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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)

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author: David A. Foster  Ícaro Dias da Silva  Rubén Díez Fernández 

Publication date August 21, 2015
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