Tectono-stratigraphic evolution of the Andean Orogen between 31 and 37°S (Chile and Western Argentina)
In this classic segment, many tectonic processes, like flat-subduction, terrane accretion and steepening of the subduction, among others, provide a robust framework for their understanding. Five orogenic cycles, with variations in location and type of magmatism, tectonic regimes and development of d...
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Geological Society of London
2015
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| LEADER | 76176caa a22041177a 4500 | ||
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| 001 | PAPER-24872 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205648.0 | ||
| 008 | 190411s2015 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84924854399 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Charrier, R. | |
| 245 | 1 | 0 | |a Tectono-stratigraphic evolution of the Andean Orogen between 31 and 37°S (Chile and Western Argentina) |
| 260 | |b Geological Society of London |c 2015 | ||
| 270 | 1 | 0 | |m Charrier, R.; Departamento de Geología, Universidad de ChileChile |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Ramos, V.A., Caminos, R., Rasgos estructurales del territorio argentino. 1. Evolución tectónica de la Argentina (1999) Geología Argentina, 29, pp. 715-784. , Instituto de Geología y Recursos Naturales, Buenos Aires, Argentina, Anales | ||
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| 504 | |a Ramos, V.A., Aguirre-Urreta, M.B., Álvarez, P.P., (1996) Geología de la Región del Aconcagua, 24. , Dirección Nacional del Servicio Geológico, Buenos Aires, Subsecretaría de Minería de la Nación Anales | ||
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| 504 | |a Wall, R., Selles, D., Gana, P., (1999) Mapa área Tiltil-Santiago, región Metropolitana, , Chile, Servicio Nacional de Geología y Minería | ||
| 504 | |a Wenzel, O., Wathelet, J., Chávez, L., Bonilla, R., La sedimentación cíclica Meso-Cenozoica en la región Carbonífera de Arauco-Concepción, Chile (1975), pp. 215-237. , II Congreso Americano de Geología Económica, Buenos Aires; Wetzel, W., Die Quiriquina Schichten als Sediment und paläontologisches Archiv (1930) Palaeontographica, 73, pp. 49-101 | ||
| 504 | |a Willner, A.P., Pressure-temperature evolution of a Late Palaeozoic paired metamorphic belt in north-central Chile (34-35° 30' S) (2005) Journal of Petrology, 46, pp. 1805-1833 | ||
| 504 | |a Willner, A.P., Glodny, J., Gerya, T.V., Godoy, E., Massonne, H., A counterclockwise PTt path of high-pressure/low-temperature rocks from the Coastal Cordillera accretionary complex of south-central Chile: constraints for the earliest stage of subduction mass flow (2004) Lithos, 75, pp. 283-310 | ||
| 504 | |a Willner, A.P., Thomson, S.N., Kröner, A., Wartho, J.-A., Wijbrans, J.R., Hervé, F., Time markers for the evolution and exhumation history of a Late Palaeozoic paired metamorphic belt in North-Central Chile (34°-35°30'S) (2005) Journal of Petrology, 46, pp. 1835-1858 | ||
| 504 | |a Willner, A.P., Gerdes, A., Massonne, H.J., History of crustal growth and recycling at the Pacific convergent margin of South America at latitudes 29-36°S revealed by a U-Pb and Lu-Hf isotope study of detrital zircon from late Paleozoic accretionary systems (2008) Chemical Geology, 253, pp. 114-129 | ||
| 504 | |a Willner, A.P., Gerdes, A., Massonne, H.-J., Schmidt, A., Sudo, M., Thomson, S.N., Vujovich, G., The geodynamics of collision of a microplate (Chilenia) in Devonian times deduced by the pressure-temperature-time evolution within part of a collisional belt (Guarguaraz Complex, W-Argentina) (2011) Contributions to Mineralogy and Petrology, 162, pp. 303-327 | ||
| 504 | |a Willner, A.P., Massonne, H.-J., Ring, U., Sudo, M., Thomson, S.N., P-T evolution and timing of a late Palaeozoic fore-arc system and its heterogeneous Mesozoic overprint in north-central Chile (latitudes 31-32°S) (2012) Geological Magazine, 149, pp. 177-207 | ||
