Origin and emplacement of syn-orogenic Variscan granitoids in Iberia the Beiras massif

The Beiras batholith consists of four main Variscan granitoid suites intruded into metasediments of Proterozoic-Cambrian and Palaeozoic age in Central Northern Portugal: a) the early, syn-D3 granodiorite-monzogranite suite (314-311 Ma); b) the highly peraluminous syn-D3 two-mica/leucogranite suite (...

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Bibliographic Details
Main Author: Azevedo, M. Rosário (author)
Other Authors: Valle Aguado, B. (author), Nolan, J. (author), Martins, M. Estela (author), Medina, J. (author)
Format: article
Language:eng
Published: 2014
Subjects:
Calc-alkaline granites
Iberian massif
Peraluminous granites
Portugal
U-Pb geochronology
Variscan post-collisional magmatism
Online Access:http://hdl.handle.net/10773/13027
Country:Portugal
Oai:oai:ria.ua.pt:10773/13027

Internet

http://hdl.handle.net/10773/13027

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