Lithium Potential in Saudi Arabia – An Initial Assessment

Abstract Lithium (Li) is a key element in the global energy transition, playing a vital role in low-carbon energy storage systems, particularly in batteries for electric vehicles (EVs). This study provides the first comprehensive geological assessment of lithium potential in Saudi Arabia by examining the natural occurrence of lithium in igneous and sedimentary rocks and the processes that lead to its enrichment in subsurface brines. The results suggest that the west coast rift basins and the Arabian Shield hold significant potential, while the eastern sedimentary basin appears to be less favorable. Lithium naturally occurs in felsic igneous rocks, especially in their glass and micaceous components, and in sedimentary rocks derived from them, such as micaceous sandstones. Enrichment of lithium in pore waters may result from two primary mechanisms: (1) Water–rock interaction at elevated temperatures (>120°C), which leaches lithium from host minerals into formation fluids; and (2) Evaporative concentration of seawater, where lithium remains in the residual brine during progressive evaporite precipitation. The felsic igneous rocks of the Arabian Shield and syn-rift sedimentary formations along the Saudi west coast show strong potential as lithium sources. In addition, evaporative processes in the region that lead to the precipitation of thick salt deposits further contribute to lithium enrichment in subsurface brines. Although current data is limited, the study identifies the west coast rift basins as the most promising areas for lithium-rich deep brines suitable for Direct Lithium Extraction (DLE). Lithium originates from the leaching of shield sediments in the deep rift basins and from leftover brines associated with the km-thick Miocene evaporates deposited in the Red Sea rift. In contrast, the Eastern Arabian Basin shows limited potential for lithium-rich brines. Evaporites are limited to a thin gypsum layer in the Jurassic Hith and older (Precambrian) deeply buried Hormuz salts, while clastic material eroded from the shield is shallow and too proximal to the outcrops for significant contributions to basinal brines. This study provides the first comprehensive assessment of lithium potential in Saudi Arabia, offering valuable insights into sustainable resource development and future exploration opportunities in the Kingdom.

Authors

Institutions

Publication Details

Published
2025-09-16
DOI
https://doi.org/10.2118/227608-ms
Citations
1
Primary Topic
Chemical Synthesis and Characterization
Type
article
Field-Weighted Citation Impact
1.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Lithium Potential in Saudi Arabia – An Initial Assessment

Volker Vahrenkamp, Manuel Ortíz
1 citations
Chemical Synthesis and Characterization
1.00
article

Lithium Potential in Saudi Arabia – An Initial Assessment

Volker Vahrenkamp, Manuel Ortíz
article en
1 citations

Abstract

Abstract Lithium (Li) is a key element in the global energy transition, playing a vital role in low-carbon energy storage systems, particularly in batteries for electric vehicles (EVs). This study provides the first comprehensive geological assessment of lithium potential in Saudi Arabia by examining the natural occurrence of lithium in igneous and sedimentary rocks and the processes that lead to its enrichment in subsurface brines. The results suggest that the west coast rift basins and the Arabian Shield hold significant potential, while the eastern sedimentary basin appears to be less favorable. Lithium naturally occurs in felsic igneous rocks, especially in their glass and micaceous components, and in sedimentary rocks derived from them, such as micaceous sandstones. Enrichment of lithium in pore waters may result from two primary mechanisms: (1) Water–rock interaction at elevated temperatures (>120°C), which leaches lithium from host minerals into formation fluids; and (2) Evaporative concentration of seawater, where lithium remains in the residual brine during progressive evaporite precipitation. The felsic igneous rocks of the Arabian Shield and syn-rift sedimentary formations along the Saudi west coast show strong potential as lithium sources. In addition, evaporative processes in the region that lead to the precipitation of thick salt deposits further contribute to lithium enrichment in subsurface brines. Although current data is limited, the study identifies the west coast rift basins as the most promising areas for lithium-rich deep brines suitable for Direct Lithium Extraction (DLE). Lithium originates from the leaching of shield sediments in the deep rift basins and from leftover brines associated with the km-thick Miocene evaporates deposited in the Red Sea rift. In contrast, the Eastern Arabian Basin shows limited potential for lithium-rich brines. Evaporites are limited to a thin gypsum layer in the Jurassic Hith and older (Precambrian) deeply buried Hormuz salts, while clastic material eroded from the shield is shallow and too proximal to the outcrops for significant contributions to basinal brines. This study provides the first comprehensive assessment of lithium potential in Saudi Arabia, offering valuable insights into sustainable resource development and future exploration opportunities in the Kingdom.

King Abdullah University of Science and Technology (SA)
Openalex Percentile: Top 19%
Chemical Synthesis and Characterization
1.00
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.