Constraints on the Neogene growth of the central Patagonian Andes at the latitude of the Chile triple junction (45–47°S) using U/Pb geochronology in synorogenic strata

@article{Folguera2018ConstraintsOT,
  title={Constraints on the Neogene growth of the central Patagonian Andes at the latitude of the Chile triple junction (45–47°S) using U/Pb geochronology in synorogenic strata},
  author={Andr{\'e}s Folguera and A. Encinas and A. Echaurren and Guido M Gianni and Dar{\'i}o Leandro Orts and V. Valencia and Gabriel Carrasco},
  journal={Tectonophysics},
  year={2018}
}
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References

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Mesozoic‐Cenozoic denudation history of the Patagonian Andes (southern Chile) and its correlation to different subduction processes
Fission track (FT) analysis is applied to assess the Mesozoic and Cenozoic thermal and denudational history of the Patagonian Andes between 44° and 51°S and the geologic and geomorphic response of…
Geochronologic and paleontologic evidence for a Pacific–Atlantic connection during the late Oligocene–early Miocene in the Patagonian Andes (43–44°S)
Tectonic development of the North Patagonian Andes and their related Miocene foreland basin (41°30′‐43°S)
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tectonic inversion of extensional structures of Early to Middle Jurassic age in the Main Andes to…
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Fission-track (FT) thermochronology has been applied to investigate the low-temperature cooling and denudation history of the Patagonian Andes along the southern part of the intra-arc transpressional…
Neogene uplift of central eastern Patagonia: Dynamic response to active spreading ridge subduction?
The Chile Triple Junction (CTJ) episodically migrated northward during the past 14 Ma from 54°S to its present‐day position at 46°30′S, as different almost trench‐parallel spreading segments entered…
Miocene to Late Quaternary Patagonian basalts (46-47°S): Geochronometric and geochemical evidence for slab tearing due to active spreading ridge subduction
Pliocene extensional tectonics in the Eastern Central Patagonian Cordillera: geochronological constraints and new field evidence
Recent field work and review of radiometric data obtained from Neogene lavas and plutonic rocks exposed in the Eastern Central Patagonian Cordillera (46–48ºS), which overlie subducted segments of the…
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