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![](./images/clear.gif) 1.- The ca. 350 Ma Beja igneous complex; a record of transcurrent slab break-off in the southern Iberia Variscan belt?
Elsevier; Amsterdam; NLD; Netherlands, 2008
Evolution and closure of the Rheic Ocean; Palaeozoic drift of peri-Gondwanan terranes and Alleghenian-Variscan orogenic processes
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