Isotopic Variations in Meteoric Waters
Harmon CraigDepartment of Earth Sciences, University of California, La Jolla
1961en
ABI
Abstract
The relationship between deuterium and oxygen-18 concentrations in natural meteoric waters from many parts of the world has been determined with a mass spectrometer. The isotopic enrichments, relative to ocean water, display a linear correlation over the entire range for waters which have not undergone excessive evaporation.
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Cited by 40 references