quintay. CIMARQ. Facultad de Ciencias de la Vida. Universidad 10 Andres Bello, Viña del Mar, Chile. 11 3 OGS Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Borgo Grotta Gigante 42/C, 12 34010, Sgonico, Italy. 13 4 Universidad de Concepción, Departamento de Oceanografía, Programa COPAS Sur-Austral, 14 Campus Concepción Víctor Lamas 1290, P.O. Box 160-C, Concepción, Chile 15 5 Escuela de Ciencias del Mar, Pontificia Universidad Católica de Valparaíso, Av. Altamirano 1480, 16 2360007 Valparaíso, Chile. 17 6 GEOMAR Helmholtz Centre for Ocean Research, Wischhofstr. 1-3, 24148 Kiel, Germany. 18 19 ABSTRACT 20 Gas hydrate occurrences along the Chilean margin has been documented, but the 21 processes associated to fluid escapes originated by gas hydrate dissociation yet are 22 unknown. Here, we report morphologies growing related to fluid migration in the 23 continental shelf offshore western Lebu (37 °S) by analysing mainly geochemical 24 features. In this study oxygen and deuterium stable water isotopes in pore water 25 were measured. -
Redalyc.Depositional Environment of Stelloglyphus Llicoensis Isp. Nov
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Le Roux, Jacobus P.; Nielsen, Sven N.; Henríquez, Álvaro Depositional environment of Stelloglyphus llicoensis isp. nov.: a new radial trace fossil from the Neogene Ranquil Formation, south-central Chile Andean Geology, vol. 35, núm. 2, julio, 2008, pp. 307-319 Servicio Nacional de Geología y Minería Santiago, Chile Disponible en: http://www.redalyc.org/articulo.oa?id=173918441006 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Revista Geológica de Chile 35 (2): 307-319. July, 2008 Revista Geológica de Chile www.scielo.cl/rgch.htm Depositional environment of Stelloglyphus llicoensis isp. nov.: a new radial trace fossil from the Neogene Ranquil Formation, south-central Chile jacobus P. Le Roux1, Sven N. Nielsen2, álvaro Henríquez1 1 Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Casilla 13518, Correo 21, Santiago, Chile. [email protected]; [email protected] 2 Institut für Geowissenschaften, Christian-Albrechts-Universität, Ludewig-Meyn-Str.10, 24118 Kiel, Germany. [email protected] ABSTRACT. Stelloglyphus llicoensis isp. nov. is a large radial, discoidal to ellipsoidal trace fossil with a central shaft and single to bifurcating branches radiating from different levels. A 30 m thick measured section of the Ranquil For- mation at Punta Litre contains an associated trace fossil assemblage including Zoophycos, Chondrites, Phycosiphon, Nereites missouriensis, Lockeia siliquaria, Psammichnites(?), Parataenidium, Ophiomorpha, and Rhizocorallium, some of which reworked the Stelloglyphus traces. -
A Review of Tertiary Climate Changes in Southern South America and the Antarctic Peninsula. Part 1: Oceanic Conditions
Sedimentary Geology 247–248 (2012) 1–20 Contents lists available at SciVerse ScienceDirect Sedimentary Geology journal homepage: www.elsevier.com/locate/sedgeo Review A review of Tertiary climate changes in southern South America and the Antarctic Peninsula. Part 1: Oceanic conditions J.P. Le Roux Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile/Centro de Excelencia en Geotérmia de los Andes, Casilla 13518, Correo 21, Santiago, Chile article info abstract Article history: Oceanic conditions around southern South America and the Antarctic Peninsula have a major influence on cli- Received 11 July 2011 mate patterns in these subcontinents. During the Tertiary, changes in ocean water temperatures and currents Received in revised form 23 December 2011 also strongly affected the continental climates and seem to have been controlled in turn by global tectonic Accepted 24 December 2011 events and sea-level changes. During periods of accelerated sea-floor spreading, an increase in the mid- Available online 3 January 2012 ocean ridge volumes and the outpouring of basaltic lavas caused a rise in sea-level and mean ocean temper- ature, accompanied by the large-scale release of CO . The precursor of the South Equatorial Current would Keywords: 2 fi Climate change have crossed the East Paci c Rise twice before reaching the coast of southern South America, thus heating Tertiary up considerably during periods of ridge activity. The absence of the Antarctic Circumpolar Current before South America the opening of the Drake Passage suggests that the current flowing north along the present western seaboard Antarctic Peninsula of southern South American could have been temperate even during periods of ridge inactivity, which might Continental drift explain the generally warm temperatures recorded in the Southeast Pacific from the early Oligocene to mid- Ocean circulation dle Miocene. -
