4.7 Article

Assessment of elemental fractionation and matrix effects during in situ Rb-Sr dating of phlogopite by LA-ICP-MS/MS: implications for the accuracy and precision of mineral ages

Journal

JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY
Volume 36, Issue 2, Pages 322-344

Publisher

ROYAL SOC CHEMISTRY
DOI: 10.1039/d0ja00299b

Keywords

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Funding

  1. Australian Research Council ARC Linkage grant [LP160101353]
  2. Mineral Exploration Cooperative Research Centre (MinEx CRC Project) [8]
  3. Agilent Technologies

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The study found that the accuracy of in situ Rb-Sr dating of igneous phlogopite mineral using LA-ICP-MS/MS technology is typically within about 3%, with occasional higher errors ranging between 4% to 8%. The bias and uncertainty in the Rb-Sr ages may be related to matrix effects between Mica-Mg and MDC, as well as different physical properties. Developing improved nano-powder reference materials with better matrix matching is crucial for enhancing the accuracy of in situ Rb-Sr dating.
Laser-ablation inductively-coupled plasma tandem mass-spectrometry (LA-ICP-MS/MS) allows for rapid and interference free analyses of Rb and Sr isotopes, permitting in situ Rb-Sr dating of minerals. However, the general lack of matrix matched reference materials remains one of its main obstacles, affecting both precision and accuracy. This study systematically investigates the impact of matrix effects and down-hole fractionation (DHF) on the in situ Rb-Sr ages of an igneous phlogopite mineral (MDC) analysed by an ICP-MS/MS using two different LA systems: (i) a RESOlution ArF (193 nm) excimer and (ii) a NWR (213 nm) Nd-YAG laser system. A phlogopite reference material (Mica-Mg), originating from the same location as the MDC, was prepared as a pressed nano-powder pellet (NP) and used in this study as a primary reference material. The results revealed that the accuracy of the Rb-Sr ages is typically within about 3% (for 70% of analysed samples), but occasionally higher ranging between 4 to 8% (ca. 30% of cases). We hypothesize that the above bias and uncertainty in the Rb-Sr ages are related to matrix effects between Mica-Mg-NP and MDC, due to their specific ablation characteristics and different physical properties. In addition, the elemental fractionation effects observed in this study for Rb-87/Sr-86 are also dependent on laser wavelength (i.e., 193 nm vs. 213 nm). Hence, developing an improved nano-powder reference material, or a mineral or glass with better matrix matching to natural phlogopite minerals would be desirable to further improve the accuracy of in situ Rb-Sr dating. Currently, regular monitoring of secondary and matrix-matched reference minerals such as the MDC phlogopite can be used to assess and evaluate the accuracy of in situ Rb-Sr dating of phlogopite, yielding ages within accuracy of ca. 3% or better.

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