On the hydrogeothermal structure of the Figuig region (eastern High Atlas, Morocco)

dc.contributor.authorJilali, Abdelhakim
dc.contributor.authorRimi, Abdelkrim
dc.contributor.authorZarhloule, Yassine
dc.contributor.authorOuzzaouit, Lalla Amina
dc.contributor.authorBarkaoui, Alae
dc.contributor.authorCorreia, António
dc.contributor.authorCarneiro, Júlio
dc.date.accessioned2016-01-26T17:04:31Z
dc.date.available2016-01-26T17:04:31Z
dc.date.issued2015-12
dc.description.abstractThis study is to analyze the tectonic, hydrogeological and geothermal circumstances that are causing the upwelling of the thermal springs in the Figuig region whose temperatures range from 27 to 34 °C. From the north, the groundwater flow in carbonated formations is channeled to the oasis of Figuig. These groundwaters emerge thanks to faults under conditions of geothermal gradients and heat flow density ranging from 22 to 35 °C/km and 58-95 mW/m2 respectively.por
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dc.identifier.authoremailjcarneiro@uevora.pt
dc.identifier.citationJilali, A., A. Rimi, Y. Zarhloule, L. A. Ouzzaouit, A. Barkaoui, C. A. and J. Carneiro (2015). "On the hydrogeothermal structure of the Figuig region (eastern High Atlas, Morocco)" Bulletin de l’Institut Scientifique 36: 123-134.por
dc.identifier.issn2458-7184
dc.identifier.scientificarea247por
dc.identifier.urihttp://hdl.handle.net/10174/16884
dc.language.isoporpor
dc.peerreviewedyespor
dc.publisherISR, Rabatpor
dc.rightsrestrictedAccesspor
dc.subjectThermal springpor
dc.subjectgeothermal gradientpor
dc.subjectheat flowpor
dc.subjectFiguigpor
dc.subjectMoroccopor
dc.titleOn the hydrogeothermal structure of the Figuig region (eastern High Atlas, Morocco)por
dc.typearticlepor

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