Articles | Volume 1, issue 1
https://doi.org/10.5194/gchron-1-85-2019
https://doi.org/10.5194/gchron-1-85-2019
Research article
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11 Dec 2019
Research article | Highlight paper |  | 11 Dec 2019

Stepwise chemical abrasion–isotope dilution–thermal ionization mass spectrometry with trace element analysis of microfractured Hadean zircon

C. Brenhin Keller, Patrick Boehnke, Blair Schoene, and T. Mark Harrison

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Cited articles

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Barboni, M., Boehnke, P., Keller, C. B., Kohl, I. E., Schoene, B., Young, E. D., and McKeegan, K. D.: Early formation of the Moon 4.51 billion years ago, Sci. Adv., 3, e1602365, https://doi.org/10.1126/sciadv.1602365, 2017. a
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Bell, E. A., Harrison, T. M., Kohl, I. E., and Young, E. D.: Eoarchean crustal evolution of the Jack Hills zircon source and loss of Hadean crust, Geochim. Cosmochim. Acta, 146, 27–42, 2014. a
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Short summary
The oldest known minerals on Earth are Hadean (> 4.0 Ga) zircons from the Jack Hills, Australia. We present the first application to such Hadean zircons of stepwise chemical abrasion–isotope dilution–thermal ionization mass spectrometry with trace element analysis (stepwise CA-ID-TIMS-TEA). We examine the evolution in the U–Pb age and trace element chemistry of zircon domains accessed by successive chemical abrasion steps in the context of the geologic history of the Jack Hills zircons.