Paleoesfuerzos alpinos en el borde suroccidental de la cuenca de Madrid (Montes de Toledo)
Loading...
Publication date
Authors
Advisors
Department
Research group
Center
Metrics
Export
Abstract
The paleostress analysis are used here to outline the Alpine deformation of the contact between the Toledo Mountains and the Madrid Basin. This limit results from a system of E-W-trending reverse faults, NW-SE-trending dextral normal strike-slip faults and NNE-SSW-trending sinistral normal strike-slip faults
Unesco Subjects
Bibliographic citation
Collections
The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España