Impact of the 1960 Major Subduction Earthquake in Northern Patagonia (Chile, Argentina)
ARTICLE IN PRESS Quaternary International 158 (2006) 58–71 Impact of the 1960 major subduction earthquake in Northern Patagonia (Chile, Argentina) Emmanuel Chaprona,b,Ã, Daniel Arizteguic, Sandor Mulsowd, Gustavo Villarosae, Mario Pinod, Valeria Outese, Etienne Juvignie´f, Ernesto Crivellie aRenard Centre of Marine Geology, Ghent University, Ghent, Belgium bGeological Institute, ETH Zentrum, Zu¨rich, Switzerland cInstitute F.A. Forel and Department of Geology and Paleontology, University of Geneva, Geneva, Switzerland dInstituto de Geociencias, Universidad Austral de Chile, Valdivia, Chile eCentro Regional Universitario Bariloche, Universidad Nacional del Comahue, Bariloche, Argentina fPhysical Geography,Universite´ de Lie`ge, Lie`ge, Belgium Available online 7 July 2006 Abstract The recent sedimentation processes in four contrasting lacustrine and marine basins of Northern Patagonia are documented by high- resolution seismic reflection profiling and short cores at selected sites in deep lacustrine basins. The regional correlation of the cores is provided by the combination of 137Cs dating in lakes Puyehue (Chile) and Frı´as (Argentina), and by the identification of Cordon Caulle 1921–22 and 1960 tephras in lakes Puyehue and Nahuel Huapi (Argentina) and in their catchment areas. This event stratigraphy allows correlation of the formation of striking sedimentary events in these basins with the consequences of the May–June 1960 earthquakes and the induced Cordon Caulle eruption along the Liquin˜e-Ofqui Fault Zone (LOFZ) in the Andes. While this catastrophe induced a major hyperpycnal flood deposit of ca. 3 Â 106 m3 in the proximal basin of Lago Puyehue, it only triggered an unusual organic rich layer in the proximal basin of Lago Frı´as, as well as destructive waves and a large sub-aqueous slide in the distal basin of Lago Nahuel Huapi. -
Terrigenous Sediment Supply Along the Chilean Continental Margin: Modern Regional Patterns of Texture and Composition
Geol Rundsch (1998) 87:477-494 © Springer-Verlag 1998 ORIGINAL PAPER F. Lamy · D. Hebbeln · G. Wefer Terrigenous sediment supply along the Chilean continental margin: modern regional patterns of texture and composition Received: 17 April 1998 / Accepted: 2 September 1998 Abstract The regional patterns of texture and composition Chile result in equivalent variations of the continental hy- of modern continental slope and pelagic sediments off drology. Additionally, bathymetric features of the shelf, Chile between 25°S and 43°S reflect the latitudinal seg- slope, and trench vary significantly. All these factors can in- mentation of geological, morphological, and climatic fea- fluence the composition and texture of modern continental tures of the continental hinterland. Grain-size characteris- slope and pelagic sediments west of the Peru–Chile trench. tics are controlled by the grain-size of source rocks, the The purpose of this study was to investigate regional dis- weathering regime, and mode of sediment input (eolian off tribution patterns of mineralogical and grain-size parame- northern Chile vs fluvial further south). Bulk-mineral as- ters in relation to source rocks, weathering regimes, modes semblages reveal a low grade of maturity. Regional varia- of sediment input, and types of deposition. We show that tions are governed by the source-rock composition of the the mineralogy of surface samples along the Chilean conti- different geological terranes and the relative source-rock nental margin is primarily controlled by relative source- contribution of the Coastal Range and Andes, as controlled rock contributions of the different geological terranes in by the continental hydrology. The relative abundance of Chile and only subordinately by varying weathering re- clay minerals is also predominantly influenced by the gimes. -
Andean Flat-Slab Subduction Through Time
Andean flat-slab subduction through time VICTOR A. RAMOS & ANDRE´ S FOLGUERA* Laboratorio de Tecto´nica Andina, Universidad de Buenos Aires – CONICET *Corresponding author (e-mail: [email protected]) Abstract: The analysis of magmatic distribution, basin formation, tectonic evolution and structural styles of different segments of the Andes shows that most of the Andes have experienced a stage of flat subduction. Evidence is presented here for a wide range of regions throughout the Andes, including the three present flat-slab segments (Pampean, Peruvian, Bucaramanga), three incipient flat-slab segments (‘Carnegie’, Guan˜acos, ‘Tehuantepec’), three older and no longer active Cenozoic flat-slab segments (Altiplano, Puna, Payenia), and an inferred Palaeozoic flat- slab segment (Early Permian ‘San Rafael’). Based on the present characteristics of the Pampean flat slab, combined with the Peruvian and Bucaramanga segments, a pattern of geological processes can be attributed to slab shallowing and steepening. This pattern permits recognition of other older Cenozoic subhorizontal subduction zones throughout the Andes. Based on crustal thickness, two different settings of slab steepening are proposed. Slab steepening under thick crust leads to dela- mination, basaltic underplating, lower crustal melting, extension and widespread rhyolitic volcan- ism, as seen in the caldera formation and huge ignimbritic fields of the Altiplano and Puna segments. On the other hand, when steepening affects thin crust, extension and extensive within-plate basaltic flows reach the surface, forming large volcanic provinces, such as Payenia in the southern Andes. This last case has very limited crustal melt along the axial part of the Andean roots, which shows incipient delamination. -
Evidence for an Early-Middle Miocene Age of the Navidad Formation (Central Chile): Paleontological, Climatic and Tectonic Implications’ of Gutiérrez Et Al
Andean Geology 41 (3): 657-669. September, 2014 Andean Geology doi: 10.5027/andgeoV41n3-a0810.5027/andgeoV40n2-a?? formerly Revista Geológica de Chile www.andeangeology.cl REPLY TO COMMENT Reply to Comment of Encinas et al. (2014) on: ‘Evidence for an Early-Middle Miocene age of the Navidad Formation (central Chile): Paleontological, climatic and tectonic implications’ of Gutiérrez et al. (2013, Andean Geology 40 (1): 66-78) Jacobus P. Le Roux1, Néstor M. Gutiérrez1, Luis F. Hinojosa2, Viviana Pedroza1, Juan Becerra1 1 Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile-Centro de Excelencia en Geotermia de los Andes, Plaza Ercilla 803, Santiago, Chile. [email protected]; [email protected]; [email protected]; [email protected] 2 Laboratorio de Paleoecología, Facultad de Ciencias-Instituto de Ecología y Biodiversidad (IEB), Universidad de Chile, Las Palmeras 3425, Santiago, Chile. [email protected] Debate in science is always good because it forces Encinas (2006) on a specimen of Neogloboquadrina both parties to re-examine the available evidence, acostaensis, but now Encinas et al. (2014) accuse which can often be interpreted in more than one way. us of contradicting ourselves when we ‘admit that In this case, it seems as if we are at least getting a Gutiérrez et al. (2013) did not mention the Sr date, little bit closer in our interpretation of paleowater because it was too old’. We never admitted anything depths for the Navidad Formation, as Encinas et al. of the sort, as our remark referred to Encinas (2006), (2014) now ‘suspect that some of the sandstone strata not ourselves. -
Gas Hydrate Versus Seabed Morphology Offshore Lebu
www.nature.com/scientificreports OPEN Gas hydrate versus seabed morphology ofshore Lebu (Chilean margin) Iván Vargas‑Cordero1*, Umberta Tinivella2, Lucía Villar‑Muñoz3,4, Joaquim P. Bento5, Carolina Cárcamo6, Diego López‑Acevedo5, Francisco Fernandoy6, Alessandra Rivero6 & Marion San Juan6,7 Gas‑hydrate occurrences along the Chilean margin have been widely documented, but the processes associated with fuid escapes caused by the dissociation of gas hydrates are still unknown. We report a seabed morphology growth related to fuid migration ofshore Lebu associated with mud cones by analysing oxygen and deuterium stable water isotopes in pore water, bathymetric, biological and sedimentological data. A relief was observed at − 127 m water depth with fve peaks. Enrichment values of δ18O (0.0–1.8‰) and δD (0.0–5.6‰) evidenced past hydrate melting. The orientation of the relief could be associated with faults and fractures, which constitute pathways for fuid migration. The benthic foraminifera observed can be associated with cold seep areas. We model that the mud cones correspond to mud growing processes related to past gas‑hydrate dissociation. The integration of (i) the seismic data analysis performed in the surrounding area, (ii) the orientation of our studied relief, (iii) the infaunal foraminifera observed, (iv) the grain size and (v) the total organic matter and isotope values revealed that this area was formerly characterised by the presence of gas hydrates. Hence, this part of the Chilean margin represents a suitable area for investigating fuid‑migration processes. Along continental margins, morphological features associated with fuid escapes such as mud volcanoes, mud mounds, pockmarks, seeps, precipitates—carbonates and hydrates-, piping/rills and brine pools have been reported worldwide (e.g.1–7).