Santamaría Casanovas, J.Remacha Grau, Eduard2017-08-072017-08-071994http://hdl.handle.net/10272/14015The "Nivel de Fuentes", in the Valdelacasa Allogroup (Precambrian-Cambrian), can be divided in five subunits. Each one of them is build-up by a basal megabreccia overlaid by a fine-grained turbidite wedge that tends to pinch-out toward the central region of the Valdelacasa anticline. The isochron character ofthe "Nivel de Fuentes" is rejected because really it is multieventspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/MegabrecciaNivel de FuentesSeismic-eventPrecambrian-CambrianCentral-lberian Zonejournal articleopen access