U-Pb ages and Hf isotope compositions of zircons in plutonic rocks from the central Famatinian arc, Argentina

• Published in: Journal of South American earth sciences Vol. 76; pp. 412 - 426
• Main Authors: Otamendi, Juan E., Ducea, Mihai N., Cristofolini, Eber A., Tibaldi, Alina M., Camilletti, Giuliano C., Bergantz, George W.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.07.2017
• Subjects: Famatinian arc; Hafnium isotope; Ordovician; Zircon; Ordovician; Hafnium isotope; Famatinian arc; Zircon
• ISSN: 0895-9811; 1873-0647
• DOI: 10.1016/j.jsames.2017.04.005

The Famatinian arc formed around the South Iapetus rim during the Ordovician, when oceanic lithosphere subducted beneath the West Gondwana margin. We present combined in situ U–Th–Pb and Lu–Hf isotope analyses for zircon to gain insights into the origin and evolution of Famatinian magmatism. Zircon crystals sampled from four intermediate and silicic plutonic rocks confirm previous observations showing that voluminous magmatism took place during a relatively short pulse between the Early and Middle Ordovician (472–465 Ma). The entire zircon population for the four plutonic rocks yields coherent εHf negative values and spreads over several ranges of initial εHf(t) units (−0.3 to −8.0). The range of εHf units in detrital zircons of Famatinian metasedimentary rocks reflects a prolonged history of the cratonic sources during the Proterozoic to the earliest Phanerozoic. Typical tonalites and granodiorites that contain zircons with evolved Hf isotopic compositions formed upon incorporating (meta)sedimentary materials into calc–alkaline metaluminous magmas. The evolved Hf isotope ratios of zircons in the subduction related plutonic rocks strongly reflect the Hf isotopic character of the metasedimentary contaminant, even though the linked differentiation and growth of the Famatinian arc crust was driven by ascending and evolving mantle magmas. Geochronology and Hf isotope systematics in plutonic zircons allow us understanding the petrogenesis of igneous series and the provenance of magma sources. However, these data could be inadequate for computing model ages and supporting models of crustal evolution. •U–Pb zircon ages reveal high magmatic flux along the Ordovician Gondwana margin.•Calc–alkaline metaluminous plutonic rocks contain zircons with evolved Hf composition.•Several phenomena converge to have isotopically evolved zircons in I-type plutonic rocks.•Hf isotope in magmatic zircons highlights contributions of metasedimentary contaminants.