Gómez Pérez, I.Fernández Mendiola, Pedro ÁngelGarcía Mondéjar, Joaquín2017-11-102017-11-101992http://hdl.handle.net/10272/14148The analysis of fades and thickness distribution in carbonate slope systems of the Albian of Ibarra (Bizkaia) indicates active synsedimentary faulting. E-W extensional faults separate blocks that record tilting and depocenter shifts through time. This local extension occurs associated to major NW-SE strike-slip sinistral movements linke d to the opening of the Bay o f BiscayspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Carbonate slopeLower AlbianSynsedimentary faultsMegabrecciasjournal articleopen access