Soria, Ana RosaLiesa, Carlos L.Meléndez Hevia, AlfonsoMeléndez Hevia, María Nieves2023-06-202023-06-2020011576-5172https://hdl.handle.net/20.500.14352/57943The sedimentary record o f El Castellar Fm. in the Calve subbasin has been divided into two stages according to the presence of a mudstone and gypsum interval. This interval represents a paleogeographic and structural significative change. The geometry and facies distribution were controlled by extensional faults. However, the first stage shows a great variety of subenvironments and facies, while the second stage is characterized by an extensive hard water lake. These evidences has been interpreted as the result of the independent movement o f the faults during the first stage and the movement o f the whole extensional faults on a sole detachment during the second stage.spajournal articlehttp://www.sociedadgeologica.es/publicaciones_geotemas.htmlopen access551.763Syntectonic sedimentationEarly CretaceousListric normal fault systemTransfer faultIberian BasinGeología estratigráfica2506.19 Estratigrafía