Estudio hidrogeolögico de la zona de Sa Marineta (Isla de Mallorca)

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dc.contributor.authorGelabert, B.
dc.contributor.authorRodríguez Perea, A.
dc.date.accessioned2014-12-09T13:06:32Z
dc.date.available2014-12-09T13:06:32Z
dc.date.issued2001
dc.description.abstractSa Marineta aquifer (NE of Mallorca) has high values of transmissivity (> 10000 m2/d) and low gradient. Groundwater flows from the Llevant Ranges to the center of the aquifer and to the sea. Vertical registers of temperature and electrical conductivity logs has allowed to recognize a marine wedge, up to 8.5 km into the land. Brackish water exists in a 3 km belt parallel to the coastline. The rest of the aquifer has good quality fresh wateren_US
dc.identifier.urihttp://hdl.handle.net/10272/9485
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.otherCross-sectionen_US
dc.subject.otherPiezometric mapen_US
dc.subject.otherHydrological profileen_US
dc.subject.otherElectrical conductivity logsen_US
dc.subject.otherStiff diagramsen_US
dc.titleEstudio hidrogeolögico de la zona de Sa Marineta (Isla de Mallorca)en_US
dc.titleHydrogeological study of Sa Marineta area (Mallorca island)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 31, (2001)