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Facies differentiation caused by wrench deformation along a deep-seated fault system (León line, Cantabrian Mountains, North Spain)
Authors:Jürgen Kullmann  Reinhard Schnenberg
Institution:Jürgen Kullmann,Reinhard Schönenberg
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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