Ratio of channel to inter-channel deposits: The ratio of channel to inter-channel deposits within the Pleistocene and Holocene alluvium also changes across the IGB aquifer from proximal to distal areas, and is highly significant to the proportion of higher permeability sand deposits, to lower permeability silts and muds, which comprise the aquifer in different regions, and the anisotropy of the alluvial aquifer system.
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Hydrogeological typologies of the Indo-Gangetic basin alluvial aquifer, South Asia.
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