Birth and demise of the Rheic Ocean magmatic arc(s): Combined U–Pb and Hf isotope analyses in detrital zircon from SW Iberia siliciclastic strata

Paleozoic continental reconstructions indicate that subduction of Rheic oceanic lithosphere led to collision be- tween Laurussia and Gondwanawhich was a major event in the formation of the Ouachita-Appalachian-Variscan orogenic belt and the amalgamation of Pangea. However, arc systems which record R...

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Bibliographic Details
Main Author: Pereira, Manuel Francisco (author)
Other Authors: Gutierrez-Alonso, Gabriel (author), Murphy, J. Brendan (author), Drost, Kerstin (author), Gama, Cristina (author), Silva, J. Brandão (author)
Format: article
Language:eng
Published: 2018
Subjects:
Detrital zircon age
Hf isotope composition
Rheic Ocean magmatic arc(s)
Devonian–Carboniferous
Laurussia–Gondwana collision
Online Access:http://hdl.handle.net/10174/22540
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/22540

Internet

http://hdl.handle.net/10174/22540

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