Sobre la hidroquímica de la cuenca del río Almanzora (Almería)

dc.contributor.authorCastillo, A.
dc.contributor.authorVallejos, Ángela
dc.contributor.authorCerón García, Juan Carlos
dc.date.accessioned2017-08-21T11:19:36Z
dc.date.available2017-08-21T11:19:36Z
dc.date.issued1993
dc.description.abstractThe waters of the Almanzora basin have very different chemistry according to the hydrogeological context; the mineralization is between 0,4 and more than 6 g/i; the hydrochemical facies is usually . calcic, bicarbonated in the carbonated aquifers, of lower salinity, and sulphated for the detritic aquifers and surface waters. Mild regional thermal ism also occurs with emergence temperatures usually ranging between 20 and 28º Ces_ES
dc.identifier.urihttp://hdl.handle.net/10272/14061
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherHydrochemistryes_ES
dc.subject.otherThermalismes_ES
dc.subject.otherAlmanzora basines_ES
dc.titleSobre la hidroquímica de la cuenca del río Almanzora (Almería)es_ES
dc.titleSome considerations about the hydrochemistry of the Almanzora basin (Almería)eng
dc.typejournal articlees_ES
dspace.entity.typePublication
relation.isAuthorOfPublicationd749adc5-e6c8-455b-8150-25433ece3f13
relation.isAuthorOfPublication.latestForDiscoveryd749adc5-e6c8-455b-8150-25433ece3f13

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