North-eastern Morocco: a high geothermal prospect

dc.contributor.authorCorreia, António
dc.contributor.authorRimi, Abdelkrim
dc.contributor.authorZarhloule, Yassine
dc.contributor.authorCarneiro, Júlio
dc.contributor.editorMarques, José Manuel
dc.contributor.editorChambel, António
dc.date.accessioned2018-02-28T11:06:53Z
dc.date.available2018-02-28T11:06:53Z
dc.date.issued2017
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 degrees C/km at depths greater than 300 m. This result confirms the average geothermal gradient estimated in a mining borehole located about 30 km west of the Berkane borehole, in which water with temperatures as high as 96 degrees 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.authoremailnd
dc.identifier.authoremailnd
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dc.identifier.authoremailjcarneiro@uevora.pt
dc.identifier.citationCorreia, A., Rimi, A., Zarhloule, Y., & Carneiro, J. (2017). North-eastern Morocco: a high geothermal prospect. In J. M. Marques & A. Chambel (Eds.), 15th Water-Rock Interaction International Symposium, Wri-15 (Vol. 17, pp. 746-749). Amsterdam: Elsevier Science Bv.por
dc.identifier.doi10.1016/j.proeps.2017.01.003por
dc.identifier.scientificarea247por
dc.identifier.urihttps://www.sciencedirect.com/science/article/pii/S1878522017300036?via%3Dihub
dc.identifier.urihttp://hdl.handle.net/10174/22629
dc.language.isoporpor
dc.peerreviewedyespor
dc.publisherELSEVIER SCIENCE BVpor
dc.rightsopenAccesspor
dc.subjectMoroccopor
dc.subjectGeothermal prospectpor
dc.subjectHeat flow densitypor
dc.subjectGeothermal potential assessmentpor
dc.titleNorth-eastern Morocco: a high geothermal prospectpor
dc.typearticlepor

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