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Sambhar Lake in the Thar desert of India behaves as a terminal lake in which inflow is balanced by evaporation. At present the source of the water to the lake is mainly through atmospheric precipitation and through surface runoff via two major seasonal streams (Roopangarh and Mendha). The meteoric contribution of water in the lake during the recharge period is suggested by the oxygen isotope...
This study used lead and sulfur isotope tracers to determine the nature and geometry of MVT-related brine flow in the Silurian paleoaquifer of the central Appalachians. Although the stratigraphy and lithology of this sedimentary package is similar to that of the important Lower Cambrian MVT-hosting paleoaquifer of the southern Appalachians, it lacks important mineralization. Lead isotope compositions...
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