Carbon consists of two stable isotopes, carbon 12 and carbon 13, which differ by the mass of only one neutron in the nucleus. The ratio 13C/12C in organic and inorganic matter is approximately 0.01 and varies up to 10% in nature.
CITATION STYLE
Stahl, W. J. (1979). Carbon Isotopes in Petroleum Geochemistry. In Lectures in Isotope Geology (pp. 274–282). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-67161-6_23
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