Browsing by Author "Torcal, F."

Now showing items 1-2 of 2

Esfuerzos recientes en el sector sudoriental de la Depresión de Granada (Cordillera Bética central)

Galindo Zaldívar, Jesús; Jabaloy, A.; Serrano, I.; Morales, J.; González Lodeiro, Francisco; Torcal, F. (Sociedad Geológica de España, 1997)

The analysis of the seismic activity and the microtectonic study of outcrops located in the southeastern Granada Depression show that the stress states have been heterogeneous from the Upper Miocene up to the present. NE-SW ...
Las fallas del recinto de la Alhambra

Azañón, José Miguel; Azor, A.; Booth Rea, G.; Martín Rosales, Wenceslao; Justo Alpaflés, J. L. de; Torcal, F.; Torcal, M. (Sociedad Geológica de España, 2003)

The Alhambra is built on a conglomeratic formation, known as the Alhambra Formation, whose age is Pliocene to Lower Pleistocene and has a visible thickness of 200 metres. The western part of the San Pedro escarpment ...

Now showing items 1-2 of 2

Esfuerzos recientes en el sector sudoriental de la Depresión de Granada (Cordillera Bética central)

Galindo Zaldívar, Jesús; Jabaloy, A.; Serrano, I.; Morales, J.; González Lodeiro, Francisco; Torcal, F. (Sociedad Geológica de España, 1997)

The analysis of the seismic activity and the microtectonic study of outcrops located in the southeastern Granada Depression show that the stress states have been heterogeneous from the Upper Miocene up to the present. NE-SW ...
Las fallas del recinto de la Alhambra

Azañón, José Miguel; Azor, A.; Booth Rea, G.; Martín Rosales, Wenceslao; Justo Alpaflés, J. L. de; Torcal, F.; Torcal, M. (Sociedad Geológica de España, 2003)

The Alhambra is built on a conglomeratic formation, known as the Alhambra Formation, whose age is Pliocene to Lower Pleistocene and has a visible thickness of 200 metres. The western part of the San Pedro escarpment ...