Procesos geotérmicos causados por la circulación del agua subterránea en el contacto entre ¡a Sierra de Cameros y la Depresión Terciaria del Ebro

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dc.contributor.authorColoma, Pablo
dc.contributor.authorSánchez Navarro, José Ángel
dc.contributor.authorMartínez Gil, F. J.
dc.date.accessioned2016-06-20T10:59:54Z
dc.date.available2016-06-20T10:59:54Z
dc.date.issued1996
dc.description.abstractThe practically important part of geothermal systems belong to the convective type where the termal energy is transported by movement of groundwater. Both geothermics and hydrology (aquifer geometry and groundwater flow patterns) should be in very close cooperation at the Interpretation of geothermal anomalies. In this work it is show an example: the geothermal processes along the Cameros Chain/Ebro Tertiary Basin contacten_US
dc.identifier.urihttp://hdl.handle.net/10272/12390
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 systemsen_US
dc.subject.otherConvectiveen_US
dc.subject.otherGroundwateren_US
dc.subject.otherCameros Chain/Ebro Tertiaren_US
dc.subject.otherBasin contacten_US
dc.titleProcesos geotérmicos causados por la circulación del agua subterránea en el contacto entre ¡a Sierra de Cameros y la Depresión Terciaria del Ebroen_US
dc.titleGeothermal processes caused by groundwater circulation along the contact between the Cameros Chain and the Ebro Tertiary Basineng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-3, (1996)