North-eastern Morocco: a high geothermal prospect.

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dc.contributor.authorCorreia, António
dc.contributor.authorRimi, Abdelkrim
dc.contributor.authorZarhloule, Yassine
dc.contributor.authorCarneiro, Júlio F.
dc.contributor.editorMarques, José Manuel
dc.contributor.editorChambel, António
dc.date.accessioned2017-01-30T12:21:48Z
dc.date.available2017-01-30T12:21:48Z
dc.date.issued2016-10-16
dc.description.abstractNew temperature data obtained in 2007 in a hydrogeological borehole (1100 m deep) near Berkane have revealed an average geothermal gradient of about 126°C/km at depths greater than 300 m. This result confirms the average geothermal gradient estimated in a mining borehole located about 30km west of the Berkane borehole, in which water with temperatures as high as 96°C was reached at a depth of about 700 m. The new geothermal gradient, exceeding by far the ones already determined for this Moroccan area allows thinking about the possibility of programs for using high temperature waters in north-eastern Morocco.por
dc.identifier.authoremailcorreia@uevora.pt
dc.identifier.authoremailnd
dc.identifier.authoremailnd
dc.identifier.authoremailjcarneiro@uevora.pt
dc.identifier.citationCorreia, A., Rimi, A., Zarhloule, Y., & Carneiro, J. (2016). North-eastern Morocco: a high geothermal prospect. Paper presented at the 15th Water Rock Interaction, Évora, Portugal.por
dc.identifier.scientificarea393por
dc.identifier.urihttp://www.wri15portugal.org/
dc.identifier.urihttp://hdl.handle.net/10174/20228
dc.language.isoporpor
dc.peerreviewedyespor
dc.publisherUniversidade de Évorapor
dc.rightsopenAccesspor
dc.subjectMoroccopor
dc.subjectGeothermal prospectpor
dc.subjectHeat flow densitypor
dc.subjectGeothermal potential assessmentpor
dc.titleNorth-eastern Morocco: a high geothermal prospect.por
dc.typearticlepor

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