New U-Pb ages for syn-orogenic magmatism in the SW sector of the Ossa Morena Zone (Portugal)

The Ossa-Morena Zone (OMZ) is a major geotectonic unit within the Iberian Massif (which constitutes an important segment of the European Variscan Belt) and one of its distinguishing features is the presence of a noteworthy compositional diversity of plutonic rocks. In the SW sector of the OMZ, the t...

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Bibliographic Details
Main Author: Moita, P. (author)
Other Authors: Santos, J. F. (author), Costa, M. M. (author), Corfu, F. (author)
Format: conferenceObject
Language:eng
Published: 2013
Subjects:
Ossa-Morena Zone
Hospitais intrusion
Syn-orogenic magmatism
Tonalites
Mafic enclaves
U-Pb zircon ages
Lower Carboniferous
Online Access:http://hdl.handle.net/10773/10994
Country:Portugal
Oai:oai:ria.ua.pt:10773/10994

Internet

http://hdl.handle.net/10773/10994

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