| Registros del 1 al 6 de 6 encontrados |
1.- A PERI-GONDWANAN ARC ACTIVE IN CAMBRIAN-ORDOVICIAN TIMES: THE EVIDENCE OF THE UPPERMOST TERRANE OF NW IBERIA
INSTITUTO GEOLOGICO DE ESPAÑA; MADRID; ESP, 2011
ORDOVICIAN OF THE WORLS
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2.- A peri-Gondwanan arc in NW Iberia; I, Isotopic and geochemical constraints on the origin of the arc; a sedimentary approach
Elsevier on behalf of International Association for Gondwana Research; Amsterdam and Kochi; III; Int, 2010
The Rheic Ocean; Palaeozoic evolution from Gondwana and Laurussia to Pangaea
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3.- A peri-Gondwanan arc in NW Iberia; II, Assessment of the intra-arc tectonothermal evolution through U/Pb SHRIMP dating of mafic dykes
Elsevier on behalf of International Association for Gondwana Research; Amsterdam and Kochi; III; Int, 2010
The Rheic Ocean; Palaeozoic evolution from Gondwana and Laurussia to Pangaea
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4.- Fabric development in a Middle Devonian intraoceanic subduction regime; the Careon Ophiolite (northwest Spain)
University of Chicago Press; Chicago, IL; USA; United States, 2010
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5.- THE BASAL TECTONIC MELANGE OF THE CABO ORTEGAL COMPLEX (NW IBERIAN MASSIF): A KEY UNIT IN THE SUTURE OF PANGEA
2009
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6.- The Corredoiras Orthogneiss (NW Iberian Massif); geochemistry and geochronology of the Paleozoic magmatic suite developed in a peri-Gondwanan arc
Elsevier; Amsterdam; NLD; Netherlands, 2012
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