Apatite Reference Materials for SIMS Microanalysis of Isotopes and Trace Elements

Allen K. Kennedy, Jörn Frederik Wotzlaw, James L. Crowley, Mark Schmitz, Urs Schaltegger, Benjamin Wade, Laure Martin, Cristina Talavera, Bryant Ware, Thi Hao Bui

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Abstract

Twelve apatite samples have been tested as secondary ion mass spectrometry (SIMS) reference materials. Laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) analysis shows that the SLAP, NUAN and GR40 apatite gems are internally homogeneous, with most trace element mass fractions having 2 standard deviations (2s) ≤ 2.0%. BR2, BR5, OL2, AFG2 and AFB1, which have U > 63 μg g-1, 206Pb/204Pb > 283, and homogeneous SIMS U-Pb data, have respective isotope dilution thermal ionisation mass spectrometry (ID-TIMS) ages of 2053.83 ± 0.21 Ma, 2040.34 ± 0.09 Ma, 868.87 ± 0.25 Ma, 478.71 ± 0.22 Ma and 473.25 ± 0.09 Ma. Minor U-Pb heterogeneity exists and accurate SIMS results require correction with the 3D Concordia-constrained common Pb composition. Among the studied samples, AFG2 and BR5 are the most homogeneous U-Pb reference materials. The SIMS sulfur isotopic compositions of eight of the apatites shows they are homogeneous, with 2s for both 103δ34S and 103δ33S < 0.55‰. One apatite, BR96, has Δ33S = -0.36 ± 0.2‰. The apatite samples have ID-TIMS 87Sr/86Sr between 0.704214 ± 0.000030 and 0.723134 ± 0.000035.

Original languageAmerican English
Pages (from-to)373-402
Number of pages30
JournalGeostandards and Geoanalytical Research
Volume47
Issue number2
DOIs
StatePublished - Jun 2023

Keywords

  • O
  • S
  • SIMS
  • Sr
  • U-Pb
  • apatite
  • isotopes
  • reference material

EGS Disciplines

  • Earth Sciences
  • Geophysics and Seismology

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