Contexto tectónico del "Parque Natural de las Lagunas de Ruidera" (acuífero del Campo de Montiel)

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dc.contributor.authorRincón Calero, P. J.
dc.contributor.authorMontero, E.
dc.contributor.authorVegas, Ramón
dc.date.accessioned2014-12-12T10:35:50Z
dc.date.available2014-12-12T10:35:50Z
dc.date.issued2001
dc.description.abstractThe spatial distribution of the drainage pattern, the subsurface flow and the maximum values of transmisivity in the aquifer of El Campo de Montiel, as well as the localisation of the springs of the Lagunas de Ruidera, can be explained as a result of the activity of a weak intraplate compressive stress field transmitted from the Betic borderen_US
dc.identifier.urihttp://hdl.handle.net/10272/9521
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.otherCampo de Montielen_US
dc.subject.otherIntraplate deformationen_US
dc.subject.otherAquiferen_US
dc.subject.otherGeomorphic indices of recent active tectonicsen_US
dc.titleContexto tectónico del "Parque Natural de las Lagunas de Ruidera" (acuífero del Campo de Montiel)en_US
dc.titleTectonic setting of the "Parque Natural de las Lagunas de Ruidera" (Campo de Montiel aquifer)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 30, (2001)