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Oxygen and hydrogen stable isotopes as recharge indicators, Central Nile Delta Quaternary aquifer, Egypt - ScienceDirect
PDF) Groundwater δ 18O and δD from central Indian Peninsula: influence of the Arabian Sea and the Bay of Bengal branches of the summer monsoon
Ice core basics
Isotopic variability in tropical cyclone precipitation is controlled by Rayleigh distillation and cloud microphysics
Total uncertainty of δD, δ 18 O, and d excess over the range of H 2 O v
Global meteoric water line - Wikipedia
Global meteoric water line - Wikipedia
Full article: Factors controlling stable isotope composition of precipitation in arid conditions: an observation network in the Tianshan Mountains, central Asia
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δ 2 H-δ 18 O (H2O) isotope values of some samples from the San
Isotopic compositions (δD, δ18O) and end-member mixing for the control interface in a complex tidal region - ScienceDirect
Relationship between δ 18 O and δ 2 H values and their frequency
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
The δD vs. δ 18 O plot of natural groundwater, lake water and
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