Thermal ionization mass spectrometry
Thermal ionization mass spectrometry is a technique which has been chiefly developed for the analysis of geological samples. The technique is used extensively for the isotope ratio measurements required for Rb—Sr, Nd—Sm and Pb—Th—U geochronology studies as well as the determination of rare-earth elements, and, less frequently, other selected elements by isotope dilution analysis.
KeywordsIsotope Dilution Mass Peak Thermal Ionization Mass Spectrometry Isotope Dilution Mass Spectrometry Isotope Ratio Measurement
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- Catanzaro, E.J., T.J. Murphy, W.R. Shields and E.L. Garner (1968) Absolute isotopic abundance ratios of common, equal-atom and radiogenic lead standards. J. Res. Natl. Bur. Stand A72 261–267.Google Scholar
- Faure, G. (1977) Principles of Isotope Geology John Wiley and Sons, New York.Google Scholar
- Hawkesworth, C.J. and P.W.C. van Calsteren (1983). Radiogenic isotopes—some geological applications. In: P. Henderson (ed.), Rare Earth Element Geochemistry (Developments in Geochemistry, 2). Elsevier, Amsterdam, 375–421.Google Scholar
- Heumann, K.G. (1982) Isotopic analysis of inorganic and organic substances by mass spectrometry. Int. J. Mass Spectrom. Ion Phys 45 87–110.Google Scholar
- Krogh, T.E. and G.L. Davis (1975) The production and preparation of 205Pb for use as a tracer for isotope dilution analysis. Carnegie Institute Yearbook 74 416–417.Google Scholar
- Schuhmann, S. and J.A. Philpotts (1979) Mass spectrometric stable isotope dilution analyses for lanthanides in geochemical materials. In: K.A. Gschneider and L. Eyring (eds.), Handbook on the Physical Chemistry of Rare Earths Elsevier/North Holland Publishing, Amsterdam, 4 471–481.Google Scholar