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Petrology and Geochemistry of Volcanic Rocks Behind the Cenozoic Arc Front in the Andean Cordillera, Central Chile (33°50'S) Andean Geology, Vol
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Muñoz, Marcia; Fuentes, Francisco; Vergara, Mario; Aguirre, Luis; Olov Nyström, Jan; Féraud, Gilbert; Demant, Alain Abanico East Formation: petrology and geochemistry of volcanic rocks behind the Cenozoic arc front in the Andean Cordillera, central Chile (33°50'S) Andean Geology, vol. 33, núm. 1, enero, 2006, pp. 109-140 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173918422005 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 Abanico East Formation: petrology and geochemistry of volcanic rocks behind the Cenozoic arc front in the Andean Cordillera, central Chile (33°50'S) Marcia Muñoz Departamento de Geología, Universidad de Chile, Casilla 13518, Correo 21, Santiago, Chile [email protected] Francisco Fuentes [email protected] Mario Vergara [email protected] Luis Aguirre [email protected] Jan Olov Nyström Swedish Museum of Natural History, SE-10405 Stockholm, Sweden [email protected] Gilbert Féraud UMR Géosciences Azur, CNRS-UNSA, Université de Nice- Sophia Antipolis, 06108 Nice Cedex 02, France [email protected] Alain Demant Laboratoire de Pétrologie Magmatique Université Aix-Marseille III, 13397 Marseille Cedex 20, France [email protected] ABSTRACT The stratigraphy, chemistry and age of rocks assigned to the eastern portion of the Abanico Formation exposed along the El Volcán river valley, Principal Cordillera east of Santiago (30º50'S/70º12'-70º5'W), are reported and discussed. -
Supplementary Data
Supplementary data Water sources Places Sites Samples Rivers Vacas, Cuevas, Tupungato and Mendoza 7 42 rivers in Punta de Vacas. Cuevas River in Puente del Inca. Horcones Superior and Horcones rivers at Mt. Aconcagua Confluencia Camp. Ice bodies Horcones Inferior Glacier and Mt. Tolosa 2 34 rock glaciers conglomerate. Groundwaters Vertiente del Inca, La Salada Stream, 6 41 Confluencia Nueva Spring, Confluencia Vieja Spring and geothermal waters of "Copa de Champagne" and "Viejo Túnel", both in "Puente del Inca". Precipitations Collectors at Laguna de Horcones and 2 4 Confluencia Camp, both in the Mt. Aconcagua Park Snow basins Valle Azul, Los Puquios and Santa María 3 33 Table S1 Sampling along the melting period 2013-2014 in Cordillera Principal geological province. Ice body type classification corresponds to the official inventory of glaciers (IANIGLA-ING, 2015a). Sites refers to quantity of sampling sites for each water source Station 2 and MDS HI m3/s Soil MDT °C Air MDT °C DMaxT DMinT °C max-min °C HI Glacier °C streamflow Mean 2.09 7.17 4.90 3.55 0.77 2.72 SD 0.95 3.15 3.35 4.35 3.30 3.02 VC% 45.34 43.90 68.31 122.56 430.53 111.07 Max 4.88 11.60 10.68 11.27 6.41 11.27 Min 0.52 1.35 -3.65 -5.95 -7.28 -5.95 Rock glaciers streamflow MDS Tolosa m3/s Mean 0.02 SD 0.01 VC% 70.80 Max 0.05 Min 0.00 Station 1 Atm Press hPa Air MDT °C DMaxT °C DMinT °C RH% Mean 706.44 11.12 17.82 4.74 37.27 SD 1.55 2.88 3.41 2.66 17.39 VC% 0.22 25.89 19.15 56.17 46.67 Max 710.04 16.57 24.84 11.20 97.60 Min 703.11 2.89 6.25 -0.53 13.60 Station 1 Soil DMT °C Wind Dir.° W mean vel. -
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Index Page numbers in italic denote Figures. Page numbers in bold denote Tables. Abanico extensional basin 2, 4, 68, 70, 71, 72, 420 Andacollo Group 132, 133, 134 basin width analogue modelling 4, 84, 95, 99 Andean margin Abanico Formation 39, 40, 71, 163 kinematic model 67–68 accommodation systems tracts 226, 227, 228, 234, thermomechanical model 65, 67 235, 237 Andean Orogen accretionary prism, Choapa Metamorphic Complex development 1, 3 20–21, 25 deformation 1, 3, 4 Aconcagua fold and thrust belt 18, 41, 69, 70, 72, 96, tectonic and surface processes 1, 3 97–98 elevation 3 deformation 74, 76 geodynamics and evolution 3–5 out-of-sequence structures 99–100 tectonic cycles 13–43 Aconcagua mountain 3, 40, 348, 349 uplift and erosion 7–8 landslides 7, 331, 332, 333, 346–365 Andean tectonic cycle 14,29–43 