Geodynamic evolution of Ossa-Morena Zone in a SW Iberian context during the Variscan cycle

Ossa-Morena Zone (OMZ) is crucial to understanding the geodynamic evolution of the Variscan cycle in SW Iberia. We review previous data, from Early to Late Paleozoic. The early Cambrian (conglomeratic and felsic metavolcanic units) lies unconformably upon Neoproterozoic formations and shows a carbon...

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Bibliographic Details
Main Author: Moreira, Noel (author)
Other Authors: Araújo, Alexandre (author), Pedro, Jorge (author), Dias, Rui (author)
Format: lecture
Language:eng
Published: 2015
Subjects:
Variscan
Iberia
tectono-metamorphic
Rheic
Online Access:http://hdl.handle.net/10174/13464
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/13464

Internet

http://hdl.handle.net/10174/13464

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