Transtensional tectonics induced by oblique reactivation of previous lithospheric anisotropies during the Late Triassic to Early Jurassic rifting in the Neuquén basin: Insights from analog models
The goal of this study was to determine the main factors that controlled the kinematic evolution and the structural architecture developed during the Late Triassic to Early Jurassic rifting that led to the opening of the Neuquén basin in the southwestern sector of Gondwana. We carried out a series o...
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Elsevier Ltd
2014
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| LEADER | 32164caa a22020057a 4500 | ||
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| 001 | PAPER-24008 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250211090815.0 | ||
| 008 | 190411s2014 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84903725741 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Bechis, F. | |
| 245 | 1 | 0 | |a Transtensional tectonics induced by oblique reactivation of previous lithospheric anisotropies during the Late Triassic to Early Jurassic rifting in the Neuquén basin: Insights from analog models |
| 260 | |b Elsevier Ltd |c 2014 | ||
| 270 | 1 | 0 | |m Bechis, F.; IIDyPCa, CONICET, Universidad Nacional de Río Negro, Mitre 630, 5 piso, CP 8400 San Carlos de Bariloche, Argentina; email: florbechis@gmail.com |
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| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a The goal of this study was to determine the main factors that controlled the kinematic evolution and the structural architecture developed during the Late Triassic to Early Jurassic rifting that led to the opening of the Neuquén basin in the southwestern sector of Gondwana. We carried out a series of analog models to simulate an extensional system with a bent geometry similar to the northeastern border of the basin. In different experiments, we varied the extension direction between NNE (N10°E) and NE (N45°E) orientations, inducing rift systems with different degrees of obliquity in each sector of the extended area. We compared the kinematic evolution and the final structural architecture observed in the experiments with data from two selected representative areas of the basin: (1) the Atuel depocenter, situated in the northern Andean sector, and (2) the Entre Lomas area, situated in the northeastern Neuquén Embayment. In both cases, the good match between the field and subsurface data and the results of the analog models supports a NNE orientation of the regional extension (N30°E-N20°E) during the synrift stage. Our experimental results suggest that lithospheric weakness zones of NNW to NW trend could have controlled and localized the extension in the Neuquén basin. These previous anisotropies were linked to the sutures and rheological contrasts generated during the collision of terranes against the southwestern margin of Gondwana during the Paleozoic, as well as further modifications of the thermo-mechanical state of the lithosphere during the Late Paleozoic to Early Mesozoic evolution. © 2014 Elsevier Ltd. |l eng | |
| 536 | |a Detalles de la financiación: Agencia Nacional de Promoción Científica y Tecnológica, PICT-2010-1441, PICT-2011-1079, PICT-38295, PICT-07-10942 | ||
| 536 | |a Detalles de la financiación: Universidad de Buenos Aires, UBACYT 855 | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas, PIP 5843 | ||
| 536 | |a Detalles de la financiación: This research was funded by Agencia Nacional de Promoción Científica y Tecnológica ( PICT-07-10942 , PICT-38295 , PICT-2010-1441 , PICT-2011-1079 ), Consejo Nacional de Investigaciones Científicas y Técnicas ( PIP 5843 ), and Universidad de Buenos Aires ( UBACYT 855 ). This is the contribution R-133 of the Instituto de Estudios Andinos Don Pablo Goeber (UBA-CONICET). The Editor-In-Chief Wouter Schellart, Joao Duarte and an anonymous reviewer are sincerely thanked for their critical and helpful comments and suggestions. | ||
| 593 | |a Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio (IIDyPCa), CONICET, Universidad Nacional de Río Negro, Mitre 630, CP 8400 San Carlos de Bariloche, Argentina | ||
| 593 | |a Laboratorio de Modelado Geológico, Instituto de Estudios Andinos (IDEAN), CONICET - Universidad de Buenos Aires, Pabellón 2, Ciudad Universitaria, CP 1428 Buenos Aires, Argentina | ||
| 593 | |a Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CONICET, Centro Científico Tecnológico Mendoza, Parque General San Martín, CC 330, CP 5500 Mendoza, Argentina | ||
| 593 | |a Instituto de Investigación en Paleobiología y Geología (IIPG), Universidad Nacional de Río Negro, Avenida General Roca 1242, CP 8332 General Roca, Argentina | ||
| 651 | 4 | |a NEUQUEN BASIN | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a NEUQUEN BASIN | |
| 690 | 1 | 0 | |a ANALOG MODELING |
| 690 | 1 | 0 | |a CENTRAL ANDES |
| 690 | 1 | 0 | |a OBLIQUE RIFTING |
| 690 | 1 | 0 | |a STRUCTURAL INHERITANCE |
| 690 | 1 | 0 | |a WESTERN GONDWANA |
| 690 | 1 | 0 | |a CONTINENTAL MARGIN |
| 690 | 1 | 0 | |a GONDWANA |
| 690 | 1 | 0 | |a JURASSIC |
| 690 | 1 | 0 | |a LITHOSPHERIC STRUCTURE |
| 690 | 1 | 0 | |a OBLIQUE FAULT |
| 690 | 1 | 0 | |a RIFTING |
| 690 | 1 | 0 | |a STRUCTURAL GEOLOGY |
| 690 | 1 | 0 | |a TECTONIC EVOLUTION |
| 690 | 1 | 0 | |a TECTONIC SETTING |
| 690 | 1 | 0 | |a TRANSTENSION |
| 690 | 1 | 0 | |a TRIASSIC |
| 700 | 1 | |a Cristallini, Ernesto Osvaldo | |
| 700 | 1 | |a Giambiagi, L.B. | |
| 700 | 1 | |a Yagupsky, D.L. | |
| 700 | 1 | |a Guzmán, C.G. | |
| 700 | 1 | |a García, V.H. | |
| 773 | 0 | |d Elsevier Ltd, 2014 |g v. 79 |h pp. 1-17 |p J. Geodyn. |x 02643707 |t Journal of Geodynamics | |
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| 961 | |a paper_02643707_v79_n_p1_Bechis |b paper |c PE | ||
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