INCREASED ACCURACY AND PRECISION IN DETRITAL ZIRCON GEOCHRONOLOGY USING CA-LA-ICPMS
To ensure that CA does not systematically bias U-Pb dates, we treated and analyzed a suite of 13 zircon reference materials and compared these data to untreated aliquots of the same materials. The dates of both the CA and non-CA reference materials are undistinguishable within 0.1-4.5% from the reference ages, indicating no negative effects from CA on LA-ICPMS analyses. Additionally, a Precambrian igneous sample that has substantial radiation damage was analyzed to assess the effects of CA on grains with significant Pb-loss. CA-LA-ICPMS results from this sample show increased concordance relative to non-CA data.
Finally, to explore how CA affects DZ age populations, we analyzed two detrital samples. One sample is Mesozoic in age and contains both Phanerozoic (100-300 Ma) and Precambrian (1000-1200 Ma) populations, whereas the second sample is Proterozoic and contains populations between 2000-3500 Ma. Chemical abrasion changed the number and distribution of peak age populations in both samples when compared to non-CA age spectra. In particular, the Phanerozoic age peaks narrowed, which we attribute to a reduction in analyses affected by Pb-loss. We propose that the increased accuracy of individual CA-LA-ICPMS U-Pb zircon dates can increase resolution of DZ age populations in samples where Phanerozoic peaks are tightly spaced in time.