Estructura y evolución del borde sur-occidental de la Fosa de Calatayud-Daroca
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Author
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Publication Date
1988 -
Publisher
Sociedad Geológica de España -
Abstract
The Calatayud-Daroca Basin is located in the Iberian Range. The SW margin of this Basin is the Jiloca fau/t. The evolution of the Basin during the Miocene, was conditioned by dextral slip on this fault. During the Pliocene the Jiloca fault had a normal slip, resulting in the Jiloca Basin formation
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Estructura-y.pdf | 241.0Kb | View/ | There is no description for this item |
Fichero | Tamaño | Formato |
| Description |
---|---|---|---|---|
Estructura-y.pdf | 241.0Kb | View/ | There is no description for this item |