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Abstract:

U–Pb SHRIMP zircon crystallization ages and Ar–Ar and K–Ar mica cooling ages for basement rocks of the Yaminué and Nahuel Niyeu areas in northeastern Patagonia are presented. Granitoids that cover the time span from Ordovician to Early Triassic constitute the main outcrops of the western sector of the Yaminué block. The southern Yaminué Metaigneous Complex comprises highly deformed Ordovician and Permian granitoids crosscut by undeformed leucogranite dikes (U–Pb SHRIMP zircon age of 254 ± 2 Ma). Mica separates from highly deformed granitoids from the southern sector yielded an Ar–Ar muscovite age of 182 ± 3 Ma and a K–Ar biotite age of 186 ± 2 Ma. Moderately to highly deformed Permian to Early Triassic granitoids made up the northern Yaminué Complex. The Late Permian to Early Triassic (U–Pb SHRIMP zircon age of 252 ± 6 Ma) Cabeza de Vaca Granite of the Yaminué block yielded Jurassic mica K–Ar cooling ages (198 ± 2, 191 ± 1, and 190 ± 2 Ma). At the boundary between the Yaminué and Nahuel Niyeu blocks, K–Ar muscovite ages of 188 ± 3 and 193 ± 5 Ma were calculated for the Flores Granite, whereas the Early Permian Navarrete granodiorite, located in the Nahuel Niyeu block, yielded a K–Ar biotite age of 274 ± 4 Ma. The Jurassic thermal history is not regionally uniform. In the supracrustal exposures of the Nahuel Niyeu block, the Early Permian granitoids of its western sector as well as other Permian plutons and Ordovician leucogranites located further east show no evidence of cooling age reset since mica ages suggest cooling in the wake of crystallization of these intrusive rocks. In contrast, deeper crustal levels are inferred for Permian–Early Triassic granitoids in the Yaminué block since cooling ages for these rocks are of Jurassic age (198–182 Ma). Jurassic resetting is contemporaneous with the massive Lower Jurassic Flores Granite, and the Marifil and Chon Aike volcanic provinces. This intraplate deformational pulse that affected northeastern Patagonia during the Early Jurassic (Sinemurian–Pliensbachian) was responsible for the partial (re)exhumation of the mid-crustal Paleozoic basement along reactivated discrete NE–SW to ENE–WSW lineaments and the resetting of isotopic systems. These new thermochronological data indicate that Early Permian magmatic rocks of the Nahuel Niyeu block were below 300 °C for ca. 20 Ma prior to the onset of the main magmatic episode of the Late Permian to Triassic igneous and metaigneous rocks of the Yaminué block. © 2016, Springer-Verlag Berlin Heidelberg.

Registro:

Documento: Artículo
Título:Jurassic cooling ages in Paleozoic to early Mesozoic granitoids of northeastern Patagonia: 40Ar/39Ar, 40K–40Ar mica and U–Pb zircon evidence
Autor:Martínez Dopico, C.I.; Tohver, E.; López de Luchi, M.G.; Wemmer, K.; Rapalini, A.E.; Cawood, P.A.
Filiación:Instituto de Geocronología y Geología Isotópica (INGEIS), Intendente Güiraldes 2160, Buenos Aires, C1428EGA, Argentina
Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Buenos Aires, Argentina
School of Earth and Geographical Sciences, University of Western Australia, Perth, Australia
Geoscience Centre of the University of Göttingen (GZG), Göttingen, Germany
Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires (IGEBA), Buenos Aires, Argentina
Department of Earth Sciences, University of St. Andrews, North Street, St Andrews, KY16 9AL, United Kingdom
School of Earth, Atmosphere and Environment, Monash University, Melbourne, VIC 3800, Australia
Palabras clave:Cooling ages; Magmatism; Paleozoic basement; Patagonia; Reset crystallization ages; argon-argon dating; cooling; crystallization; granitoid; Jurassic; magmatism; Mesozoic; mica; Paleozoic; uranium-lead dating; zircon; Patagonia
Año:2017
Volumen:106
Número:7
Página de inicio:2343
Página de fin:2357
DOI: http://dx.doi.org/10.1007/s00531-016-1430-0
Título revista:International Journal of Earth Sciences
Título revista abreviado:Int. J. Earth Sci.
ISSN:14373254
CODEN:IJESF
Registro:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_14373254_v106_n7_p2343_MartinezDopico

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Citas:

---------- APA ----------
Martínez Dopico, C.I., Tohver, E., López de Luchi, M.G., Wemmer, K., Rapalini, A.E. & Cawood, P.A. (2017) . Jurassic cooling ages in Paleozoic to early Mesozoic granitoids of northeastern Patagonia: 40Ar/39Ar, 40K–40Ar mica and U–Pb zircon evidence. International Journal of Earth Sciences, 106(7), 2343-2357.
http://dx.doi.org/10.1007/s00531-016-1430-0
---------- CHICAGO ----------
Martínez Dopico, C.I., Tohver, E., López de Luchi, M.G., Wemmer, K., Rapalini, A.E., Cawood, P.A. "Jurassic cooling ages in Paleozoic to early Mesozoic granitoids of northeastern Patagonia: 40Ar/39Ar, 40K–40Ar mica and U–Pb zircon evidence" . International Journal of Earth Sciences 106, no. 7 (2017) : 2343-2357.
http://dx.doi.org/10.1007/s00531-016-1430-0
---------- MLA ----------
Martínez Dopico, C.I., Tohver, E., López de Luchi, M.G., Wemmer, K., Rapalini, A.E., Cawood, P.A. "Jurassic cooling ages in Paleozoic to early Mesozoic granitoids of northeastern Patagonia: 40Ar/39Ar, 40K–40Ar mica and U–Pb zircon evidence" . International Journal of Earth Sciences, vol. 106, no. 7, 2017, pp. 2343-2357.
http://dx.doi.org/10.1007/s00531-016-1430-0
---------- VANCOUVER ----------
Martínez Dopico, C.I., Tohver, E., López de Luchi, M.G., Wemmer, K., Rapalini, A.E., Cawood, P.A. Jurassic cooling ages in Paleozoic to early Mesozoic granitoids of northeastern Patagonia: 40Ar/39Ar, 40K–40Ar mica and U–Pb zircon evidence. Int. J. Earth Sci. 2017;106(7):2343-2357.
http://dx.doi.org/10.1007/s00531-016-1430-0