Structural evolution of the Andes in a transitional zone between flat and normal subduction (33°30′-33°45′S), Argentina and Chile
The sector of the Andes studied in this paper (33°30′-33°45′S) presents a key region to study the relationship between tectonic setting and deformation history in a transitional zone between flat (north of 33°S) and normal (south of 33°45′S) subduction segments. The Andes at these latitudes are prim...
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2002
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| LEADER | 19479caa a22012377a 4500 | ||
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| 001 | PAPER-20357 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205145.0 | ||
| 008 | 190411s2002 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-0036263398 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Giambiagi, L.B. | |
| 245 | 1 | 0 | |a Structural evolution of the Andes in a transitional zone between flat and normal subduction (33°30′-33°45′S), Argentina and Chile |
| 260 | |c 2002 | ||
| 270 | 1 | 0 | |m Giambiagi, L.B.; Centro Regl. de Invest. Cien./Tec., CONICET, Parque San Martín s/n, Mendoza 5500, Argentina; email: lgiambia@lab.cricyt.edu.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Irigoyen, M.V., Buchan, K.L., Brown, R.L., Magnetostratigraphy of Neogene Andean foreland-basin strata, lat 33°S, Mendoza Province, Argentina (2000) Geological Society of America, Bulletin, 112 (6), pp. 803-816 | ||
| 504 | |a Isacks, B.L., Jordan, T.E., Allmendinger, R.W., Ramos, V.A., La segmentación tectónica de los Andes Centrales y su relación con la geometría de la Placa de Nazca subductada (1982) V Congreso Latinoamericano de Geología, Actas, 3, pp. 587-606. , Buenos Aires | ||
| 504 | |a Jordan, T.E., Isacks, B.L., Allmendinger, R.W., Brewer, J.A., Ramos, V.A., Ando, C.J., Andean tectonics related to geometry of subducted Nazca plate (1983) Geological Society of America Bulletin, 94 (3), pp. 341-361 | ||
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| 520 | 3 | |a The sector of the Andes studied in this paper (33°30′-33°45′S) presents a key region to study the relationship between tectonic setting and deformation history in a transitional zone between flat (north of 33°S) and normal (south of 33°45′S) subduction segments. The Andes at these latitudes are primarily composed of the Neogene Aconcagua fold-and-thrust belt and the basement-block uplift of the Cordillera Frontal. Detailed mapping has revealed that the structure within the inner part of the fold-and-thrust belt resulted from both thin-and thick-skinned tectonic interactions. In the outer part, displacement is transferred to Mesozoic décollement levels, accounting for a thin-skinned architecture. Geographically, the switch from thick- to -thin skinned tectonics occurs near the border between Chile and Argentina. Although the geometry of the subducted Nazca Plate may have influenced the timing and style of deformation in the foreland, plate geometry alone does not adequately explain the style of deformation within the fold-and-thrust belt. Here it is shown that the change in deformation style in the fold-and-thrust belt correlates with the location of pre-existing Mesozoic structure, and specifically that Neogene-age thick-skinned thrusting was controlled by the presence of Mesozoic margin-boundary normal faults. Deformation in this region of the Andean fold-and-thrust belt was thus controlled by a combination of tectonic setting and pre-existing extensional structure. © 2002 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: Agencia Nacional de Promoción Científica y Tecnológica, Pict 07-06729 | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas, PIP 4162 | ||
| 536 | |a Detalles de la financiación: This research was supported by grants from the University of Buenos Aires (UBACYT TW87), ANPCYT (Pict 07-06729), and CONICET (PIP 4162). We wish to thank Maisa Tunik, Carla Buono, Sergio Orts, Patricio Vazques Calvo, Emilio Rocha, Cochi Kim, and Martı́n Pereyra for their help in the field. Special thanks are due to Tomás Zapata, Pirzio Godoy, Leonardo Legarreta and Pamela Alvarez for their comments and discussions; and to Ernesto Cristallini for information about the Cuyo basin. We also thank Brendan McNulty, Alain Lavenu and Brian Horton for their valuable comments, which contributed to the improvement of the manuscript. | ||
| 593 | |a Laboratorido de Tectónica Andina, Universidad de Buenos Aires, Ciudad Universitaria s/n, Buenos Aires 1428, Argentina | ||
| 593 | |a Centro Regional de Investigaciones Científicas y Tecnológicas, CONICET, Parque San Martín s/n, Mendoza 5500, Argentina | ||
| 593 | |a Centro Regional de Investigaciones Científicas y Tecnológicas, CONICET, Parque San Martín s/n, Mendoza 5500, Argentina | ||
| 690 | 1 | 0 | |a ANDES |
| 690 | 1 | 0 | |a FOLD-AND-THRUST BELT |
| 690 | 1 | 0 | |a MESOZOIC ANISOTROPY |
| 690 | 1 | 0 | |a NEOGENE DEFORMATION |
| 690 | 1 | 0 | |a SUBDUCTION |
| 690 | 1 | 0 | |a CRUSTAL DEFORMATION |
| 690 | 1 | 0 | |a FOLD AND THRUST BELT |
| 690 | 1 | 0 | |a STRUCTURAL GEOLOGY |
| 690 | 1 | 0 | |a SUBDUCTION ZONE |
| 690 | 1 | 0 | |a TECTONIC SETTING |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a CHILE | |
| 700 | 1 | |a Ramos, V.A. | |
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