Estructuras pseudoanticlinales inducidas por fluidificación en la Unidad Intermedia de la cuenca de Calatayud
Loading...
Publication date
Advisors
Department
Research group
Center
Related publication
Metrics
Export
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
Unesco Subjects
Bibliographic citation
Collections
The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España