Uplift sequence of the Andes at 30°S: Insights from sedimentology and U/Pb dating of synorogenic deposits
The South Central Andes at 30°S represent a key area to understand the Andes geodynamics as it is in the middle of the flat slab segment and all the morphotectonic units of the Central Andes are well developed. This work is focused in the proximal synorogenic deposits of the Western Precordillera, i...
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2017
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| LEADER | 25899caa a22016337a 4500 | ||
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| 001 | PAPER-15118 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518204546.0 | ||
| 008 | 190410s2017 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-85010660068 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Suriano, J. | |
| 245 | 1 | 0 | |a Uplift sequence of the Andes at 30°S: Insights from sedimentology and U/Pb dating of synorogenic deposits |
| 260 | |b Elsevier Ltd |c 2017 | ||
| 270 | 1 | 0 | |m Suriano, J.; IGeBA-FCEyN, UBA-CONICET, Intendente Güiraldes 2160 - Ciudad Universitaria-Pab.II-CABA-Argentina; email: jsuriano@gl.fcen.uba.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Yañez, G.A., Ranero, C.R., von Huene, R., Díaz, J., Magnetic anomaly interpretation across the southern central Andes (32°-34°S): the role of the Juan Fernandez Ridge in the late Tertiary evolution of the margin (2001) J. Geophys. Res., 106, pp. 6325-6345 | ||
| 504 | |a Zapata, T.R., Allmendinger, R.W., Evolución de la deformación del frente de corrimiento de la Precordillera (1997) Prov. San Juan. Rev. Asoc. Geol. Argent., 52, pp. 115-131 | ||
| 520 | 3 | |a The South Central Andes at 30°S represent a key area to understand the Andes geodynamics as it is in the middle of the flat slab segment and all the morphotectonic units of the Central Andes are well developed. This work is focused in the proximal synorogenic deposits of the Western Precordillera, in the La Tranca valley, in order to unravel the uplift sequence of this belt. Nine facies associations were recognized; most of them represent piedmont facies with local provenance from Precordillera and were deposited in the wedge-top depozone, as is expected for proximal sinorogenic deposits. However there are intercalations of transference fluvial systems, which show mixed provenance indicating that Permo-Triassic igneous rocks were already exposed to the west (Frontal Cordillera). There are also lacustrine deposits which are interpreted as the result of damming by fault activity at east of the studied basin. Finally, two maximum depositional ages at ca. 11 Ma and 8 Ma of these deposits indicate that the onset of uplift of the Precordillera at 30°S is little older than 11 Ma. These data change two previous ideas about the evolution of the Precordillera: its uplift at 30° S is younger than proposed by previous works and it is nearly synchronous along strike. © 2017 Elsevier Ltd |l eng | |
| 593 | |a IGeBA-FCEyN, UBA-CONICET, Intendente Güiraldes 2160 - Ciudad Universitaria-Pab.II-CABA-C1428EGA, Argentina | ||
| 593 | |a IANIGLA, CCT Mendoza, CONICET, Parque San Martín s/n, Mendoza, 5500, Argentina | ||
| 593 | |a Department of Geology, University of Wisconsin, Eau Claire, WI 54701, United States | ||
| 593 | |a Department of Geological Sciences San Diego State University, San Diego, 92182-1020, United States | ||
| 690 | 1 | 0 | |a BERMEJO FORELAND BASIN |
| 690 | 1 | 0 | |a WEDGETOP DEPOSITS |
| 690 | 1 | 0 | |a FORELAND BASIN |
| 690 | 1 | 0 | |a OROGENY |
| 690 | 1 | 0 | |a SEDIMENTOLOGY |
| 690 | 1 | 0 | |a STRIKE (GEOLOGY) |
| 690 | 1 | 0 | |a UPLIFT |
| 690 | 1 | 0 | |a URANIUM-LEAD DATING |
| 690 | 1 | 0 | |a ANDES |
| 690 | 1 | 0 | |a PRECORDILLERA |
| 651 | 4 | |a SAN JUAN PRECORDILLERA | |
| 700 | 1 | |a Mardonez, D. | |
| 700 | 1 | |a Mahoney, J.B. | |
| 700 | 1 | |a Mescua, J.F. | |
| 700 | 1 | |a Giambiagi, L.B. | |
| 700 | 1 | |a Kimbrough, D. | |
| 700 | 1 | |a Lossada, A. | |
| 773 | 0 | |d Elsevier Ltd, 2017 |g v. 75 |h pp. 11-34 |p J. South Am. Earth Sci. |x 08959811 |w (AR-BaUEN)CENRE-1080 |t Journal of South American Earth Sciences | |
| 856 | 4 | 1 | |u https://www.scopus.com/inward/record.uri?eid=2-s2.0-85010660068&doi=10.1016%2fj.jsames.2017.01.004&partnerID=40&md5=34f65423295ffedc2b75e6ffd65964bd |y Registro en Scopus |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.jsames.2017.01.004 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_08959811_v75_n_p11_Suriano |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v75_n_p11_Suriano |y Registro en la Biblioteca Digital |
| 961 | |a paper_08959811_v75_n_p11_Suriano |b paper |c PE | ||
| 962 | |a info:eu-repo/semantics/article |a info:ar-repo/semantics/artículo |b info:eu-repo/semantics/publishedVersion | ||
| 963 | |a VARI | ||
| 999 | |c 76071 | ||