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The 87Sr/86Sr and 143Nd/144Nd values, which show variations by the radioactive decay of long half-life isotopes of 87Rb and 147Sm, respectively, are routinely used for geochemical tracing and petrogenesis research. Thermal ionization mass spectrometry (TIMS), with its excellent accuracy, high sensitivity, and low memory, has been widely used to determine Sr and Nd isotopic ratios.
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