Resumen de Estructuras pseudoanticlinales inducidas por fluidificación en la Unidad Intermedia de la cuenca de Calatayud

Enrique Sanz Rubio, Manuel Hoyos Gómez, Juan Carlos Cañaveras, Sergio Sánchez Moral

• Soft 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 paleorelief