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Inter-basin groundwater flow pathways and hydrogeochemical evolution regulated by deep fault systems
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DOI：10.1016/j.apgeochem.2026.106971.png)
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Abstract
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• Deep fault systems control inter-basin groundwater flow (IGF) on the Tibetan Plateau. • Hydrogeochemical evidence identifies IGF from Nam Co Lake to adjacent basins. • IGF migrates southward along shallow, middle, and deep fault-controlled pathways. • Carbonate and silicate dissolution regulate IGF evolution at different depths. • IGF mixing ratios range 1-26.5%, contributing <6% to adjacent river runoff.
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