Condicionantes estructurales de la unidad hidrogeológica del Campo de Montiel (Provincias de Ciudad Real y Albacete)

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dc.contributor.authorRincón Calero, P. J.
dc.contributor.authorMontero, E.
dc.contributor.authorVegas, Ramón
dc.date.accessioned2016-11-22T11:15:56Z
dc.date.available2016-11-22T11:15:56Z
dc.date.issued1996
dc.description.abstractThe type of crustal deformation in the Campo de Montiel can assistin the understanding of the internal features of the main aquifer developed in the Jurassic carbonate platform . The direction of subsurface flow, the transmisivity and internal subdivision of the aquifer are interpreted in terms of cover and whole crust flexures as well as N140E directed transverse fault and fracture zonesen_US
dc.identifier.urihttp://hdl.handle.net/10272/12868
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.otherIntraplate deformationen_US
dc.subject.otherJurassic limestonesen_US
dc.subject.otherAquiferen_US
dc.subject.otherHidrological featuresen_US
dc.titleCondicionantes estructurales de la unidad hidrogeológica del Campo de Montiel (Provincias de Ciudad Real y Albacete)en_US
dc.titleStructural constrains for the hydrogeoiogical unit of the Campo de Mondei (Provs. Ciudad Real and Albacete)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-6, (1996)