Geologists are always faced with many questions when studying natural sys-tems. Among them, some can be answered using clay minerals if one considers a particular aspect of their chemical composition: isotopes. The goal of this chapter is to give the basics of the stable and radioactive isotope chemistry through the description of some geological examples. This is simply an intro-duction to a broad field of investigation. More detailed presentations may be found in the suggested reading listed at the end of the chapter.
CITATION STYLE
Clays in Sedimentary Environments. (2005). In Clays (pp. 295–327). Springer-Verlag. https://doi.org/10.1007/3-540-27141-4_7
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