Contribución de los datos isotópicos al conocimiento hidrogeológico del sector Caspe-Maella

Thumbnail Image

Files

Contribucion.pdf (688.56 KB)

Publication date

1998

Authors

Advisors

Department

Research group

Center

Metrics

Google Scholar

Export

Research Projects

Organizational Units

Journal Issue

URI

http://hdl.handle.net/10272/10160

Abstract

The isotopie ratios of 180/16 O and 2H/1H, confirms the discharge of a regional carbonate aquifer in the Caspe - Maella area. 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

Keywords

Isotopie ratios wO/u O and 2H/H; Groundwater discharge; Regional aquifer; Iberian Chain; Caspe - Maella sector

Unesco Subjects

Bibliographic citation

Collections

Geogaceta -- Nº 25, (1998)
Atribución-NoComercial-SinDerivadas 3.0 España
The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España