Evaluación del flujo geotérmico en manantiales de Aragón

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dc.contributor.authorSánchez Navarro, José Ángel
dc.contributor.authorColoma, Pablo
dc.contributor.authorPérez García, Adán
dc.contributor.authorLeiva Juán, A. de
dc.date.accessioned2015-02-18T09:29:32Z
dc.date.available2015-02-18T09:29:32Z
dc.date.issued1999
dc.description.abstractThe geothermal flow wich emerges by convection at the springs in Aragon is evaluated, and compared with the theoretical heat flow wich penetrates the surface of the region by conduction. The geological materials through wich the convection takes place are defined (geothermal formations), and the areas where thermal convection appears most intensely are relateden_US
dc.identifier.urihttp://hdl.handle.net/10272/9950
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 flowen_US
dc.subject.otherSpringsen_US
dc.subject.otherConductionen_US
dc.subject.otherConvectionen_US
dc.subject.otherGeothermal formationsen_US
dc.titleEvaluación del flujo geotérmico en manantiales de Aragónen_US
dc.titleEvaluation of geothermal flow at the springs in Aragoneng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 27, (1999)