Introduction and Definitions
Zinc is comprised of five natural stable isotopes, 64Zn(48.6%), 66Zn (27.9%), 67Zn (4.1%), 68Zn (18.8%), and 70Zn (0.6%). Due to its relatively high first ionization potential (9.4 eV), the measurement of Zn isotope ratios is very difficult by thermal ionization mass spectrometry (TIMS). This explains the very limited Zn isotope data produced before the advent of multi-collection inductively coupled plasma mass spectrometry (MC-ICP-MS). Since the first commercialized MC-ICP-MS in the late 1990s and the first high precision Zn isotope ratio measurements (Maréchal et al. 1999), more than 1000 papers have been published (source ISI Web of Science) on various geochemistry topics associated with Zn isotopes (e.g., oceanography, cosmochemistry, environmental sciences, medical sciences). Generally, the isotopic data are acquired by MC-ICP-MS by either standard bracketing (e.g., Maréchal et al. 1999; Weiss et al. 2005; Viers et al. 2007; Balistrieri et al. 2008)...
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Moynier, F. (2018). Zinc Isotopes. In: White, W.M. (eds) Encyclopedia of Geochemistry. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-39312-4_215
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