摘要

Thermal ionization mass spectrometry (TIMS) is considered the most accurate technique for determining Sr-Nd-Pb isotopic ratios in geological samples. However, time-consuming and complex sample separation procedures greatly hinder the instrumental measurement efficiency. In this study, a single-column separation chemistry procedure for Sr-Nd-Pb from single rock dissolution was developed. The chemistry procedure was designed to minimize the number of evaporation steps and considerably shorten the separation time, enabling high throughput for TIMS. In contrast to conventional three-column separation procedures (similar to 3 days), this technique was characterized by high efficiency superiority in terms of separation time (similar to 8 hours), a 3-fold enhancement in the separation efficiency. The stability of our procedure was demonstrated by replicated TIMS measurements of Sr-87/Sr-86, Nd-143/Nd-144, Pb-206/Pb-204, Pb-207/Pb-204 and Pb-208/Pb-204 ratios for six international silicate rock reference materials, spanning a wide range of bulk compositions. The analytical results obtained for these standards agreed well with published data. The external reproducibility (2 RSD, n = 10) of a BCR-2 standard sample was +/- 0.0020% for Sr-87/Sr-86, +/- 0.0023% for Nd-143/Nd-144, and +/- 0.021-0.033% for Pb-206/Pb-204, Pb-207/Pb-204 and Pb-208/Pb-204 ratios.