Le karst dans les gypses de Sorbas (Almeria). Aspects morphologiques et hydrogéologiques
Les gypses du bassin néogène de Sorbas présentent de nombreuses cavités karstiques ainsi que des tumulus , bombements de la couche superficielle de gypse. La dénudation karstique actuelle est évaluée à 260 m3/km2/an. - (AW)
The Sorbas massif (Almeria, SE Spain) is one of most karstified gypsiferous areas of the world, with hundreds of dolines and different karst features. In this massif more than 1000 caves have been discovered in an area of about 12 km2. Its Messinian
for better understanding the role of the karst aquifer in the groundwater recharge of the Aguas River. This study took place in the southern part of the Sorbas gypsum plateau with several steps and multiple field campaigns for geo-morphological
Adjustment of a drainage network to capture induced base-level change : an example from the Sorbas Basin, SE Spain
Quaternary catchments in the south of the Sorbas Basin, SE Spain have been affected by 2 regionally significant river captures. The river captures were triggered by changes in regional gradients associated with sustained Quaternary uplift
U-series dating of immature and mature calcretes as a basis for constructing Quaternary landform chronologies for the Sorbas basin, southeast Spain
Immature and mature calcretes from an alluvial terrace sequence in the Sorbas basin were dated by the U-series isochron technique. By using this technique to date calcretes that have formed during terrace aggradation and at the terrace surface after
The river drains 2 interconnected Neogene sedimentary basins, the Sorbas and Almeria basins, and crosses 2 major geological structures, the Sierras de Alhamilla/Cabrera and the Carboneras Fault Zone. Regional epeirogenic uplift resulted in sustained