Cuevas, JuliaAranguren, A.Badillo, J. M.Tubía, José María2015-04-142015-04-141997http://hdl.handle.net/10272/10333We report the existence of a thrust system in the central part of the Basque Arc (Basque-Cantabrian basin, Guipúzcoa). From bottom to top, the thrust system is formed by theAia, Pagoeta and Azpeitia allochthonous sheets. The kinematic and structural analysis provides a top to the NE movement, and reveals the widespread reactivation of normal faults during the Pyrenean inversion tectonicsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Thrust systemInversion tectonicsBasque Cantabrian basinTectónica de inversion en el sector central del Arco Vasco (Cuenca Vasco-Cantábrica)Inversion tectonics in the central part of the Basque Arc (Basque-Cantabrian basin)journal articleopen access