| 504 | |a Winocur, D.A., Litvak, V.D., Ramos, V.A., Sepúlveda, S.A., Giambiagi, L.B., Moreiras, S.M., Pinto, L., Farías, M., Magmatic and tectonic evolution of the Oligocene Valle del Cura basin, main Andes of Argentina and Chile: evidence for generalized extension (2014) Geodynamic Processes in the Andes of Central Chile and Argentina, 399. , http://dx.doi.org/10.1144/SP399.2, Geological Society, London, Special Publications, First published online February 17, 2014 | ||
| 504 | |a Yáñez, G., Cembrano, S., Pardo, M., Ranero, C., Sellés, D., The Challenger-Juan Fernández-Maipo major tectonic transition of the Nazca-Andean subduction system at 33°-34°S: geodynamic evidence and implications (2001) Journal of South American Earth Sciences, 15, pp. 23-38 | ||
| 504 | |a Yury-Yáñez, R.E., Otero, R.A., Soto-Acuña, S., Suárez, M.E., Rubilar-Rogers, D., Sallaberry, M., First bird remains from the Eocene of Algarrobo, central Chile (2012) Andean Geology, 39, pp. 548-557 | ||
| 520 | 3 | |a In this classic segment, many tectonic processes, like flat-subduction, terrane accretion and steepening of the subduction, among others, provide a robust framework for their understanding. Five orogenic cycles, with variations in location and type of magmatism, tectonic regimes and development of different accretionary prisms, show a complex evolution. Accretion of a continental terrane in the Pampean cycle exhumed lower to middle crust in Early Cambrian. The Ordovician magmatic arc, associated metamorphism and foreland basin formation characterized the Famatinian cycle. In Late Devonian, the collision of Chilenia and associated high-pressure/low-temperature metamorphism contrasts with the late Palaeozoic accretionary prisms. Contractional deformation in Early to Middle Permian was followed by extension and rhyolitic (Choiyoi) magmatism. Triassic to earliest Jurassic rifting was followed by subduction and extension, dominated by Pacific marine ingressions, during Jurassic and Early Cretaceous. The Late Cretaceous was characterized by uplift and exhumation of the Andean Cordillera. An Atlantic ingression occurred in latest Cretaceous. Cenozoic contraction and uplift pulses alternate with Oligocene extension. Late Cenozoic subduction was characterized by the Pampean flat-subduction, the clockwise block tectonic rotations in the normal subduction segments and the magmatism in Payenia. These processes provide evidence that the Andean tectonic model is far from a straightforward geological evolution. © 2015 The Geological Society of London. |l eng | |
| 593 | |a Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile | ||
| 593 | |a Escuela de Ciencias de la Tierra, Universidad Andres Bello, Campus República, Salvador Sanfuentes 357, Santiago, Chile | ||
| 593 | |a Laboratorio de Tectónica Andina, Instituto de Estudios Andinos Don Pablo Groeber, Universidad de Buenos Aires-CONICET, Intendente Güirales 2160, Ciudad Universitaria, Capital Federal, Buenos Aires, C1428EGA, Argentina | ||
| 690 | 1 | 0 | |a ACCRETIONARY PRISM |
| 690 | 1 | 0 | |a ANDEAN OROGENY |
| 690 | 1 | 0 | |a CAMBRIAN |
| 690 | 1 | 0 | |a MAGMATISM |
| 690 | 1 | 0 | |a ORDOVICIAN |
| 690 | 1 | 0 | |a PERMIAN |
| 690 | 1 | 0 | |a SUBDUCTION ZONE |
| 690 | 1 | 0 | |a TECTONIC EVOLUTION |
| 690 | 1 | 0 | |a TECTONIC SETTING |
| 690 | 1 | 0 | |a TECTONOSTRATIGRAPHY |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a CHILE | |
| 700 | 1 | |a Ramos, V.A. | |
| 700 | 1 | |a Tapia, F. | |
| 700 | 1 | |a Sagripanti, L. | |
| 773 | 0 | |d Geological Society of London, 2015 |g v. 399 |h pp. 13-61 |p Geol. Soc. Spec. Publ. |x 03058719 |t Geological Society Special Publication | |
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| 856 | 4 | 0 | |u https://doi.org/10.1144/SP399.20 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_03058719_v399_n_p13_Charrier |y Handle |
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| 999 | |c 85825 | ||