Abstract
LA-MC-ICP-MS U–Pb zircon ages and whole-rock geochemical data obtained from volcanic rocks erupted in the northern margin of Gondwana provide new insights on the polyphase magmatic evolution of the NW Iberian domain during the establishment of passive margin conditions in Lower Paleozoic times. The U–Pb data show crystallization ages of ca. 455 Ma for two calc-alkaline rhyolites sampled in the Upper Parautochthon of the eastern Galicia—Trás-os-Montes Zone (GTMZ) and for an intraplate basalt intruded into Middle Ordovician slates of the autochthonous series of the Central Iberian Zone (CIZ). Together with previous data, the ages obtained reveal a periodic magmatic activity across the northern Gondwana margin during the Lower Paleozoic, which is comparable to that observed in NE Iberia and in other massifs of the Mediterranean realm. Both geochronological and geochemical data reinforce paleontological and stratigraphic evidences for paleogeographic proximity between these domains and contribute to the recognition of extensional-related magmatism along the northern margin of Central Gondwana associated with the opening of the Rheic Ocean.
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Acknowledgments
We kindly thank Michel Faure and an anonymous reviewer for their comments and corrections. This contribution was funded by the Instituto Geológico y Minero de España (IGME) through its PhD program, by the Instituto Dom Luiz—Universidade de Lisboa (IDL) postdoctoral Grant (program “Incentivo/CTE/LA0019/2014”) and by the Fundação para a Ciencia e Tecnologia (FCT, Portugal) postdoctoral Grant SFRH/BPD/99550/2014 given to IDS. It has been as well partially funded by the research projects CGL2007-65338-C02-02/BTE and CGL2011-22728 of the Spanish Ministry of Science and Innovation, as part of the National Program of Projects in Fundamental Research, in the frame of the V and VI National Plans of Scientific Research, Development and Technologic Innovation. RDF appreciates financial support from FCT (Portugal) through its postdoctoral program. This work is a contribution to the IGCP Project No. 597 (Amalgamation and breakup of Pangaea), IGCP project 648 (Supercontinent Cycle and Global Geodynamics), IDL Research Group 5, to the project FCT “GOLD” (PTDC/GEO-GEO/2446/2012) and to the IGME Project No. 2281.
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Dias da Silva, Í., Díez Fernández, R., Díez-Montes, A. et al. Magmatic evolution in the N-Gondwana margin related to the opening of the Rheic Ocean—evidence from the Upper Parautochthon of the Galicia-Trás-os-Montes Zone and from the Central Iberian Zone (NW Iberian Massif). Int J Earth Sci (Geol Rundsch) 105, 1127–1151 (2016). https://doi.org/10.1007/s00531-015-1232-9
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DOI: https://doi.org/10.1007/s00531-015-1232-9