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129
SAVIN,S.M., EpSTEIN,S.: The oxygen and hydrogen isotope geochemistry of clay
minerals. Geochim. Cosmochim. Acta 34,25--42 (1970a).
SAVIN,S.M., EpSTEIN,S.: The oxygen and hydrogen isotope geochemistry of ocean
sediments and shales. Geochim. Cosmochim. Acta 34, 43--64 (1970b).
SAVIN, S. M., EpSTEIN, S.: The oxygen isotopic compositions of coarse grained sedimentary rocks and minerals. Geochim. Cosmochim. Acta 34, 323-329 (1970c).
SCALAN,R. c.: Ph. D. Thesis, University of Arkansas 1957.
SCHIEGL, W. E., VOGEL,J. c.: Deuterium content of organic matter. Earth Planet.
Sci. Letters 7,307-313 (1970).
SCHILLER, W. R., GEHLEN, K. VON, NIELSEN, H.: Hydrothermal exchange and fractionation of sulfur isotopes in synthesized ZnS and PbS. Econ. Geol. 65, 350
(1970).
SCHOEN,R., RYE,R.O.: Sulfur isotope distribution in solfataras, Yellowstone National Park. Science 170, 1002 (1970).
SCHNEIDER,A.: The sulfur isotope composition of basaltic rocks. Contr. Mineral.
Petrol. 24,95 (1970).
SCHNEIDER,A., NIELSEN,H.: Zur Genese des elementaren Schwefels im Gips von
Weenzen. Contr. Mineral. Petrol. 11,705 (1965).
SCHREINER,G.D.L., VERBEEK,A.A.: Variations in 39K/41K ratio and movement of
potassium in granite-shale contact region. Proc. Roy. Soc. London A285, 423
(1965).
SCHREINER,G.D.L., WELKE,H.J.: Variations in 39K/41K ratio and movement of
potassium in heated and stressed xenoliths. Geochim. Cosmochim. Acta 35, 719
(1971).
SCHWARCZ, H. P.: Oxygen and carbon isotopic fractionation between coexisting
calcite and dolomite. J. Geol. 74, 38--48 (1966).
SCHWARCZ,H.P.: The stable isotopes of carbon. In: WEDEPOHL,K.H. (Ed.): Handbook of Geochemistry, 6-B-1. Berlin-Heidelberg-New York: Springer 1969.
SCHWARCZ,H.P., CLAYTON,R.N.: Oxygen isotope studies ofamphibolites. Can. J.
Earth Sci. 2, 72-84 (1965).
SCHWARCZ,H.P., AGYEI,E.K., McMuLLEN, C. c.: Boron isotopic fractionation
during clay adsorption from sea-water. Earth Planet. Sci. Letters 6, 1-5 (1969).
SCHWARCZ, H. P., CLAYTON, R. N., MAYEDA, T.: Oxygen isotopic studies of calcareous and pelitic metamorphic rocks, New England. Bull. Geol. Soc. Am. 81,
2299 (1970).
SENFTLE, F. E., BRACKEN,J. T.: Theoretical effect of diffusion on isotopic abundance
ratios in rocks and associated fluids. Geochim. Cosmochim. Acta 7, 61 (1955).
SHACKLETON, N.: Oxygen isotope analyses and Pleistocene temperatures re-assessed. Nature 215,15 (1967).
SHACKLETON, N.: Depth of pelagic foraminifera and isotopic changes in Pleistocene
Oceans. Nature 218,79 (1968).
SHACKLETON, N.: The last interglacial in marine and terrestrial records. Proc. Roy.
Soc. London B 174,135 (1969).
SHARMA,T., CLAYTON,R.N.: Measurement of 0 18 /0 16 ratios of total oxygen of
carbonates. Geochim. Cosmochim. Acta 29,1347-1354 (1965).
SHEPPARD,S.M.F., EpSTEIN,S.: D/H and 0 18 /0 16 ratios of minerals of possible
mantle or lower crustal origin. Earth Planet. Sci. Letters 9, 232 (1970).
SHEPPARD, S. M. F., NIELSEN, R. L., TAYLOR, H. P.: Oxygen and hydrogen isotope
ratios of clay minerals from Porphyry Copper deposits. Econ. Geol. 64, 755777 (1969).