Apraiz, A.2016-06-292016-06-291996http://hdl.handle.net/10272/12438The Lora del Rio metamorphic core is located in the easternmost part of the Monesterio Antiform. A detailled structural and metamorphic study combined with cartographic data enable the characterization of 3 different units. These units reflect a first tectonic event of crustal thickening during the hercynian orogenic phase and the unroofing of the thickened crust by subsequent extensional deformationspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Extensional tectonismMigmatic domeOssa-Morena ZoneHercynian Massifjournal articleopen access