Structure and development of the Andean system between 36° and 39°S
One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The northern portion is characterized by prominent basement structures and a thick-skinned orogenic front with relief of over 2000. m with a deep level of exhumation where more than 4. km of section has b...
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2014
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| LEADER | 28696caa a22017537a 4500 | ||
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| 001 | PAPER-24024 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205548.0 | ||
| 008 | 190411s2014 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84890153878 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Rojas Vera, E.A. | |
| 245 | 1 | 0 | |a Structure and development of the Andean system between 36° and 39°S |
| 260 | |c 2014 | ||
| 270 | 1 | 0 | |m Rojas Vera, E.A.; IDEAN (UBA-CONICET), Laboratorio de Tectónica Andina, Departamento de Geología, Universidad de Buenos AiresArgentina; email: erv081@yahoo.com.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Willner, A.P., Time Markers for the Evolution and Exhumation History of a Late Palaeozoic Paired Metamorphic Belt in North-Central Chile (34-35°30'S) (2005) Journal of Petrology, 46, pp. 1835-1858 | ||
| 504 | |a Yuan, X., Asch, G., Bataille, K., Bock, G., Bohm, M., Echtler, H., Kind, R., Wölbern, I., Deep seismic images of the Southern Andes (2006) Evolution of an Andean Margin: A Tectonic and Magmatic View from the Andes to the Neuquén Basin (35-39°S Lat), 407, pp. 61-72. , Geological Society of America, Special Paper | ||
| 504 | |a Zamora Valcarce, G., Zapata, T., Estilo Estructural de la Faja Plegada a los 37°S (2005) Congreso de exploración y desarrollo de hidrocarburos, vol. 6, CD room | ||
| 504 | |a Zamora Valcarce, G., (2007), p. 303. , Estructura y Cinemática de la faja plegada y corrida del Agrio, Cuenca Neuquina. PhD Thesis. Universidad de Buenos Aires, Buenos Aires; Zamora Valcarce, G., Zapata, T., Del Pino, D., Ansa, A., Structural evolution and magmatic characteristics of the Agrio fold-and-thrust belt (2006) Evolution of an Andean Margin: A Tectonic and Magmatic View from the Andes to the Neuquén Basin (35-39°S Lat), 407, pp. 125-145. , Geological Society of America, Special Paper | ||
| 504 | |a Zamora Valcarce, G., Zapata, T., Ramos, V.A., Rodriguez, F., Bernanrdo, L.M., Evolución tectónica del frente andino en Neuquén (2009) Revista de la Asociación Geológica Argentina, 65, pp. 192-203 | ||
| 504 | |a Zapata, T., Brissón, I., Dzelalija, F., The role of basement in the Andean fold and thrust belt of the Neuquén Basin (1999) Proceedings Thrust Tectonics, pp. 122-124 | ||
| 504 | |a Zollner, W., Amos, A.J., (1973) Descripción geológica de la Hoja 32b, Chos Malal (Prov. Neuquén), Bulletin 143, , Servicio Geológico Minero Argentino, Buenos Aires | ||
| 520 | 3 | |a One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The northern portion is characterized by prominent basement structures and a thick-skinned orogenic front with relief of over 2000. m with a deep level of exhumation where more than 4. km of section has been eroded. Contrastingly, the southern part is formed by mildly inverted basement structures restricted mainly to the hinterland zone, which reaches only 1500-1700. m relief. We quantify the variable contributions of two main contractional stages through the construction of three regionally balanced sections across the Andes, constrained by field and geophysical data. Extensional re-activation described for this segment in late Oligocene-early Miocene and Pliocene to Quaternary times, after the two main contractional episodes, suggests only 3. km of stretching that represents 30-10% of the original longitude. We, therefore, conclude that while initial Late Cretaceous to Eocene compression was similar along strike (~10-7. km), it is the contrasting degrees of Neogene shortening (~16-6. km) that have played the largest role in the along strike differences in structure and morphology along this portion of the southern Andes. Variable Neogene arc expansion could be responsible for the contrasting contractional deformation: In the north, late Miocene arc-related rocks cover most of the retroarc zone (>200. km with respect to the late Miocene arc front in the south), presumably driven by a shallow subduction episode in the area, whereas to the south they remain restricted to the continental drainage divide. Other factors involving architecture of previous rift structures, are proposed as additional mechanisms that accommodated variable shortening magnitudes through inversion. © 2013 Elsevier Ltd. |l eng | |
| 593 | |a IDEAN (UBA-CONICET), Laboratorio de Tectónica Andina, Departamento de Geología, Universidad de Buenos Aires, Argentina | ||
| 593 | |a Repsol, Exploración, Lima, Peru | ||
| 593 | |a Y.P.F. S.A. Exploración, Buenos Aires, Argentina | ||
| 690 | 1 | 0 | |a EXTENSIONAL REACTIVATION |
| 690 | 1 | 0 | |a FOLD AND THRUST BELT |
| 690 | 1 | 0 | |a NEOGENE CONTRACTION |
| 690 | 1 | 0 | |a SOUTHERN CENTRAL ANDES |
| 690 | 1 | 0 | |a EXHUMATION |
| 690 | 1 | 0 | |a EXTENSIONAL TECTONICS |
| 690 | 1 | 0 | |a FOLD AND THRUST BELT |
| 690 | 1 | 0 | |a GEOMORPHOLOGY |
| 690 | 1 | 0 | |a NEOGENE |
| 690 | 1 | 0 | |a OROGENY |
| 690 | 1 | 0 | |a STRUCTURAL GEOLOGY |
| 690 | 1 | 0 | |a TECTONIC EVOLUTION |
| 690 | 1 | 0 | |a ANDES |
| 700 | 1 | |a Folguera, A. | |
| 700 | 1 | |a Zamora Valcarce, G. | |
| 700 | 1 | |a Bottesi, G. | |
| 700 | 1 | |a Ramos, V.A. | |
| 773 | 0 | |d 2014 |g v. 73 |h pp. 34-52 |p J. Geodyn. |x 02643707 |t Journal of Geodynamics | |
| 856 | 4 | 1 | |u https://www.scopus.com/inward/record.uri?eid=2-s2.0-84890153878&doi=10.1016%2fj.jog.2013.09.001&partnerID=40&md5=f3cee31af94391a05efebaf540303c0d |y Registro en Scopus |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.jog.2013.09.001 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_02643707_v73_n_p34_RojasVera |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02643707_v73_n_p34_RojasVera |y Registro en la Biblioteca Digital |
| 961 | |a paper_02643707_v73_n_p34_RojasVera |b paper |c PE | ||
| 962 | |a info:eu-repo/semantics/article |a info:ar-repo/semantics/artículo |b info:eu-repo/semantics/publishedVersion | ||
| 999 | |c 84977 | ||