Sanz Rubio, E.Hoyos, M.Cañaveras, J.C.Sánchez Moral, S.2017-03-212017-03-211995http://hdl.handle.net/10272/13488Soft sediment deformation structures are described in a dolomitic palustrine-lacustrine sequence in the neogene Calatayud basin. Pseudoanticlines with associated dish structures are possibly result of a fluidization process related with groundwater saline flows proceeding from an adjacent evaporitic paleoreliefspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Deformation structuresPseudoanticlinesFluidizationCalatayud basinMioceneEstructuras pseudoanticlinales inducidas por fluidificación en la Unidad Intermedia de la cuenca de CalatayudPseudoanticlines structures induced by fluidization in the Intermediate Unit of the Calatayud basinjournal articleopen access