as source of hummocky deposits 360–362 Cretaceous 32–36 TCN 36Cl dating 363 early period 30–35 aeolian deposits, Frontal Cordillera piedmont 299, Jurassic 29–32 302–303 late period 35–43 Aetostreon 206, 207, 209, 212 andesite aggradation 226, 227, 234, 236 Agrio Formation 205, 206, 207, 209, 210 cycles, Frontal Cordillera piedmont 296–300 Chachahue´n Group 214 Agrio fold and thrust belt 215, 216 Neuque´n Basin 161, 162 Agrio Formation 133, 134, 147–148, 203, Angualasto Group 20, 22, 23 205–213, 206 apatite ammonoids 205, 206–211 fission track dating 40, 71, 396, 438 stratigraphy 33, 205–211 (U–Th)/He thermochronology 40, 75, 387–397 Agua de la Mula Member 133, 134, 205, 211, 213 Ar/Ar age Agua de los Burros Fault 424, 435 Abanico Formation -
Remote Sensing
remote sensing Article Quantitative Assessment of Vertical and Horizontal Deformations Derived by 3D and 2D Decompositions of InSAR Line-of-Sight Measurements to Supplement Industry Surveillance Programs in the Tengiz Oilfield (Kazakhstan) Emil Bayramov 1,2,*, Manfred Buchroithner 3 , Martin Kada 2 and Yermukhan Zhuniskenov 1 1 School of Mining and Geosciences, Nazarbayev University, 53 Kabanbay Batyr Ave, Nur-Sultan 010000, Kazakhstan; [email protected] 2 Methods of Geoinformation Science, Institute of Geodesy and Geoinformation Science, Technical University of Berlin, 10623 Berlin, Germany; [email protected] 3 Institute of Cartography, Helmholtzstr. 10, 01069 Dresden, Germany; [email protected] * Correspondence: [email protected] Abstract: This research focused on the quantitative assessment of the surface deformation veloci- ties and rates and their natural and man-made controlling factors at Tengiz Oilfield in Kazakhstan using the Small Baseline Subset remote sensing technique followed by 3D and 2D decompositions and cosine corrections to derive vertical and horizontal movements from line-of-sight (LOS) mea- Citation: Bayramov, E.; Buchroithner, surements. In the present research we applied time-series of Sentinel-1 satellite images acquired M.; Kada, M.; Zhuniskenov, Y. during 2018–2020. All ground deformation derivatives showed the continuous subsidence at the Quantitative Assessment of Vertical Tengiz oilfield with increasing velocity. 3D and 2D decompositions of LOS measurements to vertical and Horizontal Deformations movement showed that the Tengiz Oil Field 2018–2020 continuously subsided with the maximum Derived by 3D and 2D annual vertical deformation velocity around 70 mm. Based on the LOS measurements, the maximum Decompositions of InSAR annual subsiding velocity was observed to be 60 mm. -
Redalyc.Influence of Depositional Load on the Development of a Shortcut
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Muñoz-Sáez, Carolina; Pinto, Luisa; Charrier, Reynaldo; Nalpas, Thierry Influence of depositional load on the development of a shortcut fault system during the inversion of an extensional basin: The Eocene Oligocene Abanico Basin case, central Chile Andes (33°-35°S) Andean Geology, vol. 41, núm. 1, enero-, 2014, pp. 1-28 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173929668001 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 (1): 1-28. January, 2014 Andean Geology doi: 10.5027/andgeoV41n1-a01 formerly Revista Geológica de Chile www.andeangeology.cl Influence of depositional load on the development of a shortcut fault system during the inversion of an extensional basin: The Eocene-Oligocene Abanico Basin case, central Chile Andes (33°-35°S) Carolina Muñoz-Sáez1, 5, *Luisa Pinto1, 2, Reynaldo Charrier1, 2, 3, Thierry Nalpas4 1 Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Casilla 13518, Correo 21, Santiago, Chile. [email protected] 2 Advanced Mining Technology Center (AMTC), Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Beauchef 850, Santiago. 3 Escuela de Ciencias de la Tierra, Universidad Andrés Bello, Campus República, República 230, Santiago. [email protected] 4 Géosciences Rennes, UMR CNRS 6118-Université de Rennes 1, Campus Beaulieu, 263 Avenue du General Leclerc, 35042 Rennes Cedex, France. -
Geo-Climatic Hazards in the Eastern Subtropical Andes: Distribution, Climate Drivers and Trends Iván Vergara1, Stella M
