The Significance of Changes of Source Areas During Carboniferous Turbiditic Deposition (Southwestern Iberia)

U–Pb dating of detrital zircons from the Carboniferous turbidites of southwestern Iberia (the Cabrela, Mértola, Mira, and Brejeira formations) shows that synorogenic sedimentation during the Carboniferous was marked by significant variations in the source areas, involving the denudation of different...

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Bibliographic Details
Main Author: Pereira, Manuel Francisco (author)
Other Authors: Chichorro, Martim (author), Gutierrez-Alonso, G. (author), Vilallonga, Filipa (author), Drost, K. (author), Ribeiro, Carlos (author), Silva, J.B. (author), Albardeiro, Luis (author), Hofmann, M. (author), Linnemann, U. (author)
Format: lecture
Language:por
Published: 2015
Subjects:
U-Pb geochronology
South Portuguese Zone
Ossa-Morena Zone
Variscan orogeny
Pangea
Online Access:http://hdl.handle.net/10174/13458
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/13458

Internet

http://hdl.handle.net/10174/13458

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