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• W2078978679 abstract "In the Betic Cordillera, the initial thickening of the Alborán Domain produced an Alpine high pressure-low temperature (HP-LT) metamorphism in the Alpujárride and Nevado-Filábride complexes. After 19 Ma this thickening process evolved to an extensional stage with uplift rates of between 1 and 2 mm year−1. The extensional stage generated structures in a heterogeneous shear regime with a top-to-the-west sense of movement. The present-day Alpujárride-Nevado-Filábride contact is a detachment fault generated in this shearing regime. In the footwall, the first structure developed in this extensional stage is a planar-linear fabric characterized by constrictive strain, that is axial planar to kilometric recumbent tight to isoclinal folds. The planar-linear fabric is folded by inclined close to open folds with axes parallel to the stretching lineation. The planar-linear fabric and folds are deformed by a late extensional crenulation cleavage near the detachment surface. Finally, brittle deformation was generated within the same kinematic framework as that of the ductile structures. In the hanging wall, meanwhile, deformation had a brittle character producing faults and joints." @default.
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• W2078978679 date "1993-03-01" @default.
• W2078978679 modified "2023-10-18" @default.
• W2078978679 title "The Alpujárride-Nevado-Fibábride extensional shear zone, Betic Cordillera, SE Spain" @default.
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• W2078978679 doi "https://doi.org/10.1016/0191-8141(93)90148-4" @default.
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