Procesos geotérmicos causados por la circulación del agua subterránea en el contacto entre ¡a Sierra de Cameros y la Depresión Terciaria del Ebro

Abstract

The practically important part of geothermal systems belong to the convective type where the termal energy is transported by movement of groundwater. Both geothermics and hydrology (aquifer geometry and groundwater flow patterns) should be in very close cooperation at the Interpretation of geothermal anomalies. In this work it is show an example: the geothermal processes along the Cameros Chain/Ebro Tertiary Basin contact