Facies differentiation caused by wrench deformation along a deep-seated fault system (León line, Cantabrian Mountains, North Spain) |
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Authors: | Jürgen Kullmann Reinhard Schnenberg |
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Institution: | Jürgen Kullmann,Reinhard Schönenberg |
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Abstract: | The “León line” is a deep-seated fault system in the Variscan orogen of the Canta-brian Mountains. This fault system appears to have been active at least from the early Devonian to the end of the Carboniferous. Vertical as well as horizontal movements resulted in a strikingly different development of facies conditions to the north and south of the Leon line. |
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