https://doi.org/10.5194/nhess-2019-381 Preprint. Discussion started: 21 January 2020 c Author(s) 2020. CC BY 4.0 License. Geo-climatic hazards in the eastern subtropical Andes: Distribution, Climate Drivers and Trends Iván Vergara1, Stella M. Moreiras2, 3, Diego Araneo2, 3 and René Garreaud4, 5 1 CONICET-IPATEC, Bariloche, 8400, Argentina 5 2 CONICET-IANIGLA, Mendoza, 5500, Argentina 3 National University of Cuyo, Mendoza, 5502, Argentina 4 University of Chile, Santiago, 8330015, Chile 5 Center for Climate and Resilience Research, Santiago, 8320198, Chile 10 Correspondence to: Iván Vergara ([email protected]) Abstract. Detection and understanding of historical changes in the frequency of geo-climatic hazards (G-CHs) is crucial for the quantification of current hazard and their future projection. Here we focus in the eastern subtropical Andes (32-33° S), using meteorological data and a century-long inventory on 553 G-CHs triggered by rainfall or snowfall. First we analysed their spatio-temporal distributions and the role of climate variability on the year-to-year changes in the number of days with 15 G-CHs. Precipitation is positively correlated with the number of G-CHs across the region and year-round; mean temperature is negatively correlated with snowfall-driven hazards in the western (higher) half of the study region during winter, and with rainfall-driven hazards in the eastern zone during summer. The trends of the G-CHs frequency since the mid-20th century were calculated taking cautions for their non-systematic monitoring. The G-CHs series for the different triggers, zones and seasons were generally stationary. -
Kinematics of the Active West Andean Fold-And-Thrust Belt (Central Chile): Structure and Long-Term Shortening Rate
Kinematics of the active West Andean fold-and-thrust belt (Central Chile): structure and long-term shortening rate M. Riesner1, R. Lacassin1, M. Simoes1, R. Armijo1, R. Rauld 1, 2, * and G. Vargas2 1 Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Univ Paris Diderot, UMR 7154 CNRS, F-75005 Paris, France 2 Dept. de Geofísica, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago, Chile. * Now at Xterrae, Of. 61 Hernando de Aguirre 194, Providencia, Santiago, Chile. Corresponding author: Magali Riesner ([email protected]) Key Points: • 3D structural map and geological cross-section of the WAFTB east of Santiago. • Kinematics of deformation deduced from precise mapping of syn-tectonic Farellones formation. • Long-term shortening rate of 0.1-0.5 mm/yr, with possible deceleration by ~20 Ma. Abstract : West-verging thrusts, synthetic with the Nazca - South America subduction interface, have been recently discovered at the western front of the Andes. At ~33°30’S, the active San Ramón fault stands as the most frontal of these west-verging structures, and represents a major earthquake threat for Santiago, capital city of Chile. Here we elaborate a detailed 3D structural map and a precise cross-section of the West Andean fold-and-thrust belt based on field observations, satellite imagery and previous structural data, together with digital topography. We then reconstruct the evolution of this frontal belt using a trishear kinematic approach. Our reconstruction implies westward propagation of deformation with a total shortening of 9-15 km accumulated over the last 25 Myr. An overall long-term shortening rate of 0.1-0.5 mm/yr is deduced. -
Darwin at Puente Del Inca: Observations on the Formation of the Inca's Bridge and Mountain Building
