Resumen de Diaclasas de tensión regionales en el Complejo Nevado-Filábride y su relación con el contacto Alpujárride/Nevado-Filábride (Sierra Nevada, Cordilleras Béticas)

Jesús Galindo Zaldívar, Francisco González Lodeiro

• Nevado-Filábride rocks have been strained by a NW-SE principal set of systematic tension joints. The orientation of the least principal stress derived from the Nevado­ Filábride/ Alpujárride contact fault gouge agree with the one obtained from joint analysis.