Zircon O- and Hf-isotope constraints on the genesis and tectonic significance of Permian magmatism in Patagonia

Paula Castillo, C. Mark Fanning, Robert J. Pankhurst, Francisco Hervé, Carlos W. Rapela

Resultado de la investigación: Contribución a una revistaArtículorevisión exhaustiva

25 Citas (Scopus)

Resumen

The genesis of Permian magmatism in southern South America is actively debated, particularly in relation to the origin of Patagonia. U-Pb zircon ages of c. 255 Ma for igneous rocks from the basement of Tierra del Fuego are the first evidence for southerly prolongation of this magmatism. Zircon in these rocks has εHft values <-1 and δ18O > 7.4‰, indicating recycling of Cambrian rocks. Permian granites in the north of the North Patagonian Massif record mantle-like δ18O magmatic input at c. 280 and 255 Ma, but reworking of upper crust between these two events, paralleling the recognized deformational history. In northwestern Patagonia, Early Permian granitic rocks have zircon with eHft values ranging from +0.1 to -7.2, and δ18O > 6.2‰, suggesting continuity of the Permian magmatic belt along the western margin of South America farther north. Comparison with a sample from the Sierra de la Ventana suggests melting of similar crust on both sides of the Patagonia-South American hypothetical suture. These features, together with other geological considerations, are consistent with an autochthonous or parautochthonous origin of northern Patagonia and connection between southern Patagonia and the Antarctic Peninsula in late Palaeozoic time.

Idioma originalInglés
Páginas (desde-hasta)803-816
Número de páginas14
PublicaciónJournal of the Geological Society
Volumen174
N.º5
DOI
EstadoPublicada - 1 sep 2017

Áreas temáticas de ASJC Scopus

  • Geología

Huella

Profundice en los temas de investigación de 'Zircon O- and Hf-isotope constraints on the genesis and tectonic significance of Permian magmatism in Patagonia'. En conjunto forman una huella única.

Citar esto