δD vs δ 18 O values and d-excess vs δ 18 O values for natural water

δD vs. δ 18 O relationship at a height of 15 m for 2835 model

Divergence of stable isotopes in tap water across China

The δD vs. δ 18 O plot of natural groundwater, lake water and

Using Stable Isotopes (δ18O and δD) to Study the Dynamics of Upwelling and Other Oceanic Processes in Northwestern South China Sea - Zhou - 2022 - Journal of Geophysical Research: Oceans - Wiley Online Library

Global meteoric water line - Wikipedia

δD vs δ 18 O values and d-excess vs δ 18 O values for natural water

Table 1 from Measurement of δ18O, δ17O, and 17O-excess in water by off-axis integrated cavity output spectroscopy and isotope ratio mass spectrometry.

Frontiers Using dual water isotopes to quantify the mixing of water masses in the Pearl River Estuary and the adjacent northern South China Sea

Frontiers Spatiotemporal Variation of Hydrogen and Oxygen Stable Isotopes in the Yarlung Tsangpo River Basin, Southern Tibetan Plateau

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

ESSD - The CISE-LOCEAN seawater isotopic database (1998–2021)

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

CP - Improving temperature reconstructions from ice-core water-isotope records