Estructuras sigmoïdes en el macizo granítico hercínico de Cauterets-Panticosa (Pirineos)
Sigmoid structures in the Hercynian Cauterets-Panticosa granité (Pyrenees)
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Author
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Publication Date
1996 -
Publisher
Sociedad Geológica de España -
Abstract
The emplacement of the Cauterets-Panticosa granite massif (western Pyrenees) was controlled by dextral, 100° E-trending shear zones. The anisotropy of magnetic susceptibility allows us to obtain detailed structural maps of foliation trajectories and magmatic lineations of the Cauterets-Panticosa massif. Both types of structures draw large-scale sigmoid structures related to the dextral shear zones
Fichero | Tamaño | Formato |
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Estructuras.pdf | 278.7Kb | View/ |
Fichero | Tamaño | Formato |
| Description |
---|---|---|---|---|
Estructuras.pdf | 278.7Kb | View/ |