Abstract
The relationship between deu· terium and oxygen-18 concentrations in natural meteoric waters from many parts of the world has been determined with a mass spectrometer. The isotopic enrich- ments, relative to ocean water, display a linear correlation over the entire range for waters which have not undergone ex- cessive evaporation.
Cite
CITATION STYLE
APA
Heller, P. L., & Frost, C. D. (1988). Isotopic Provenance of Clastic Deposits: Application of Geochemistry to Sedimentary Provenance Studies (pp. 27–42). https://doi.org/10.1007/978-1-4612-3788-4_2
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