4.4 Article

A New Appraisal of Sri Lankan BB Zircon as a Reference Materialfor LA-ICP-MS U-Pb Geochronology and Lu-Hf IsotopeTracing

Journal

GEOSTANDARDS AND GEOANALYTICAL RESEARCH
Volume 41, Issue 3, Pages 335-358

Publisher

WILEY
DOI: 10.1111/ggr.12167

Keywords

BB zircon; Sri Lankan reference material; U-Pb geochronology; Hf isotope system; rare earth elements; LA-ICP-MS

Funding

  1. CNPq [402852/2012-5, 401334/2012-0, 302633/2011-1, 305284/2015-0]
  2. FAPEMIG [CRA RDP00067-10, APQ03943, APQ-01448-15]
  3. FINEP (CT-INFRA)
  4. PROPP/UFOP [03/2014, 02/2015]
  5. CAPES
  6. National Research Foundation (South Africa)
  7. CNPq (Science without Borders Program, Brazil)
  8. Natural Environment Research Council [nigl010001] Funding Source: researchfish
  9. NERC [nigl010001] Funding Source: UKRI

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A potential zircon reference material (BB zircon) for laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) U-Pb geochronology and Hf isotope geochemistry is described. A batch of twenty zircon megacrysts (0.5-1.5cm(3)) from Sri Lanka was studied. Within-grain rare earth element (REE) compositions are largely homogeneous, albeit with some variation seen between fractured and homogeneous domains. Excluding fractured cathodoluminescence bright domains, the variation in U content for all analysed crystals ranged from 227 to 368 mu g g(-1) and the average Th/U ratios were between 0.20 and 0.47. The Hf isotope composition (0.56-0.84 g/100 g Hf) is homogeneous within and between the grains - mean Hf-176/Hf-177 of 0.281674 +/- 0.000018 (2s). The calculated alpha dose of 0.59 x 10(18) g(-1) for a number of BB grains falls within the trend of previously studied, untreated zircon samples from Sri Lanka. Aliquots of the same crystal (analysed by ID-TIMS in four different laboratories) gave consistent U-Pb ages with excellent measurement reproducibility (0.1-0.4% RSD). Interlaboratory assessment (by LA-ICP-MS) from individual crystals returned results that are within uncertainty equivalent to the TIMS ages. Finally, we report on within- and between-grain homogeneity of the oxygen isotope systematic of four BB crystals (13.16 parts per thousand VSMOW).

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