Oblique half-graben inversion of the Mesozoic Neuquén Rift in the Malargüe Fold and Thrust Belt, Mendoza, Argentina: New insights from analogue models
The Malargüe fold and thrust belt, located in the Andean mountains between 34°S and 36°30′S, formed in response to contraction during Cenozoic times. Its structural style and geometry was controlled by the Mesozoic rift system that formed the Neuquén basin in west-central Argentina. The rift archite...
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2008
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| LEADER | 17263caa a22014657a 4500 | ||
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| 001 | PAPER-22372 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250211091226.0 | ||
| 008 | 190411s2008 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-45849096069 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Yagupsky, D.L. | |
| 245 | 1 | 0 | |a Oblique half-graben inversion of the Mesozoic Neuquén Rift in the Malargüe Fold and Thrust Belt, Mendoza, Argentina: New insights from analogue models |
| 260 | |c 2008 | ||
| 270 | 1 | 0 | |m Yagupsky, D.L.; Laboratorio de Modelado Geológico (LaMoGe), Universidad de Buenos Aires, Ciudad Universitaria, C1428EHA, Buenos Aires, Argentina; email: daniely@gl.fcen.uba.ar |
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| 504 | |a Yagupsky, D.L., Cristallini, E.O., Zamora, G., Varadé, R., Sistema compresivo sobreimpuesto a un rift oblicuo: aplicaciones en la faja plegada y corrida de Malargüe, Sur de Mendoza (2007) Revista de la Asociación Geológica Argentina, 62 (I), pp. 124-138 | ||
| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a The Malargüe fold and thrust belt, located in the Andean mountains between 34°S and 36°30′S, formed in response to contraction during Cenozoic times. Its structural style and geometry was controlled by the Mesozoic rift system that formed the Neuquén basin in west-central Argentina. The rift architecture in the southern sector of this belt was previously interpreted in terms of the present N-S compressive structural trends, assuming the inversion of pre-existing normal faults with the same orientation. Here, we propose that the NW-SE-trending El Manzano-Liu Cullín lineament, located in the northern termination of the Sierra Azul, reflects the presence of a half-graben master fault in the subsurface. This hypothesis is supported by subsurface data, a balanced cross section, and it is tested using a series of scaled sandbox analogue models. We suggest that the lineament responds to a reactivated NW-trending half-graben fault, hidden by the mainly N-S-trending Andean structures. The proposed orientation is in agreement with the NE-SW extension developed in the Neuquén basin during the Triassic-Early Jurassic. The modeling of the inverted oblique half-graben reveals that the strikes of the main structures of inversion-related belts may often be independent of the orientation of the previously developed extensional system, providing a new perspective for their interpretation. © 2008. |l eng | |
| 536 | |a Detalles de la financiación: Umweltbundesamt | ||
| 536 | |a Detalles de la financiación: Fundación Antorchas | ||
| 536 | |a Detalles de la financiación: Agencia Nacional de Promoción Científica y Tecnológica, PICT 38295 | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas, PIP 5758/05 | ||
| 536 | |a Detalles de la financiación: We wish to thank Repsol-YPF for authorization to publish borehole and seismic data. This study has been supported by CONICET (PIP 5758/05), UBA, Fundación Antorchas and Agencia Nacional de Promoción Científica y Técnica (PICT 38295). Special thanks to Ben Brooks and Phoebe Judge for their useful suggestions and comments. The editor J. Hippertt, and reviewers F. Hongn and F. Storti provided very useful comments that helped to substantially improve the manuscript. | ||
| 593 | |a Laboratorio de Modelado Geológico (LaMoGe), Universidad de Buenos Aires, Ciudad Universitaria, C1428EHA, Buenos Aires, Argentina | ||
| 593 | |a Repsol YPF S.A. Talero 360, 8300 Neuquén, Argentina | ||
| 593 | |a Repsol YPF, Esmeralda 255, Of. 10001E, Buenos Aires, Argentina | ||
| 650 | 1 | 7 | |2 spines |a NEON |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a MENDOZA | |
| 651 | 4 | |a NEUQUEN | |
| 651 | 4 | |a SOUTH AMERICA | |
| 690 | 1 | 0 | |a ANALOGUE MODELING |
| 690 | 1 | 0 | |a MALARGUE FOLD |
| 690 | 1 | 0 | |a OBLIQUE INVERSION |
| 690 | 1 | 0 | |a THRUST BELT |
| 690 | 1 | 0 | |a (1 1 1) ORIENTATION |
| 690 | 1 | 0 | |a CENOZOIC |
| 690 | 1 | 0 | |a CROSS SECTIONING |
| 690 | 1 | 0 | |a EARLY JURASSIC |
| 690 | 1 | 0 | |a FOLD-AND-THRUST BELTS |
| 690 | 1 | 0 | |a HALF-GRABEN |
| 690 | 1 | 0 | |a NORMAL FAULTS |
| 690 | 1 | 0 | |a RIFT SYSTEMS |
| 690 | 1 | 0 | |a STRUCTURAL STYLES |
| 690 | 1 | 0 | |a STRUCTURAL TRENDS |
| 690 | 1 | 0 | |a SUBSURFACE DATA |
| 690 | 1 | 0 | |a TRIASSIC |
| 690 | 1 | 0 | |a COMPUTER NETWORKS |
| 690 | 1 | 0 | |a MATHEMATICAL MODELS |
| 690 | 1 | 0 | |a TECTONICS |
| 690 | 1 | 0 | |a ANALOG MODEL |
| 690 | 1 | 0 | |a FOLD AND THRUST BELT |
| 690 | 1 | 0 | |a GRABEN |
| 690 | 1 | 0 | |a INVERSION TECTONICS |
| 690 | 1 | 0 | |a LINEAMENT |
| 690 | 1 | 0 | |a MESOZOIC |
| 690 | 1 | 0 | |a NORMAL FAULT |
| 690 | 1 | 0 | |a OBLIQUE FAULT |
| 690 | 1 | 0 | |a RIFT ZONE |
| 690 | 1 | 0 | |a RIFTING |
| 690 | 1 | 0 | |a MALARGUE |
| 690 | 1 | 0 | |a CAPSICUM PUBESCENS |
| 700 | 1 | |a Cristallini, Ernesto Osvaldo | |
| 700 | 1 | |a Fantín, J. | |
| 700 | 1 | |a Valcarce, G.Z. | |
| 700 | 1 | |a Bottesi, G. | |
| 700 | 1 | |a Varadé, R. | |
| 773 | 0 | |d 2008 |g v. 30 |h pp. 839-853 |k n. 7 |p J. Struct. Geol. |x 01918141 |w (AR-BaUEN)CENRE-335 |t Journal of Structural Geology | |
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