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Estructura en escamas del sector noroccidental de la Sierra de Cazorla (zona prebética) y del borde de la depresión del Guadalquivir (provincia de Jaén)

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1970
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Granada : Secretariado de Publicaciones de la Universidad, C.S.I.C, Sección de Geología de la Facultad de Ciencias
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Abstract
The succession of different stages of deformation, the last of them having taken place in the middle Miocene, has determined the imbricated structure of the Sierra de Cazorla and the easternmost boundary of the Guadalquivir Basin. The evolution of the structural features is analyzed and a tectonic interpretation of the resulting structure is attempted.
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