Thesis Collection
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Browsing by Author "García Tortosa, F.J."
Now showing items 1-6 of 6
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Las unidades alpujárrídes y maláguides entre Cabo Cope y Cabo de Palos (Murcia, España)
(Sociedad Geológica de España, 1999)According to their stratigraphic characters and tectonic positions, the Alpujarride units existing in this area are reduced to three units "type" that, cited from bottom to top, are: Peñas Blancas, Cabo Tiñoso and Portman ... -
Nueva evidencia sobre la edad del tránsito endorreico-exorreico de la cuenca de Guadix-Baza
(2008)The Guadix-Baza basin was an endorheic continental basin during the Pliocene and part of the Pleistocene, later being captured by a tributary of the Guadaquivir River which would turn into the Guadiana Menor River. This ... -
Nuevos datos para la estimación de los valores de levantamiento desde el Tortoniense Superior a la actualidad en la parte centro-occidental de la Sierra de Carrascoy (provincia de Murcia)
(Sociedad Geológica de España, 1997)The existence of sediments of the Late Tortonian near the top, and in the slopes, of Sierra de Carrascoy, deposited above a former erosionaI surface excavated in the basement, permits precise estimation of the vertical ... -
Origen de las simas de Partagat (Sierra de Aitana, Alicante)
(2006)The Partagat chasms, located at the highest part of the Sierra de Aitana (Province of Alicante), are large joints which have opened up in Eocene limestone. They measure up to 15-20 metres in width and dozens of metres ... -
Tasas de deformación GPS en la cuenca del Bajo Segura (Cordillera Bética oriental)
(Sociedad Geológica de España, 2014)We estimate the present deformation rates ofthe Bajo Segura Basin (NE end of the Eastern Betic shear zone), from the analysis of a GPS network with 11 sites. We analyze the data from four observation campaigns carried out ... -
Tectónica reciente en el frente de Cabalgamiento Bético. Las deformaciones de Jimena y Bedmar (Jaén)
(2008)In the area of Jimena-Bedmar, in the Guadalquivir basin, the northwards displacement of the External Betic units deformed the sedimentary Miocene infilling of the basin. Especially remarkable is an E-W anticline affecting ...
