Characteristics of hydrogen and oxygen stable isotope ratios in precipitation collected in a snowfall region, Aomori Prefecture, Japan
Author:
Affiliation:
1. Institute for Environmental Sciences
2. Tohoku Nuclear Co. Ltd.
Publisher
Geochemical Society of Japan
Subject
Geochemistry and Petrology,Geophysics
Link
https://www.jstage.jst.go.jp/article/geochemj/48/1/48_2.0279/_pdf
Reference37 articles.
1. Aoki, M. (1992) Magmatic fluid discharged to the surface from the Osorezan geothermal system, northern Honshu, Japan. Rep. Geol. Surv. Jpn. 279, 16-21.
2. Araguas-Araguas, L., Froehilich, K. and Rozanski, K. (1998) Stable isotope composition of precipitation over southeast Asia. J. Geophys. Res. 103(D22), 28721-28742.
3. Coleman, M. L., Shepherd, T. J., Durham, J. J., Rouse, J. E. and Moore, G. R. (1982) Reduction of water with zinc for hydrogen isotope analysis. Anal. Chem. 54, 993-995.
4. Coplen, T. B. (1996) New guidelines for reporting stable hydrogen, carbon, and oxygen isotope-ratio data. Geochim. Cosmochim. Acta 60, 3359-3360.
5. Craig, H. (1961) Isotope variations in meteoric waters. Science 133, 1702-1703.
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