Resumen de Procesos geotérmicos causados por la circulación del agua subterránea en el contacto entre la Sierra de Cameros y la Depresion Terciaria del Ebro

Pablo Coloma López, José Ángel Sánchez Navarro, Francisco Javier Martínez Gil

• he 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 clase cooperatíon at the interpretation of geotherma/ anomalies. In this work it is show an example: the geothermal processes along the Cameros Chain/Ebro Tertiary Basin contact.