Resumen de Isopiezas y direcciones del flujo regional en el acuífero carbonatado mesozoico del margen Ibérico de la Depresión del Ebro.

José Ángel Sánchez Navarro, Javier San Román Saldaña, J. L. de Miguel Cabeza, Antonio Pérez García, Francisco Javier Martínez Gil

• Groundwater discharge from the Iberian Chain into the Ebro tertiary basin takes place through the mesozoic carbonated rocks. These rocks extend from La Rioja to the Mediterranean sea. In this work, it is shown the Jurassic aquifer equipotential levels map as well as the groundwater flow directions. The recharge and discharge areas, the aquifer-river relationship, and the hydrogeological limits of the aquifer are also shown