Cretaceous intraplate contraction in Southern Patagonia: A far-field response to changing subduction dynamics?

GIANNI, G. M.; DÍAZ, M.; FOLGUERA, A.; NAVARRETE, C.; GIMÉNEZ, M. E.; LIENDO, I.; ENCINAS, A.

TECTONICS

AMER GEOPHYSICAL UNION

Año: 2018 vol. 37 p. 2915 - 2937

0278-7407

The origin, extent and timing of intraplate contractionin Patagonia are among the least understood geological processesof southern South America. Particularly, the intraplate Deseado fold-thrust belt (FTB),located in the Patagonian broken foreland (47º-48º30?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 spatio-temporal 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 tectonicforces 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 favorsstudies supporting inception of Andean shortening since Cretaceous times.