Abstract
In the external units of the Sardinian Variscides Nappe Zone, volcanic and volcanoclastic successions of Middle Ordovician age follow Lower Paleozoic calc-alkaline magmatism developed at the northern Gondwana margin. We present geochemical and zircon U–Pb isotopic data for the Truzzulla Formation, a low-to-medium-grade metamorphic volcanic–volcanoclastic succession belonging to the Monte Grighini Unit, the deepest unit in the Nappe Zone. Geochemical and radiometric data allow us to define a Late Ordovician (Katian) magmatic (volcanic) event of calc-alkaline affinity. These new data, in conjunction with previously published data, indicate that in the Sardinian Variscides, the age of Lower Paleozoic Andean-type calc-alkaline magmatism spans from Middle to Late Ordovician. Moreover, the age distribution of calc-alkaline volcanics and volcanoclastic rocks in the Nappe Zone is consistent with a diachronous development of Middle–Late Ordovician Andean-type magmatic arc through the portion of the northern Gondwanian margin now represented by the Sardinian Variscides. This reconstruction of the Sardinian Variscides reflects the complex magmatic and tectonic evolution of the northern margin of Gondwana in the Lower Paleozoic.
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Acknowledgments
M. E. Spano gratefully acknowledges the Sardinia Regional Government for the financial support to her PhD scholarship (P. O. R. Sardegna F. S. E. Operational Programme of the Autonomous Region of Sardinia, European Social Found 2007–2013—Axis IV Human Resources, Objective l.3, Line of Activity l.3.1.). Financial support from the University of Cagliari is acknowledged. We are grateful to reviewers L. Gaggero (University of Genova) and J. Wotzlaw (University of Geneva) for their helpful comments and criticism. The authors wish to thank the Ente Foreste della Regione Autonoma della Sardegna for hospitality during the field work.
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Cruciani, G., Franceschelli, M., Musumeci, G. et al. U–Pb zircon dating and nature of metavolcanics and metarkoses from the Monte Grighini Unit: new insights on Late Ordovician magmatism in the Variscan belt in Sardinia, Italy. Int J Earth Sci (Geol Rundsch) 102, 2077–2096 (2013). https://doi.org/10.1007/s00531-013-0919-z
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DOI: https://doi.org/10.1007/s00531-013-0919-z