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1.- Crustal growth and deformational processes in the northern Gondwana margin; constraints from the Evora Massif (Ossa-Morena Zone, southwest Iberia, Portugal)
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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