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

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....

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Detalhes bibliográficos
Autor principal: Jilali, Abdelhakim (author)
Outros Autores: Rimi, Abdelkrim (author), Zarhloule, Yassine (author), Ouzzaouit, Lalla Amina (author), Barkaoui, Alae (author), Correia, António (author), Carneiro, Júlio (author)
Formato: article
Idioma:por
Publicado em: 2016
Assuntos:
Thermal spring
geothermal gradient
heat flow
Figuig
Morocco
Texto completo:http://hdl.handle.net/10174/16884
País:Portugal
Oai:oai:dspace.uevora.pt:10174/16884
Descrição
Resumo: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.

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