@article{10272/8600,
year = {2006},
url = {http://hdl.handle.net/10272/8600},
abstract = {This study proposes a tectonic reinterpretation of the southwest end of the Cazorla Arc from two different points
of view never used before in external zones of the Betic Cordillera: the paleogeographic study of the Triassic
sedimentary sequences together with the structural analysis of the ductile fabrics developed in clay- and gypsumbearing
Triassic rocks. This new approach has allowed to distinguish two kinematically distinct tectonic episodes
separated in the time: a first strike-slip E-W system of faults followed by a relatively recent strike-slip SE-NW system,
both dextral. The study from these points of view of other similar regions could clarify the origin of the so-called
Triassic chaotic complexes, at the same time that improve the knowledge of the tectonic evolution of the Cordillera},
title = {Estructura y paleogeografía de los materiales del Triásico en la terminación meridional del Arco de Cazorla (Jaén, Cordillera Bética): Implicaciones tectónicas},
title = {Structure and palaeogeography of Triassic materials at the southern end of the Cazorla Arc (Jaén, Cordillera
Bética): Tectonic implications},
author = {Pérez Valera, Fernando and Sánchez Gómez, Mario and Pérez López, Alberto},
}