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

1. Sanz Rubio, Enrique
2. Hoyos Gómez, Manuel
3. Cañaveras, Juan Carlos
4. Sánchez Moral, Sergio

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lock_openArias Montano externo

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Abstract

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

Data source: Dialnet