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131
STAHL,W., WENDT,!': Fractionation of calcium isotopes in carbonate precipitation. Earth Planet. Sci. Letters 5, 184 (1968).
STANTON, R. L.: The application of sulphur isotope studies in ore genesis theory. A
suggested model. N.Z.J. Geol. Geophys. 3, 375-389 (1960).
STANTON,R. L., RAFfER, T. A.: The isotopic constitution of sulphur in some stratiform lead-zinc ores. Mineral. Deposita 1,16-29 (1966).
STEVENS, L. M., KROUT, L., WALLING, D., VENTERS, A., ENGELKEMEIER, A.,
Ross,L.E.: The isotopic composition of atmospheric carbon monoxide. Earth
Planet. Sci. Letters 16, 147~165 (1972).
SUZUOKI, T., EpSTEIN, S.: Hydrogen isotope fractionation factor (b's) between muscovite, biotite, hornblende and water (Abstr.). Eos (Trans. Am. Geophys.
Union) 51, 451 (1970).
TAKEMATSU,N., MATSUO,S., SATO,S.: Isotopic composition of magnesium in upper
mantle material and a meteorite. Geochemical J. 1, 51 (1967).
TAN, F. c., HUDSON,J. D.: Carbon and oxygen isotopic relationships of dolomites
and coexisting calcites, Great Estuarine Series (Jurassic), Scotland. Geochim.
Cosmochim. Acta 35,755 (1971).
TARUTANI,T., CLAYTON,R.N., MAYEDA,T.K.: The effect of polymorphism and
magnesium substitution on oxygen isotope fractionation between calcium carbonate and water. Geochim. Cosmochim. Acta 33, 987 (1969).
TATSUMI, T.: Sulfur isotopic fractionation between coexisting sulfide minerals from
some Japanese ore deposits. Econ. Geol. 60, 1645~1659 (1965).
TAYLOR, H. P.: Isotopic evidence for large-scale oxygen exchange during metamorphism of Adirondack igneous rocks (abstract). Geol. Soc. Am. Spec. Paper
76, 163 (1964).
TAYLOR,H.P.: Oxygen isotope studies of hydrothermal mineral deposits. In:
BARNES,H.L.(Ed.): Geochemistry of hydrothermal ore deposits. New YorkLondon: Holt, Rinehart and Winston Inc. 1967.
TAYLOR, H. P.: The oxygen isotope geochemistry of igneous rocks. Contr. Mineral.
Petrol. 19, 1~71 (1968a).
TAYLOR, H. P.: Oxygen isotope studies of anorthosites with special reference to the
origin of bodies in the Adirondack Mountains, New York. In: Origin of anorthosites, N.Y. State Museum Spec. Publ. 1968b.
TAYLOR, H. P.: Oxygen isotope evidence for large-scale interaction between meteoric ground waters and Tertiary granodiorite intrusions, Western Cascade
Range, Oregon. J. Geophys. Res. 76, 7855 (1971).
TAYLOR, H. P., EpSTEIN, S.: 18 0/ 16 0 ratios of feldspars and quartz in zoned granitic
pegmatites. Geol. Soc. Am. Spec. Paper 68, 283 (1961).
TAYLOR,H.P., EpSTEIN,S.: Relation between 0 18 /0 16 ratios in coexisting minerals
of igneous and metamorphic rocks. !. Principles and experimental results. Bull.
Geol. Soc. Am. 73,461 (1962a).
TAYLOR,H.P., EpSTEIN,S.: Relation between 0 18 /0 16 ratios in coexisting minerals
of igneous and metamorphic rocks. II. Application to petrologic problems. Bull.
Geol. Soc. Am. 73, 675 (1962b).
TAYLOR,H.P., EpSTEIN,S.: 0 18 /0 16 ratios in rocks and coexisting minerals of the
Skaergaard intrusion. J. Petrol. 4, 51 (1963).
TAYLOR, H. P., EpSTEIN, S.: Comparison of oxygen isotope analyses of tektites, soils
and impactite glasses. In: Cosmic and Isotopic Chemistry. Amsterdam: North
Holland Pull. Co. 1964.
TAYLOR,H.P., EpSTEIN,S.: Oxygen isotope studies of Ivory Coast tektites and impactite glass from the Bosumtwi crater, Ghana. Science 153, 173 (1966a).
