Magmatic evolution in the N-Gondwana margin related to the opening of the Rheic Ocean—evidence from the Upper Parautochthon of the Galicia-Trás-os-Montes Zone and from the Central Iberian Zone (NW Iberian Massif)
Instituto Dom Luiz, Faculdade de Ciências da Universidade de Lisboa, Campo Grande, Edifício C8, Piso 3, Lisbon, Portugal; Departamento de Geociências, Instituto Dom Luiz, ECT, Universidade de Évora, Apartado 94, Évora, Portugal; Department of Geological Sciences, University of Florida, P.O. Box 112120, Gainesville, FL, United States; Instituto Geológico y Minero de España, Unidad de Salamanca, Azafranal, 48, Salamanca, Spain
Recommended Citation:
Dias da Silva Í.,Díez Fernández R.,Díez-Montes A.,et al. Magmatic evolution in the N-Gondwana margin related to the opening of the Rheic Ocean—evidence from the Upper Parautochthon of the Galicia-Trás-os-Montes Zone and from the Central Iberian Zone (NW Iberian Massif)[J]. International Journal of Earth Sciences,2016-01-01,105(4)