RT Journal Article
T1 Isopiezas y direcciones del flujo regional en el acuífero carbonatado mesozoico del margen Ibérico de la Depresión del Ebro
T1 Equipotencial levels and groundwater flow directions in the mesozoic carbonated aquifer from the Iberian chain into the Thro Tertiary basin
A1 Sánchez Navarro, José Ángel
A1 San Román, J.
A1 Miguel, J. L. de
A1 Pérez Muñoz, Antonio
A1 Martínez Gil, F. J.
AB 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
PB Sociedad Geológica de España
YR 1991
FD 1991
LK http://hdl.handle.net/10272/17990
UL http://hdl.handle.net/10272/17990
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026