Radiogenic isotopes provide powerful tracers for studying the ages and origins of Earth systems.
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Stable isotope tracers involve only non-radiogenic isotopes and usually are mass-dependent.
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Isotopic tracers are usually subdivided into two categories : stable isotope tracers and radiogenic isotope tracers.
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It also suggests that this temperature means that the concentration of radiogenic isotopes is greater than within the earth.
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Radiogenic isotope tracers are most powerful when used together with other tracers : The more tracers used, the more control on mixing processes.
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Many radiogenic isotope measurements are made by ionization of a solid source, whereas stable isotope measurements of light elements ( e . g.
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Because their abundances are normally quoted as activity ratios rather than atomic ratios, they are best considered separately from the other radiogenic isotope systems.
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These decay-products are termed radiogenic isotopes, in order to distinguish them from the much larger group of'non-radiogenic'isotopes.
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They are particularly useful to understand mixing processes between different components, because ( heavy ) radiogenic isotope ratios are not usually fractionated by chemical processes.
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U-series isotopes are unique amongst radiogenic isotopes because, being in the U-series decay chains, they are both radiogenic and radioactive.
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