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Data · dataset · 2024

Lead isotope data for metal artefacts, marls and shales

Listed in Teesside University Research Data Repository

Lead isotope compositions for metal samples 1 to 30 and 32 (31 was excluded) and samples 33–36 (marls, shales) were submitted as small chips.

Description

The samples were analysed by multicollector-inductively coupled plasma mass spectrometry (MC-ICP-MS) at the University of Melbourne, Australia. Samples (1–241 mg) were weighed into Savillex PFA beakers and reacted with 7M HNO3 (2 mL, 120°C, 15 h).

Cu-rich samples formed blue solutions with minor residue while marl/ shale samples produced abundant residue. After drying, the samples were re-dissolved in 0.6M HBr, followed by Pb extraction on small (15 × 0.4 mm) beds of AG1-X8 (100–200 mesh) anion resin, using the HBr-HCl technique. Pb isotope ratios were measured on a Nu Plasma MC-ICP-MS with sample introduction via a low-uptake PFA nebuliser and Aridus desolvator.

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Data were collected using total Pb signal of 10–12 V, and instrumental mass bias was corrected using thallium doping (Woodhead, 2002). The thallium doping technique is expected to yield iPb/204Pb results with an external precision of 0.04%–0.08% (2std dev). This is confirmed by the results for the SRM 981 Pb standard, analysed as unknowns in the same sessions.

Seven analyses of Pb extracted from the BCR-2 reference basalt show greater variability, but the average agrees with the GeoREMpreferred composition (georem.mpch-mainz.gwdg.de) and is consistent with the long-term laboratory average and with TIMS reference data.

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Inferred from text
Isotope geochemistry 77% · Mass spectrometry 75%
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