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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Bibliographic Details
Main Author: Jilali, Abdelhakim (author)
Other Authors: Rimi, Abdelkrim (author), Zarhloule, Yassine (author), Ouzzaouit, Lalla Amina (author), Barkaoui, Alae (author), Correia, António (author), Carneiro, Júlio (author)
Format: article
Language:por
Published: 2016
Subjects:
Thermal spring
geothermal gradient
heat flow
Figuig
Morocco
Online Access:http://hdl.handle.net/10174/16884
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/16884

Internet

http://hdl.handle.net/10174/16884

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