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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)

Dias da Silva, Ícaro ; Díez Fernández, Rubén ; Díez Montes, Alejandro ; González Clavijo, Emilio ; Foster, David A. | Springer Science Business Media | 2016-06

LA-MC-ICP-MS U–Pb zircon ages and wholerock geochemical data obtained from volcanic rocks erupted in the northern margin of Gondwana provide new insights on the polyphase magmatic evolution of the NW Iberian domain during the establishment of pa[...]

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Peralkaline and alkaline magmatism of the Ossa-Morenazone (SW Iberia): Age, source, and implications for thePaleozoic evolution of Gondwanan lithosphere

Díez Fernández, Rubén ; Pereira, Manuel Francisco ; Foster, David A. | Geological Society of America. | 2015-02

The Ossa-Morena zone in SW Iberia represents a section of the northern margin of West Gondwana that formed part of a Cordilleran-type orogenic system during the Neoproterozoic (Cadomian orogeny). The crustal section in this zone preserves the re[...]

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