Kinematic analysis of a transtensional fault system: The Atuel depocenter of the Neuquén basin, southern Central Andes, Argentina
The Atuel depocenter of the Neuquén basin originated as an Upper Triassic to Lower Jurassic rift system, later inverted during the Andean contractional deformation. In order to study the extensional architecture and the kinematic evolution of this depocenter, we collected a large amount of field and...
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2010
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| LEADER | 18370caa a22015377a 4500 | ||
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| 001 | PAPER-7777 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250211091013.0 | ||
| 008 | 190411s2010 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-77957019748 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Bechis, F. | |
| 245 | 1 | 0 | |a Kinematic analysis of a transtensional fault system: The Atuel depocenter of the Neuquén basin, southern Central Andes, Argentina |
| 260 | |c 2010 | ||
| 270 | 1 | 0 | |m Bechis, F.; CONICET - IIDyPCA, Universidad Nacional de Río Negro (UNRN), Sarmiento Inferior 3974, CP 8400, San Carlos de Bariloche, Argentina; email: florbechis@gmail.com |
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| 504 | |a Allmendinger, R.W., (2002) StereoWin Version 1.2.0, , http://www.geo.cornell.edu/geology/faculty/RWA/programs.html | ||
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| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a The Atuel depocenter of the Neuquén basin originated as an Upper Triassic to Lower Jurassic rift system, later inverted during the Andean contractional deformation. In order to study the extensional architecture and the kinematic evolution of this depocenter, we collected a large amount of field and sub-surface data, consisting of slip data from outcrop-scale normal faults, thickness and facies distribution within the synrift deposits, and structural data from angular and progressive unconformities. The Atuel depocenter has a NNW trend, showing a bimodal distribution of NNW and WNW major faults (first and second order faults). On the other hand, from kinematic indicators measured on outcrop-scale faults (third and fourth order faults), we found a mean NE internal extension direction, which is oblique to the general trend of the sub-basin. Taking these particular characteristics into account, we interpreted the Atuel depocenter as an oblique rift system. We evaluated two mechanisms in order to explain the development of this transtensional system: 1) reactivation of upper-crustal NNW-oriented Paleozoic shear zones, and 2) oblique stretching of a previous NNW-oriented lithospheric weakness zone. © 2010 Elsevier Ltd. |l eng | |
| 593 | |a CONICET - IIDyPCA, Universidad Nacional de Río Negro (UNRN), Sarmiento Inferior 3974, CP 8400, San Carlos de Bariloche, Argentina | ||
| 593 | |a CONICET - IANIGLA, CCT Mendoza, CC 330, CP 5500, Mendoza, Argentina | ||
| 593 | |a CONICET - Laboratorio de Modelado Geológico, FCEN, UBA, Ciudad Universitaria, Pabellón 2, CP 1428, Buenos Aires, Argentina | ||
| 593 | |a E505 East Tower, Knightsbridge, Esplanade Road, Century City, 7441, Cape Town, South Africa | ||
| 593 | |a CONICET - CIMAR, UNCOMA, Av. Buenos Aires 1300, CP 8300, Neuquén, Argentina | ||
| 651 | 4 | |a NEUQUEN BASIN | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a NEUQUEN BASIN | |
| 690 | 1 | 0 | |a CENTRAL ANDES |
| 690 | 1 | 0 | |a KINEMATIC ANALYSIS |
| 690 | 1 | 0 | |a OBLIQUE RIFT |
| 690 | 1 | 0 | |a TRANSTENSION |
| 690 | 1 | 0 | |a BIMODAL DISTRIBUTION |
| 690 | 1 | 0 | |a CENTRAL ANDES |
| 690 | 1 | 0 | |a FACIES DISTRIBUTION |
| 690 | 1 | 0 | |a FAULT SYSTEM |
| 690 | 1 | 0 | |a FOURTH ORDER |
| 690 | 1 | 0 | |a GENERAL TRENDS |
| 690 | 1 | 0 | |a JURASSIC |
| 690 | 1 | 0 | |a KINEMATIC ANALYSIS |
| 690 | 1 | 0 | |a KINEMATIC EVOLUTION |
| 690 | 1 | 0 | |a KINEMATIC INDICATORS |
| 690 | 1 | 0 | |a LITHOSPHERIC |
| 690 | 1 | 0 | |a NORMAL FAULTS |
| 690 | 1 | 0 | |a OBLIQUE RIFT |
| 690 | 1 | 0 | |a PALEOZOIC |
| 690 | 1 | 0 | |a RIFT SYSTEMS |
| 690 | 1 | 0 | |a SECOND ORDERS |
| 690 | 1 | 0 | |a SHEAR ZONE |
| 690 | 1 | 0 | |a STRUCTURAL DATA |
| 690 | 1 | 0 | |a SUB-SURFACES |
| 690 | 1 | 0 | |a SUBBASINS |
| 690 | 1 | 0 | |a SYN-RIFT |
| 690 | 1 | 0 | |a TRANSTENSION |
| 690 | 1 | 0 | |a UPPER TRIASSIC |
| 690 | 1 | 0 | |a ANGULAR DISTRIBUTION |
| 690 | 1 | 0 | |a GEOCHRONOLOGY |
| 690 | 1 | 0 | |a KINEMATICS |
| 690 | 1 | 0 | |a DEPOCENTER |
| 690 | 1 | 0 | |a EXTENSIONAL TECTONICS |
| 690 | 1 | 0 | |a KINEMATICS |
| 690 | 1 | 0 | |a OBLIQUE FAULT |
| 690 | 1 | 0 | |a RIFT ZONE |
| 690 | 1 | 0 | |a TECTONIC EVOLUTION |
| 690 | 1 | 0 | |a TRANSTENSION |
| 690 | 1 | 0 | |a ANDES |
| 700 | 1 | |a Giambiagi, L. | |
| 700 | 1 | |a García, V. | |
| 700 | 1 | |a Lanés, S. | |
| 700 | 1 | |a Cristallini, Ernesto Osvaldo | |
| 700 | 1 | |a Tunik, M. | |
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