Cretaceous Intraplate Contraction in Southern Patagonia: A Far-Field Response to Changing Subduction Dynamics?
The origin, extent, and timing of intraplate contraction in Patagonia are among the least understood geological processes of southern South America. Particularly, the intraplate Deseado fold-thrust belt (FTB), located in the Patagonian broken foreland (47°–48°30′S), is one of the most enigmatic area...
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Blackwell Publishing Ltd
2018
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| 024 | 7 | |2 scopus |a 2-s2.0-85052969662 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Gianni, G.M. | |
| 245 | 1 | 0 | |a Cretaceous Intraplate Contraction in Southern Patagonia: A Far-Field Response to Changing Subduction Dynamics? |
| 260 | |b Blackwell Publishing Ltd |c 2018 | ||
| 270 | 1 | 0 | |m Gianni, G.M.; Instituto Geofísico Sismológico Ing. Volponi, Universidad Nacional de San JuanArgentina; email: guidogianni22@gmail.com |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a The origin, extent, and timing of intraplate contraction in Patagonia are among the least understood geological processes of southern South America. Particularly, the intraplate Deseado fold-thrust belt (FTB), located in the Patagonian broken foreland (47°–48°30′S), is one of the most enigmatic areas. In this belt, time constraints on tectonic events are limited and synorogenic deposits have not been documented so far. Furthermore, the driving mechanism for intraplate contraction remains unknown. In this study, we carried out a structural and sedimentological analysis. We report the first syntectonic deposits in this area in the Baqueró (Aptian) and Chubut (Cenomanian/Campanian) groups and a newly found unit referred to as the Albian beds (109.9 ± 1.5 Ma). Thus, several contractional stages in late Aptian, Albian, and Cenomanian-Campanian are then inferred. We suggest that the Deseado FTB constituted the southernmost expression of the early Patagonian broken foreland in Cretaceous times. Additionally, we analyzed the spatiotemporal magmatic arc behavior as a proxy of dynamic changes in the Andean subduction during determined stages of intraplate contraction. We observe a significant arc broadening from ~121 to 82 Myr and magmatic quiescence after ~67 Ma. This is interpreted as a slab shallowing to flattening process. Far-field tectonic forces would have been produced by increased plate coupling linked to the slab flattening as indirectly indicated by the correlation between Cretaceous arc expansion and intraplate contraction. Finally, the tectonic evolution of the Deseado FTB favors studies supporting inception of Andean shortening since Cretaceous times. ©2018. American Geophysical Union. All Rights Reserved. |l eng | |
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: The authors want to recognize the support received by CONICET and the fruitful discussions with Miguel Ramos and Andrés Echaurren from the Laboratorio de Tectónica Andina. The geochronological data used are listed in the references text and Supporting Information S1. Comments by Etienne Jaillard and two anonymous reviewers helped to improve this manuscript. We are thankful to the Editor Laurent Jolivet for an effective handling of the manuscript. | ||
| 593 | |a Instituto Geofísico Sismológico Ing. Volponi, Universidad Nacional de San Juan, San Juan, Argentina | ||
| 593 | |a Departamento de Geología, Universidad Nacional de la Patagonia San Juan Bosco, Comodoro Rivadavia, Argentina | ||
| 593 | |a Departamento de Geología, Universidad Nacional de San Juan, San Juan, Argentina | ||
| 593 | |a Departamento de Ciencias de la Tierra, Universidad de Concepción, Concepción, Chile | ||
| 593 | |a IDEAN, Instituto de Estudios Andinos Don Pablo Groeber, UBA - CONICET. Departamento de Ciencias Geológicas, FCEN, Universidad de Buenos Aires, Buenos Aires, Argentina | ||
| 690 | 1 | 0 | |a ARC MIGRATION |
| 690 | 1 | 0 | |a BROKEN FORELAND |
| 690 | 1 | 0 | |a GROWTH STRATA |
| 690 | 1 | 0 | |a INTRAPLATE CONTRACTION |
| 690 | 1 | 0 | |a PATAGONIAN ANDES |
| 690 | 1 | 0 | |a SYNOROGENIC DEPOSITS |
| 690 | 1 | 0 | |a DEPOSITS |
| 690 | 1 | 0 | |a ARC MIGRATION |
| 690 | 1 | 0 | |a BROKEN FORELAND |
| 690 | 1 | 0 | |a GROWTH STRATA |
| 690 | 1 | 0 | |a MAGMATIC QUIESCENCE |
| 690 | 1 | 0 | |a PATAGONIAN ANDES |
| 690 | 1 | 0 | |a SEDIMENTOLOGICAL ANALYSIS |
| 690 | 1 | 0 | |a SUBDUCTION DYNAMICS |
| 690 | 1 | 0 | |a TECTONICS |
| 690 | 1 | 0 | |a CRETACEOUS |
| 690 | 1 | 0 | |a FOLD AND THRUST BELT |
| 690 | 1 | 0 | |a FORELAND BASIN |
| 690 | 1 | 0 | |a INTRAPLATE PROCESS |
| 690 | 1 | 0 | |a SUBDUCTION |
| 690 | 1 | 0 | |a ANDES |
| 690 | 1 | 0 | |a PATAGONIA |
| 651 | 4 | |a SOUTHERN SOUTH AMERICA | |
| 700 | 1 | |a Navarrete, C. | |
| 700 | 1 | |a Liendo, I. | |
| 700 | 1 | |a Díaz, M. | |
| 700 | 1 | |a Giménez, M.E. | |
| 700 | 1 | |a Encinas, A. | |
| 700 | 1 | |a Folguera, A. | |
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