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