Caus, E.Teixell, AntonioBernaus, J. M.2016-05-302016-05-301996http://hdl.handle.net/10272/12190The Sopeira Basin is a small extensional basin with a conlinuous record of deposition from the upper Albian to the upper Turonian. In its early stages (upper Albian-middle Cenomanian) the sedimentation was controlled by local factors (extensional tectonics) with an influence of eustatic sea- level change. Later, during the upper Cenomanian-middle Turonian, the main sedimentary features are controlled mainly by global oceanic changesspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/TectonicsEustasyEutrophycationCenomanian-TuronianPyreneesjournal articleopen access