170 Revista de la Asociación Geológica Argentina 64 (1): 170- 179 (2009) DARWIN AT PUENTE DEL INCA: OBSERVATIONS ON THE FORMATION OF THE INCA'S BRIDGE AND MOUNTAIN BUILDING Victor A. RAMOS Laboratorio de Tectónica Andina, FCEN, Universidad de Buenos Aires - CONICET. Email: [email protected] ABSTRACT The analyses of the observations of Charles Darwin at Puente del Inca, during his second journey across the High Andes drew attention on two different aspects of the geological characteristics of this classic area. Most of his descriptions on the characteristics and the origin of the natural bridge were not published, mainly due to his poor impression of Puente del Inca. However, the application of the uniformitarian principles shows that it was formed as an ice bridge associated with snow and debris avalanches later on cemented by the minerals precipitated by the adjacent hot-water springs. Darwin's observations on the complex structural section at Puente del Inca, together with his findings of shallow water marine fossil mollusks in the thick stratigraphic column of the area interfingered with volcanic rocks, led him to speculate on several geological processes. Based on his geological observations, Darwin argued on the mountain uplift, the subsidence of the marine bottom, the epi- sodic lateral growth of the cordillera, and their association with earthquakes and volcanic activity, which was an important advance in the uniformitarian hypothesis of mountain uplift proposed by Charles Lyell. Darwin was able to recognize the epi- sodic nature of mountain uplift, and based on these premises he concluded that the Andes were still undergoing uplift. -
Debris Flows Occurrence in the Semiarid Central Andes Under Climate Change Scenario
geosciences Review Debris Flows Occurrence in the Semiarid Central Andes under Climate Change Scenario Stella M. Moreiras 1,2,* , Sergio A. Sepúlveda 3,4 , Mariana Correas-González 1 , Carolina Lauro 1 , Iván Vergara 5, Pilar Jeanneret 1, Sebastián Junquera-Torrado 1 , Jaime G. Cuevas 6, Antonio Maldonado 6,7, José L. Antinao 8 and Marisol Lara 3 1 Instituto Argentino de Nivología, Glaciología & Ciencias Ambientales, CONICET, Mendoza M5500, Argentina; [email protected] (M.C.-G.); [email protected] (C.L.); [email protected] (P.J.); [email protected] (S.J.-T.) 2 Catedra de Edafología, Facultad de Ciencias Agrarias, Universidad Nacional de Cuyo, Mendoza M5528AHB, Argentina 3 Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago 8320000, Chile; [email protected] (S.A.S.); [email protected] (M.L.) 4 Instituto de Ciencias de la Ingeniería, Universidad de O0Higgins, Rancagua 2820000, Chile 5 Grupo de Estudios Ambientales–IPATEC, San Carlos de Bariloche 8400, Argentina; [email protected] 6 Centro de Estudios Avanzados en Zonas Áridas (CEAZA), Universidad de La Serena, Coquimbo 1780000, Chile; [email protected] (J.G.C.); [email protected] (A.M.) 7 Departamento de Biología Marina, Universidad Católica del Norte, Larrondo 1281, Coquimbo 1780000, Chile 8 Indiana Geological and Water Survey, Indiana University, Bloomington, IN 47404, USA; [email protected] * Correspondence: [email protected]; Tel.: +54-26-1524-4256 Citation: Moreiras, S.M.; Sepúlveda, Abstract: This review paper compiles research related to debris flows and hyperconcentrated flows S.A.; Correas-González, M.; Lauro, C.; in the central Andes (30◦–33◦ S), updating the knowledge of these phenomena in this semiarid region. -
Where Does the Chilean Aconcagua River Come From? Use of Natural Tracers for Water Genesis Characterization in Glacial and Periglacial Environments
water Article Where Does the Chilean Aconcagua River Come from? Use of Natural Tracers for Water Genesis Characterization in Glacial and Periglacial Environments Sebastián Andrés Crespo 1,* ,Céline Lavergne 2,3 , Francisco Fernandoy 4 , Ariel A. Muñoz 1, Leandro Cara 5 and Simón Olfos-Vargas 1 1 Instituto de Geografía, Facultad de Ciencias del Mar y Geografía, Pontificia Universidad Católica de Valparaíso, Valparaíso 2362807, Chile; [email protected] (A.A.M.); [email protected] (S.O.