Alpine kink bands on foliated rocks of the Central System variscan basement
DOI:
https://doi.org/10.55407/geogaceta102340Keywords:
kink bands, alpine thrusts, Central SystemAbstract
The spatial and kinematic association between kink bands in rocks with variscan foliation and alpine thrusts in the Central System basement, allow us to deduce that the former have a Cenozoic age, and not variscan or late-variscan. Systematically, the fold axes trend of the kinks is sub-parallel to the strike of the thrusts. Three key outcrops are studied: the Villares de Jadraque thrust, the Valdesotos thrust and the El Atazar back-thrust.
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