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handle: 10261/273638
In the Iberian Massif a voluminous igneous activity was recorded along its reputed rifting axial (i.e., the Ossa-Morena Zone, OMZ) where three phases, separated by relatively quiescent periods, are distinguished. The first two, Early and Main rift-stage magmatic events, were defined in detail by Sánchez García et al. (2003) and are almost exclusive of the OMZ, while the Late rift-stage magmatic event mainly occurs in the Central Iberian (CIZ) and Galicia-Trás-os Montes (GTMZ) zones (Ollo de Sapo Formation and associated plutons).
Ordovician geodynamics: The Sardic Phase in the Pyrenees, Mouthoumet and Montagne Noire massifs International Meeting (2017. Figueras, España)
GeoBioTec, Departamento de Ciências da Terra, Universidade Nova de Lisboa, Portugal
Instituto de Geociencias, Consejo Superior de Investigaciones Científicas, España
Instituto de Geociencias, Universidad Complutense de Madrid, España
Laboratório Nacional de Energia e Geologia, Portugal
Instituto Geológico y Minero de España, España
Peer reviewed
evolución, rift, Península Ibérica, Galicia
evolución, rift, Península Ibérica, Galicia
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