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Many laboratories have measured the abundances of naturally occurring actinide-series nuclides in volcanic rocks over the past three decades to constrain the time scales and extents of igneous processes. The number of practicing laboratories and the size and quality of the global volcanic rock data set has grown steadily during this time. Development and refinement of mass spectrometric (MS) analysis of minor U-series nuclides in igneous rocks has led to improved data quality.
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