Middle Eocene-Oligocene broken-foreland evolution in the Andean Calchaqui Valley, NW Argentina: Insights from stratigraphic, structural and provenance studies

Two end-member models have been proposed for the Paleogene Andean foreland: a simple W-E migrating foreland model and a broken-foreland model. We present new stratigraphic, sedimentological and structural data from the Paleogene Quebrada de los Colorados (QLC) Formation, in the Eastern Cordillera, w...

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Autor principal: Del Papa, C.
Otros Autores: Hongn, F., Powell, J., Payrola, P., Do Campo, M., Strecker, M.R, Petrinovic, I., Schmitt, A.K, Pereyra, R.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 2013
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100 1 |a Del Papa, C. 
245 1 0 |a Middle Eocene-Oligocene broken-foreland evolution in the Andean Calchaqui Valley, NW Argentina: Insights from stratigraphic, structural and provenance studies 
260 |c 2013 
270 1 0 |m Del Papa, C.; CICTERRA-CONICET, Universidad Nacional de Córdoba, Av. Velez Sarsfield 1611, 2 Piso, Córdoba X5016GCA, Argentina; email: delpapacecilia@yahoo.com 
506 |2 openaire  |e Política editorial 
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520 3 |a Two end-member models have been proposed for the Paleogene Andean foreland: a simple W-E migrating foreland model and a broken-foreland model. We present new stratigraphic, sedimentological and structural data from the Paleogene Quebrada de los Colorados (QLC) Formation, in the Eastern Cordillera, with which to test these two different models. Basin-wide unconformities, growthstrata and changes in provenance indicate deposition of the QLC Formation in a tectonically active basin. Both west- and east-vergent structures, rooted in the basement, controlled the deposition and distribution of the QLC Formation from the Middle Eocene to the Early Miocene. The provenance analysis indicates that the main source areas were basement blocks, like the Paleozoic Oire Eruptive Complex, uplifted during Paleogene shortening, and that delimits the eastern boundary of the present-day intraorogenic Puna plateau. A comparison of the QLC sedimentary basin-fill pattern with those of adjacent Paleogene basins in the Puna plateau and in the Santa Bárbara System highlights the presence of discrete depozones. These reflect the early compartmentalization of the foreland, rather than a stepwise advance of the deformation front of a thrust belt. The early Tertiary foreland of the southern central Andes is represented by a ca. 250-km-wide area comprising several deformation zones (Arizaro, Macón, Copalayo and Calchaquí) in which doubly vergent or asymmetric structures, rooted in the basement, were generated. Hence, classical foreland model is difficult to apply in this Paleogene basin; and our data and interpretation agree with a broken-foreland model. © 2013 John Wiley & Sons Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologists.  |l eng 
593 |a CICTERRA, CONICET-Universidad Nacional de Córdoba, Córdoba, Argentina 
593 |a IBIGEO, CONICET-Universidad Nacional de Salta, Salta, Argentina 
593 |a CONICET, Universidad Nacional de Tucumán, Tucumán, Argentina 
593 |a INGEIS, CONICET, Universidad de Buenos Aires, Buenos Aires, Argentina 
593 |a Institutfür Erd- und Umweltwissenschaften, Universität Potsdam, Potsdam, Germany 
593 |a Department of Earth and Space Sciences, University of California, Los Angeles, CA, United States 
690 1 0 |a BASIN EVOLUTION 
690 1 0 |a DEFORMATION 
690 1 0 |a DEPOSITION 
690 1 0 |a EOCENE-OLIGOCENE BOUNDARY 
690 1 0 |a FORELAND BASIN 
690 1 0 |a LITHOSTRATIGRAPHY 
690 1 0 |a PROVENANCE 
690 1 0 |a SEDIMENTARY BASIN 
690 1 0 |a SEDIMENTOLOGY 
690 1 0 |a CALCHAQUI VALLEYS 
651 4 |a ARGENTINA 
700 1 |a Hongn, F. 
700 1 |a Powell, J. 
700 1 |a Payrola, P. 
700 1 |a Do Campo, M. 
700 1 |a Strecker, M.R. 
700 1 |a Petrinovic, I. 
700 1 |a Schmitt, A.K. 
700 1 |a Pereyra, R. 
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856 4 0 |u https://doi.org/10.1111/bre.12018  |y DOI 
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