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Abstract:

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.

Registro:

Documento: Artículo
Título: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
Autor:Bechis, F.; Cristallini, E.O.; Giambiagi, L.B.; Yagupsky, D.L.; Guzmán, C.G.; García, V.H.
Filiación: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
Laboratorio de Modelado Geológico, Instituto de Estudios Andinos (IDEAN), CONICET - Universidad de Buenos Aires, Pabellón 2, Ciudad Universitaria, CP 1428 Buenos Aires, Argentina
Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CONICET, Centro Científico Tecnológico Mendoza, Parque General San Martín, CC 330, CP 5500 Mendoza, Argentina
Instituto de Investigación en Paleobiología y Geología (IIPG), Universidad Nacional de Río Negro, Avenida General Roca 1242, CP 8332 General Roca, Argentina
Palabras clave:Analog modeling; Central Andes; Neuquén basin; Oblique rifting; Structural inheritance; Western Gondwana; continental margin; Gondwana; Jurassic; lithospheric structure; oblique fault; rifting; structural geology; tectonic evolution; tectonic setting; transtension; Triassic; Argentina; Neuquen Basin
Año:2014
Volumen:79
Página de inicio:1
Página de fin:17
DOI: http://dx.doi.org/10.1016/j.jog.2014.04.010
Título revista:Journal of Geodynamics
Título revista abreviado:J. Geodyn.
ISSN:02643707
Registro:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02643707_v79_n_p1_Bechis

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Citas:

---------- APA ----------
Bechis, F., Cristallini, E.O., Giambiagi, L.B., Yagupsky, D.L., Guzmán, C.G. & García, V.H. (2014) . 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. Journal of Geodynamics, 79, 1-17.
http://dx.doi.org/10.1016/j.jog.2014.04.010
---------- CHICAGO ----------
Bechis, F., Cristallini, E.O., Giambiagi, L.B., Yagupsky, D.L., Guzmán, C.G., García, V.H. "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" . Journal of Geodynamics 79 (2014) : 1-17.
http://dx.doi.org/10.1016/j.jog.2014.04.010
---------- MLA ----------
Bechis, F., Cristallini, E.O., Giambiagi, L.B., Yagupsky, D.L., Guzmán, C.G., García, V.H. "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" . Journal of Geodynamics, vol. 79, 2014, pp. 1-17.
http://dx.doi.org/10.1016/j.jog.2014.04.010
---------- VANCOUVER ----------
Bechis, F., Cristallini, E.O., Giambiagi, L.B., Yagupsky, D.L., Guzmán, C.G., García, V.H. 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. J. Geodyn. 2014;79:1-17.
http://dx.doi.org/10.1016/j.jog.2014.04.010