Detrital zircon from a late Paleozoic accretionary complex of SW Iberia (Variscan Belt): History of crustal growth and recycling at the Rheic convergent margin

In this study we present new U-Pb ages of detrital zircons from greywackes and quartzites of the Pulo do Lobo Anticline (PLA) that have been interpreted to represent a Late Paleozoic accretionary complex in SW Iberia. The PLA separates the Ossa Morena Zone, which has a North- Gondwana affinity throu...

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Bibliographic Details
Main Author: Pereira, M.F. (author)
Other Authors: Drost, K. (author), Chichorro, M. (author), Silva, J.B. (author), Sola, R. (author)
Format: lecture
Language:eng
Published: 2013
Subjects:
detrital zircon
Pulo do Lobo
Online Access:http://hdl.handle.net/10174/7936
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/7936

Internet

http://hdl.handle.net/10174/7936

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