Sondeos de investigación en un acuífero kárstico costero (Castell de Ferro, Granada)

dc.contributor.authorPulido Bosch, Antonio
dc.contributor.authorPulido Leboeuf, P.
dc.contributor.authorVallejos, Ángela
dc.contributor.authorCalvache Quesada, María Luisa
dc.contributor.authorGisbert, Josep
dc.contributor.authorAndreu Rodes, José Miguel
dc.contributor.authorSánchez Martos, Francisco
dc.contributor.authorMolina, Luis
dc.date.accessioned2015-03-27T12:53:10Z
dc.date.available2015-03-27T12:53:10Z
dc.date.issued1998
dc.description.abstractData from 4 investigation boreholes, drilled in the marbles of the Castell de Ferro aquifer and separated some 5 m each one from the next one, are discussed. Several karstic discontinuities are detected at different depths depending on which borehole they are in. Flowmeter measurements show the presence of vertical flows at different positions. An electrical conductivity anomaly is detected and interpreted as a result of the drilling methoden_US
dc.identifier.urihttp://hdl.handle.net/10272/10199
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.otherDown the hole hammeren_US
dc.subject.otherKarsten_US
dc.subject.otherWell loggingen_US
dc.subject.otherVertical flowsen_US
dc.titleSondeos de investigación en un acuífero kárstico costero (Castell de Ferro, Granada)en_US
dc.typejournal articleen_US
dspace.entity.typePublication

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