López Horgue, Mikel A.Fernández Mendiola, Pedro ÁngelGarcía Mondéjar, Joaquín2015-04-092015-04-091997http://hdl.handle.net/10272/10293A detailed mapping of the Zufia Formation near Estella-Lizarra (Navarra) has led to the discovery of a shallow-water marine carbonate-terrigenous unit of early Cenomanian age. The Aramendia unit consists basically of calcarenites. Facies analysis, lateral and vertical distribution are used to build a sedimentary model of a carbonate shoal. The calcarenitic shoal separates two principal domains: 7/ to the south, a back-shoal trough with calcarenitic material exported from the shoal and terrigenous input derived from the terrestrial hinterland, and 2/ a deeper fore-shoal trough with marly sedimentation and occasional intercalation of shoal derived beds. This fore-shoal area is devoid of terrigenous input after the shoal-barrier effect. A tectonic control influenced the foundation of the shoal on a structural paleohighspaAn error occurred on the license name.An error occurred getting the license - uri.Carbonate shoalSedimentary modelTectonic controlLower CenomanianEstella-LizarraSpainjournal articleopen access