Cenozoic tectonic evolution of the Alto Tunuyán foreland basin above the transition zone between the flat and normal subduction segment (33°30′-34°S), western Argentina
The Alto Tunuyán basin is a Neogene foreland basin located between Cordillera Principal and Cordillera Frontal, from 33°30′ to 34°00′ south latitude. At this latitude, the feature that characterizes the subduction geometry beneath the Andean Cordillera is a transition in the slab dip from nearly hor...
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2001
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| LEADER | 16193caa a22010817a 4500 | ||
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| 001 | PAPER-20534 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205156.0 | ||
| 008 | 190411s2001 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-0035693904 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Giambiagi, L.B. | |
| 245 | 1 | 0 | |a Cenozoic tectonic evolution of the Alto Tunuyán foreland basin above the transition zone between the flat and normal subduction segment (33°30′-34°S), western Argentina |
| 260 | |c 2001 | ||
| 270 | 1 | 0 | |m Giambiagi, L.B.; IANIGLA-CRICYT, Dr. Adrián Lean s/n, Mendoza CP 5500, Argentina; email: lgiambia@lab.cricyt.edu.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Giambiagi, L.B., Interpretación tectónica de los depósitos neógenos de la cuenca de antepaís del Alto Tunuyán, en la región del río Palomares, Cordillera Principal de Mendoza (1999) Asociación Geológica Argentina, Revista, 54 (4), pp. 361-374 | ||
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| 504 | |a Johnson, N.M., Jordan, T.E., Johnsson, P.A., Naeser, C.W., Magnetic polarity stratigraphy, age, and tectonic setting of fluvial sediments in an eastern Andean foreland basin, San Juan Province, Argentina (1986) Foreland Basins, 8, pp. 63-75. , Allen, P., Homewood, P. (Eds.). International Association of Sedimentologists. Special Publication | ||
| 504 | |a Jordan, T.E., Retroarc foreland and related basin (1995) Tectonic of Sedimentary Basins, pp. 331-362. , Spera, C., Ingersoll, R.V. (Eds.). Blackwell Scientific, Cambridge | ||
| 504 | |a Jordan, T.E., Allmendinger, R.W., The Sierras Pampeanas of Argentina: A modern analogue of Laramide deformation (1986) American Journal of Science, 286, pp. 737-764 | ||
| 504 | |a Jordan, T.E., Isacks, B.L., Ramos, V.A., Allmendinger, R.W., Mountain building in the High Andes (1983) Episodes, 3, pp. 20-26 | ||
| 504 | |a Jordan, T.E., Tamm, V., Figueroa, G., Flemming, P.B., Richards, D., Tabbutt, K., Cheatham, T., Development of the Miocene Manantiales foreland basin, Cordillera Principal, San Juan, Argentina (1996) Revista Geológica de Chile, 23 (1), pp. 43-79 | ||
| 504 | |a Kay, S.M., Maksaev, V., Moscoso, R., Mpodozis, C., Nasi, C., Gordillo, C.E., Tertiary Andean magmatism in Chile and Argentina between 28°S and 33°S: Correlation of magmatic chemistry with a changing Benioff zone (1987) Journal of South American Earth Science, 1 (1), pp. 21-38 | ||
| 504 | |a Kozlowski, E., Manceda, R., Ramos, V.A., Estructura (1993) Geología y Recursos Naturales de Mendoza, 1 (18), pp. 235-256. , Ramos, V.A. (Ed.). XII Congreso Geológico Argentino y II Congreso Exploración de Hidrocarburos. Relatorio, Buenos Aires | ||
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| 520 | 3 | |a The Alto Tunuyán basin is a Neogene foreland basin located between Cordillera Principal and Cordillera Frontal, from 33°30′ to 34°00′ south latitude. At this latitude, the feature that characterizes the subduction geometry beneath the Andean Cordillera is a transition in the slab dip from nearly horizontal, north of 33°S, to normal dip, south of 34°S. This particular tectonic setting apparently controlled the Neogene tectonic history of the area. The Neogene sedimentary infill of the basin is represented by the Tunuyán Conglomerate and the Palomares, Butaló, and Papal formations. Thrusting and uplift of the Cordillera Principal began during the early Miocene. Deformation and uplift of the volcanic arc, located on the western part of the thrust belt, produced the sediment source for the lower 200 m of the Tunuyán Conglomerate. As deformation migrated progressively eastward during middle Miocene times, it involved the underlying Mesozoic sequences, the erosion of which provided the material accumulated in the rest of the Tunuyán Conglomerate. The Palomares Formation unconformably overlying the former unit reflects the uplift of Cordillera Frontal. Deposition of the Butaló and Papal formations over the partially deformed broken foreland basin reflects accumulation during a period of tectonic quiescence and low rate of erosion in the eastern part of Cordillera Principal and the western part of Cordillera Frontal. The basement uplift of Cordillera Frontal generated a sticking point that prevented the propagation of the thrust belt toward the foreland. Consequently, out-of-sequence thrusts developed in the Cordillera Principal and the basin was partially cannibalized. © 2001 Elsevier Science Ltd. All rights reserved. |l eng | |
| 536 | |a Detalles de la financiación: Universidad de Buenos Aires, UBACYT TW87 | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas, PIP 4162 | ||
| 536 | |a Detalles de la financiación: We wish to thank Carla Buono, Sergio Orts, Patricio Vazques Calvo, and Emilio Rocha for their help in the field. This research was supported by grants from the University of Buenos Aires (UBACYT TW87) and CONICET (PIP 4162). Special thanks are due to Victor A. Ramos for his comments and discussions. Reviews and suggested improvements by Gustavo Gonzalez Bonorino, Guillermo Re, and Pablo Kraemer are also greatly appreciated. | ||
| 593 | |a Laboratorio de Tectónica Andina, Departamento de Ciencias Geológicas, Universidad de Buenos Aires, Buenos Aires 1428, Argentina | ||
| 593 | |a IANIGLA-CRICYT, Parque General San Martín, Dr Adrian Lean s/n, CP 5500 Mendoza, Argentina | ||
| 690 | 1 | 0 | |a ANDEAN EVOLUTION |
| 690 | 1 | 0 | |a FORELAND BASIN SYSTEM |
| 690 | 1 | 0 | |a TRANSITION SUBDUCTION SEGMENT |
| 690 | 1 | 0 | |a ANDEAN OROGENY |
| 690 | 1 | 0 | |a CENOZOIC |
| 690 | 1 | 0 | |a FORELAND BASIN |
| 690 | 1 | 0 | |a NEOGENE |
| 690 | 1 | 0 | |a SUBDUCTION |
| 690 | 1 | 0 | |a TECTONIC EVOLUTION |
| 651 | 4 | |a ARGENTINA | |
| 700 | 1 | |a Tunik, M.A. | |
| 700 | 1 | |a Ghiglione, M. | |
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