RT Journal Article
T1 Hidrogeología del Sector Caspe-Maeíla. Primeros Resultados
T1 Hidrogeology Of Caspe-Maella Sector. First Outputs
A1 Baquer, E.
A1 Coloma, Pablo
A1 Sánchez Navarro, José Ángel
A1 Miguel, J. L. de
AB The existence of a structural high in the Caspe- Maella area, related with the palaeozoic outcrop of Puigmoreno provokes the groundwater discharge of the carbonate mesozoic aquifer (regional aquifer).The recharge area of this aquifer takes place in the Iberian Chain and the discharge takes place through low permeable tertiary detritical material of Ebro Basin
PB Sociedad Geológica de España
YR 1997
FD 1997
LK http://hdl.handle.net/10272/10245
UL http://hdl.handle.net/10272/10245
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026