Schriften
Degens, E. T.: Das O18/O16-Verhältnis im Urozean und der geochemische Stoffumsatz. N. Jb. Geol. Paläont, Mh. 1959, S. 180.
Degens, E. T., &Epstein, S.: The relationship between the 018/016 ratios in coexisting carbonates, Cherts and diatomite. Bull. Amer. Assoc. Petr. Geol., 1960.
Epstein, S.: The variations of the O18/O16 ratio in nature and some geological implications. Researches in Geochemistry, New York, John Wiley & Sons, Inc. 1959, S. 217.
Epstein, S., &Mayeda, T.: Variation of O18 content of waters from natural sources. Geochim. et Cosmochim. Acta,4, 1953, S. 213.
Sakai, H.: Fractionation of sulphur isotopes in nature. Geochim. et Cosmochim. Acta,12, 1957, S. 150.
Thode, H. G., Macnamara, J., &Fleming, W. H.: Sulphur isotope fractionation in nature and geological and biological time scales. Geochim. et Cosmochim. Acta, 3, 1953, S. 235.
Urey, H. C., Lowenstam, H. A., Epstein, S., &McKinney, C. R.: Measurement of paleotemperatures and temperatures of the Upper Cretaceous of England, Denmark and the southeastern United States. Bull. Geol. Soc. Amer.62, 1951, S. 399.
Vinogradov, A. P., Chupakhin, M. S., Grinenko, V. A., &Trofimov, A. V.: The isotopic composition of sulphur in connection with the growth of pyrites of sedimentary origin. Geokhimiya,1, 1956, S. 96.
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Degens, E.T. Stabile Isotope in Iihren Beziehungen zur Zeit. Geol Rundsch 49, 277–278 (1960). https://doi.org/10.1007/BF01802411
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DOI: https://doi.org/10.1007/BF01802411