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

• P. Coioma López ^[1] ; J. A. Sánchez Navarro ^[1] ; F. J. Martínez Gii ^[1]
  1. [1] Universidad de Zaragoza

     Universidad de Zaragoza

     Zaragoza, España

     
• Localización: Geogaceta, ISSN 0213-683X, Nº. 20, 3, 1996, págs. 749-752
• Idioma: español
• Títulos paralelos:
  • Geothermal processes taused by groundwater circu/ation a/ong the contact between the Cameros Chain and the Ebro Tertiary Basin
• Enlaces
  • Texto completo (pdf)
• Resumen

  • 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.