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![](./images/clear.gif) 1.- Tectonic evolution of the upper allochthon of the Ordenes Complex (northwestern Iberian Massif); structural constraints to a polyorogenic peri-Gondwanan terrane
Geological Society of America (GSA); Boulder, CO; USA; United States, 2007
The evolution of the Rheic Ocean; from Avalonian-Cadomian active margin to Alleghenian-Variscan collision
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