Los manantiales termominerales de Salar (Granada). Un sistema de flujo profundo ligado esencialmente a la descarga de Sierra Gorda

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dc.contributor.authorLópez Chicano, Manuel
dc.contributor.authorPulido Bosch, Antonio
dc.date.accessioned2017-04-04T09:55:41Z
dc.date.available2017-04-04T09:55:41Z
dc.date.issued1995
dc.description.abstractWithin the framework of the geometry and functioning of the carbonate aquifer of the Sierra Corda (Granada, Spain) the discharge zone o f Salar has outstanding anomalous characteristics — in geothermal, hydrochemical, isotope and hydrodynamic terms— with respect to the other springs which drain the aquifer. Monitoring of the principal physico-chemical characteristics of the springs during more than one hydrological cycle indicates the deep mixing of waters before dischargeen_US
dc.identifier.urihttp://hdl.handle.net/10272/13543
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGeothermal anomalyen_US
dc.subject.otherHydrogeochemistryen_US
dc.subject.otherDeep flowen_US
dc.subject.otherCarbonate aquifersen_US
dc.titleLos manantiales termominerales de Salar (Granada). Un sistema de flujo profundo ligado esencialmente a la descarga de Sierra Gordaen_US
dc.titleThe thermomineral springs of Salar (Granada, Spain). A deep-flow system linked to the discharge of Sierra Gordaeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 18, (1995)