Geochemical evolution of geothermal fluids around the western Red Sea and East African Rift geothermal provinces

Article

Chandrasekharam, D., Lashin, A., Al Arifi, N., Al-Bassam, A. M. and Chandrasekhar, V.. 2018. "Geochemical evolution of geothermal fluids around the western Red Sea and East African Rift geothermal provinces." Journal of Asian Earth Sciences. 164, pp. 292-306. https://doi.org/10.1016/j.jseaes.2018.06.013
Article Title

Geochemical evolution of geothermal fluids around the western Red Sea and East African Rift geothermal provinces

ERA Journal ID1740
Article CategoryArticle
AuthorsChandrasekharam, D. (Author), Lashin, A. (Author), Al Arifi, N. (Author), Al-Bassam, A. M. (Author) and Chandrasekhar, V. (Author)
Journal TitleJournal of Asian Earth Sciences
Journal Citation164, pp. 292-306
Number of Pages15
Year2018
Place of PublicationUnited Kingdom
ISSN1367-9120
1878-5786
Digital Object Identifier (DOI)https://doi.org/10.1016/j.jseaes.2018.06.013
Web Address (URL)https://www.sciencedirect.com/science/article/pii/S1367912018302359?via%3Dihub
Abstract

The geothermal provinces of the western Red Sea coast and East African countries have evolved synchronous with the evolution of the landmasses around the Red Sea. The Red Sea opening was initiated subsequent to the opening of the Aden Gulf that was triggered by the Afar plume. During the Late Oligocene, the Red Sea rift started extending from south towards north culminating into a failed arm near the Suez Gulf. The geothermal systems evolved due to shallow mantle below the Danakil depression and circulating seawater. Besides the volcanic flows, the regional sedimentary aquifers like the Wajid Sandstone and Amron limestone, that occur in Ethiopia, Egypt, Eritrea and Djibouti, that were deposited prior to the younger tectonic events that started at 31 Ma are the main geothermal reservoirs in these countries. In contrast, rain surface and evaporated lake water are the main sources for the Kenyan geothermal systems. Although these geothermal fluids show variation in their chemical components due to different recharging sources, all the geothermal systems are of high temperature, capable of generating electricity. © 2018 Elsevier Ltd

KeywordsAfar; ANS; Danakil; geothermal; Red Sea rift; Sub-Saharan; electricity generation; geochemistry; geothermal energy; geothermal system; high temperature; East African Rift; Gulf of Suez; Indian Ocean; Red Sea
ANZSRC Field of Research 2020370799. Hydrology not elsewhere classified
410406. Natural resource management
401102. Environmentally sustainable engineering
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Byline AffiliationsIndian Institute of Technology, India
King Saud University, Saudi Arabia
GeoSyndicate Power, India
Institution of OriginUniversity of Southern Queensland
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