Thermal ionization mass spectrometry
Thermal ionization mass spectrometry is a technique which has been chiefly developed for the analysis of geological samples. The technique is used extensively for the isotope ratio measurements required for Rb—Sr, Nd—Sm and Pb—Th—U geochronology studies as well as the determination of rare-earth elements, and, less frequently, other selected elements by isotope dilution analysis.
KeywordsSilicate Tungsten Radioactive Isotope Palladium Cerium
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