Late Cenozoic brittle deformation in the Southern Patagonian Andes: Record of plate coupling/decoupling during variable subduction?
The Andes of southern Patagonia experienced a Miocene shift towards faster and higher angle subduction followed by the approach and collision of the Chile oceanic ridge. We present a kinematic study characterizing palaeostress fields computed from brittle tectonics to better constrain upper crustal...
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Blackwell Publishing Ltd
2018
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| 024 | 7 | |2 scopus |a 2-s2.0-85049345555 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Barberón, V. | |
| 245 | 1 | 0 | |a Late Cenozoic brittle deformation in the Southern Patagonian Andes: Record of plate coupling/decoupling during variable subduction? |
| 260 | |b Blackwell Publishing Ltd |c 2018 | ||
| 270 | 1 | 0 | |m Barberón, V.; IDEAN (Universidad de Buenos Aires-CONICET)Argentina; email: vanesabarberon@yahoo.com.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a The Andes of southern Patagonia experienced a Miocene shift towards faster and higher angle subduction followed by the approach and collision of the Chile oceanic ridge. We present a kinematic study characterizing palaeostress fields computed from brittle tectonics to better constrain upper crustal deformation during this complex scenario. Although previous studies already suggested variable kinematics, it is striking that in a long-lasting subduction environment, the computed palaeostress tensors are mostly strike-slip (55%), while 35% are extensional, and only 10% compressive which are concentrated along a main frontal thrust. Cross-cutting relationships and synsedimentary deformation indicate that a long-lived strike-slip regime was punctuated by a lower Miocene extensional event in the foreland before the main compressional event. The results are discussed in contrasting geodynamic models of plate coupling/decoupling versus direction and rate of convergence of the subducting plate, to explain the main mechanisms that control back-arc deformation. © 2018 John Wiley & Sons Ltd |l eng | |
| 536 | |a Detalles de la financiación: Universidad Nacional de La Plata | ||
| 536 | |a Detalles de la financiación: PIP 2014–2016, A15U02 | ||
| 536 | |a Detalles de la financiación: PICT-2013–1291 | ||
| 536 | |a Detalles de la financiación: Conseil National de la Recherche Scientifique | ||
| 536 | |a Detalles de la financiación: 2Universite de Bourgogne–Franche-Comte, CNRS-UMR6249, Besanc©on cedex, France 3Centro de Investigaciones Geologicas (UNLP-CONICET), La Plata, Argentina 4Facultad de Ciencias Naturales y Museo, Universidad Nacional de la Plata, La Plata, Argentina | ||
| 536 | |a Detalles de la financiación: This work was carried out thanks to the financial support of grants projects Agencia PICT-2013–1291; CONICET PIP 2014–2016 GI directed by M. G.; Argentinian-French ECOS-SUD project A15U02 (C. S., and M. G.), and thanks to the French projects Franco-Suisse (Franche-Comte region), and SYSTER (INSU CNRS) directed by C. S. The authors are grateful to Parques Nacionales of Argentina for permitting access to Perito Moreno and Patagonia National Parks. Special thanks to the park rangers at Lago Belgrano, Comision de Fomento de Hipolito Yrigoyen and the people of Lago Posadas, especially to Luciana and Gendarmerıa for allowing access to outcrops, kind logistical support and assistance. Finally, we want to acknowledge B. Horton and anonymous reviewers who provided significant and constructive comments to improve the manuscript. This is contribution R-223 of the Instituto de Estudios Andinos IDEAN Don Pablo Groeber (UBA-CONICET). | ||
| 593 | |a IDEAN (Universidad de Buenos Aires-CONICET), Buenos Aires, Argentina | ||
| 593 | |a Université de Bourgogne–Franche-Comté, CNRS-UMR6249, Besançon cedex, France | ||
| 593 | |a Centro de Investigaciones Geológicas (UNLP-CONICET), La Plata, Argentina | ||
| 593 | |a Facultad de Ciencias Naturales y Museo, Universidad Nacional de la Plata, La Plata, Argentina | ||
| 690 | 1 | 0 | |a BRITTLE DEFORMATION |
| 690 | 1 | 0 | |a GEODYNAMICS |
| 690 | 1 | 0 | |a PATAGONIA |
| 690 | 1 | 0 | |a PLATE COUPLING/DECOUPLING |
| 690 | 1 | 0 | |a SOUTHERN ANDES |
| 690 | 1 | 0 | |a TECTONICS |
| 690 | 1 | 0 | |a BRITTLE DEFORMATION |
| 690 | 1 | 0 | |a CENOZOIC |
| 690 | 1 | 0 | |a GEODYNAMICS |
| 690 | 1 | 0 | |a PLATE TECTONICS |
| 690 | 1 | 0 | |a STRIKE-SLIP FAULT |
| 690 | 1 | 0 | |a SUBDUCTION |
| 690 | 1 | 0 | |a ANDES |
| 690 | 1 | 0 | |a PATAGONIA |
| 700 | 1 | |a Sue, C. | |
| 700 | 1 | |a Ghiglione, M. | |
| 700 | 1 | |a Ronda, G. | |
| 700 | 1 | |a Aragón, E. | |
| 773 | 0 | |d Blackwell Publishing Ltd, 2018 |g v. 30 |h pp. 296-309 |k n. 4 |p Terra Nova |x 09544879 |t Terra Nova | |
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