2 Petrotectonic Processes in Convergent Margins: Insights from Laurentia and Beyond
Friday, 28 March 2025
8:00 AM - 12:00 PM
120
QUANTIFYING RADIATION DAMAGE IN LOW ALPHA DOSE ZIRCON
Paper number: 2-6
Program: Theme Sessions
Time: 9:40 AM – 10:00 AM
Authors
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Aaron JubbU.S. Geological Survey, Reston, VA
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Heather LowersGeology, Geophysics, and Geochemistry Science Center, Denver, CO
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Paul HackleyGeology, Energy & Minerals Science Center, Reston, VA
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William OdomU.S. Geological Survey, Reston, VA
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Jay ThompsonGeology, Geophysics, and Geochemistry Science Center, Denver, CO
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A. Kate SoudersGeology, Geophysics, and Geochemistry Science Center, Denver, CO
Abstract
Natural zircon, heat-treated natural zircon, and synthetic zircon were examined. Zircon compositions were determined by both LA-ICP-MS and by EPMA. LA-ICP-MS has the advantage of lower detection limits for the parent elements (U and Th), while EPMA provides a smaller spot size that more closely matches the spot size of spectroscopic analyses. The spectroscopic response of zircon was examined using both an XCLent hyperspectral cathodoluminescence (CL) detector that collected data simultaneously with the EPMA analyses and a Horiba XploraPlus that collected Raman and fluorescence data. Preliminary results show that for doses between ~1e13 to ~1e14 α/mg, Raman and Dy3+ FWHM values are invariant, as expected. In contrast, the hyperspectral CL data shows significant changes in the integrated intensity of the broadband yellow CL signal at the same dose. The signal initially increases, then falls before disappearing at ~1e14 α/mg. These preliminary findings show promise in using broadband yellow luminescence in zircon to quantify radiation damage at doses lower than resolvable via existing spectroscopic methods.
Geological Society of America Abstracts with Programs. Vol. 57, No. 3
doi: 10.1130/abs/2025NE-408606
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