Génesis y evolución de la fosa de la Cerdanya (Pirineos Orientales)
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Author
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Publication Date
1986 -
Publisher
Sociedad Geológica de España -
Abstract
The Cerdanya basin is located at the SW end of the Tet fault, in its NW block. Its formation, during the Upper Miocene, was conditioned by dextral slip of this fault anf the normal slip of E-W trending faults that absorbed the movement of the former
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Genesis.pdf | 147.3Kb | View/ | There is no description for this item |
Fichero | Tamaño | Formato |
| Description |
---|---|---|---|---|
Genesis.pdf | 147.3Kb | View/ | There is no description for this item |