Plot of dD vs. d 18 O values showing the meteoric water line

Applicability of d-excess and 17O-excess as groundwater tracers for determination of recharge area

dD vs. d 18 O of rain, fog, stream water and shallow groundwater in the

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Using 18O and D to Quantify Ground-Water/ Surface-Water Interactions in Karst Systems of Florida

dD vs. d 18 O plot showing isotopic compositions of kaolinite, 7 A ˚

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Tracing isotopic signatures (δD and δ18O) in precipitation and glacier melt over Chorabari Glacier–Hydroclimatic inferences for the Upper Ganga Basin (UGB), Garhwal Himalaya - ScienceDirect

HESS - Isotopic offsets between bulk plant water and its sources are larger in cool and wet environments