-V.) 2 Laboratory of Aquatic Environmental Research, Centro de Estudios Avanzados, Universidad de Playa Ancha, Viña del Mar 2581782, Chile; [email protected] 3 HUB Ambiental UPLA, Universidad de Playa Ancha, Valparaíso 234000, Chile 4 Laboratorio de Análisis Isotópico (LAI), Facultad de Ingeniería, Universidad Andrés Bello, Viña del Mar 2531015, Chile; [email protected] 5 Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA-CONICET), Mendoza 5500, Argentina; [email protected] * Correspondence: [email protected] Received: 1 August 2020; Accepted: 12 September 2020; Published: 21 September 2020 Abstract: The Aconcagua river basin (Chile, 32 ◦S) has suffered the effects of the megadrought over the last decade. The severe snowfall deficiency drastically modified the water supply to the catchment headwaters. Despite the recognized snowmelt contribution to the basin, an unknown streamflow buffering effect is produced by glacial, periglacial and groundwater inputs, especially in dry periods. Hence, each type of water source was characterized and quantified for each season, through the combination of stable isotope and ionic analyses as natural water tracers. The δ18O and electric conductivity were identified as the key parameters for the differentiation of each water source. -
Analísis Fitoecológicos Integrado Del Piso Basal Del Valle Del Río De Las
ANÁLISIS FITOECOLÓGICO INTEGRADO DEL PISO BASAL DEL VALLE DEL RÍO DE LAS CUEVAS, MENDOZA, ARGENTINA Moira Alessandro de Rodríguez Instituto de Geografia Universidad Nacional de Cuyo moiraba®yahoo. com.ar Resumen f Este artículo parte de un trabajo mayor, relaciona la distribución del tipo de vegetación con el clima local y el impacto antrópico en el piso basal del valle del río de las Cuevas, Mendoza, Argentina. El clima zonal, orográficamente modificado por la presencia de la cadena montañosa andina, genera la distribución de Adesmia pinifolia y Adesmia aegiceras, tipo de vegetación leñosa arbustiva. Esta vegetación y el escaso suelo en mosaico, sufren un serio deterioro por influencia de las actividades turísticas y de recreación, especialmente por pertenecer a un piso climático infraperiglacial que lo torna muy frágil. Palabras clave: vegetación, valle, altoandino, degradación, geosistema Abstract This article, part of a major investigation, relates the distribution of the type of vegetation, with local climate and the human impact in the low stage of Cuevas river valley, in Mendoza, Argentina. Zonal climate orographycally modified by the presence ·of the Andean range, generales the distribution of Adesmia pinito/la and Adesm/a aegiceras, a wood shrub type of vegetation. This vegetation and its poor and discontinuad soil suffer a serious human impact relatad to tourism and recreation, especially because it's an ecosystem with an under "per glaciar" staga climata, that makas it a vary fragile anvironmant. Key words: vagetation, vallay, highandaan, degradation, geosystem INTRODUCCIÓN Este trabajo es parte de una investigación mayor sobre la fitoecologia del ecosistema de un valle altoandino de Mendoza, Argentina, entre los 30° y 36° de latitud sur (figura 1 ). -
3D Display Techniques for Cartographic Purposes: Semiotic Aspects
Buchroithner, Manfred 3D DISPLAY TECHNIQUES FOR CARTOGRAPHIC PURPOSES: SEMIOTIC ASPECTS Manfred F. Buchroithner*, Robert Schenkel**, Sabine Kirschenbauer*** Dresden University of Technology, Germany Institute of Cartography *[email protected], **[email protected], ***[email protected] KEY WORDS: 3D-Display Techniques, Cartographic Semiotic, Psychological Cues, Cognition ABSTRACT The variety of the cartographic 3D-visualisation is constantly increasing and thereby more and more fields of application are being developed. These facts require that the coherence of technical, perceptive-psychological and cartographic-theoretical aspects has to be subdivided and classified. Through these formulations of interdependence of the single parameters shall be pointed out. The consideration of communication-theoretical and perceptive-theoretical aspects shall lead to a purpose-oriented realisation of the 3D-visualisation techniques according to the user’s necessities. KURZFASSUNG Das thematische Gebiet “Kartographische 3D-Visualisierung”, dessen Vielfältigkeit ständig zunimmt und dem immer mehr Anwendungsbereiche erschlossen werden, erfordert, daß die Zusammenhänge von technisch- verfahrensspezifischen, wahrnehmungspsychologischen und kartographisch-theoretischen Faktoren aufgeschlüsselt und klassifiziert werden. Hierdurch sollen Ansätze einer Interdependanz der einzelnen Parameter aufgezeigt werden. Die Berücksichtigung kommunikationstheoretischer und wahrnehmungstheoretischer Aspekte soll zu einer anwendergerechten