Benavente Herrera, JoséCarrasco Cantos, FranciscoAlmécija Ruiz, CarmenRodríguez Jiménez, P.Cruz Sanjulián, J. J.2017-08-172017-08-171993http://hdl.handle.net/10272/14043The results of temperature and electrical conductivit y logs carrie dout in some recently drilled boreholes across the northern shoreline of the Fuente de Pledra Salt Lake, provid e the first data a bout a relative lythick transition zone between the freshw ater of the regional underground flow and the dense brine bodies occurring beneath the lake floor. Water-head values also point out to the reflux of brines flowing up along the hypothetical Chyben-Herzberg interfacespaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Groundwater flowTransition zoneBrinesSalt lakejournal articleopen access