Please use this identifier to cite or link to this item: http://hdl.handle.net/10174/16884

Title: On the hydrogeothermal structure of the Figuig region (eastern High Atlas, Morocco)
Authors: Jilali, Abdelhakim
Rimi, Abdelkrim
Zarhloule, Yassine
Ouzzaouit, Lalla Amina
Barkaoui, Alae
Correia, António
Carneiro, Júlio
Keywords: Thermal spring
geothermal gradient
heat flow
Figuig
Morocco
Issue Date: Dec-2015
Publisher: ISR, Rabat
Citation: Jilali, 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.
Abstract: This 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.
URI: http://hdl.handle.net/10174/16884
ISSN: 2458-7184
Type: article
Appears in Collections:CGE - Publicações - Artigos em Revistas Internacionais Com Arbitragem Científica

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