Permo-Triassic oblique extension in the Potrerillos-Uspallata area, western Argentina
The Permo-Triassic evolution of southwestern South America was characterized by the development of a great amount of volcanism under extensional conditions. Structural analyses of faults developed contemporaneously with this volcanism in the key area of Potrerillos-Uspallata suggest the existence of...
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2008
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| LEADER | 15232caa a22011177a 4500 | ||
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| 001 | PAPER-22286 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205350.0 | ||
| 008 | 190411s2008 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-55049083369 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Giambiagi, L. | |
| 245 | 1 | 0 | |a Permo-Triassic oblique extension in the Potrerillos-Uspallata area, western Argentina |
| 260 | |c 2008 | ||
| 270 | 1 | 0 | |m Giambiagi, L.; CONICET-IANIGLA Centro Regional de Investigaciones Científicas y Tecnológicas, Parque San Martín s/n, 5500 Mendoza, Argentina; email: lgiambia@lab.cricyt.edu.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a The Permo-Triassic evolution of southwestern South America was characterized by the development of a great amount of volcanism under extensional conditions. Structural analyses of faults developed contemporaneously with this volcanism in the key area of Potrerillos-Uspallata suggest the existence of an oblique extensional setting controlled by the presence of a pre-existing lithospheric anisotropy. A clear parallelism between the trace of an inferred Devonian suture zone, the Late Paleozoic San Rafael orogenic belt and the Permo-Triassic rifting suggests that Early and Late Paleozoic tectonic inheritance permitted the reactivation of a NNW-trending zone of lithospheric weakness. The reactivation of this pre-existing weak zone during Late Permian to Early Triassic times has resulted in the generation of a new complex fault system, which concentrated the oblique-slip normal displacement related to a NNE-SSW stretching (N23°E). © 2008 Elsevier 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, PICT 07-10942 | ||
| 536 | |a Detalles de la financiación: This research was supported by Grants from the University of Buenos Aires (UBACYT TW87) and CONICET (PICT 07-10942). We gratefully acknowledge the use of Richard Allmendinger’s FaultKinWin program and Ernesto Cristallini´s Estereografica GR program. Special thanks are due to Natalia Marchese, Guillermo Peralta, Cristian Guerra, Diego Márquez, Diego Di Carlo and Ezequiel García Morabito for their help in the field. | ||
| 593 | |a CONICET-IANIGLA Centro Regional de Investigaciones Científicas y Tecnológicas, Parque San Martín s/n, 5500 Mendoza, Argentina | ||
| 593 | |a Laboratorio de Tectónica Andina, Universidad de Buenos Aires, Departamento de Ciencias Geológicas, Ciudad Universitaria, Pabellon II, 1428 Capital Federal, Argentina | ||
| 690 | 1 | 0 | |a ANDES |
| 690 | 1 | 0 | |a CHOIYOI GROUP |
| 690 | 1 | 0 | |a LITHOSPHERIC ANISOTROPY |
| 690 | 1 | 0 | |a OBLIQUE EXTENSION |
| 690 | 1 | 0 | |a PERMO-TRIASSIC VOLCANISM |
| 690 | 1 | 0 | |a DISPLACEMENT |
| 690 | 1 | 0 | |a EXTENSIONAL TECTONICS |
| 690 | 1 | 0 | |a LITHOSPHERIC STRUCTURE |
| 690 | 1 | 0 | |a NORMAL FAULT |
| 690 | 1 | 0 | |a OBLIQUE FAULT |
| 690 | 1 | 0 | |a OROGENIC BELT |
| 690 | 1 | 0 | |a PERMIAN-TRIASSIC BOUNDARY |
| 690 | 1 | 0 | |a RIFTING |
| 690 | 1 | 0 | |a STRUCTURAL CONTROL |
| 690 | 1 | 0 | |a SUTURE ZONE |
| 690 | 1 | 0 | |a TECTONIC EVOLUTION |
| 690 | 1 | 0 | |a VOLCANISM |
| 690 | 1 | 0 | |a ANDES |
| 690 | 1 | 0 | |a POTRERILLOS |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a MENDOZA | |
| 651 | 4 | |a SOUTH AMERICA | |
| 700 | 1 | |a Martinez, A.N. | |
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