Abstract
Extraterrestrial materials consist of samples from the moon, Mars, Vesta and a variety of smaller bodies such as asteroids and comets. These planetary samples have been used to deduce the evolution of our solar system. A major difference between extraterrestrial and terrestrial materials is the existence of primordial isotopic heterogeneities in the early solar system. These heterogeneities are not observed on Earth, because they have become obliterated during high-temperature processes over geologic time. Nevertheless, isotopes have been used as a genetic link between meteorites and the Earth (i.e. Clayton in Treatise on geochemistry, Elsevier, Amsterdam, 2004).
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Hoefs, J. (2021). Variations of Stable Isotope Ratios in Nature. In: Stable Isotope Geochemistry. Springer Textbooks in Earth Sciences, Geography and Environment. Springer, Cham. https://doi.org/10.1007/978-3-030-77692-3_3
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