Tectónica sinsedimentaria en un talud carbonatado con resedimentación gravitatoria en masa (Ibarra, Albiense Inferior, Bizkaía)

Abstract

The 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 Biscay