GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania

Paper No. 263-7
Presentation Time: 3:35 PM

TANDEM LA-ICP-MS AND CA-ID-TIMS DETRITAL ZIRCON U-PB GEOCHRONOLOGY: ANALYSIS OF A GLOBAL DATASET


HOWARD, Benjamin, Department of Geosciences, University of Arkansas, 340 N. Campus Drive, 216 Gearhart Hall, Fayetteville, AR 72701, SHARMAN, Glenn R., Department of Geosciences, University of Arkansas, Fayetteville, AR 72701, CROWLEY, James L., Department of Geosciences, Boise State University, Boise, ID 83725 and REAT WERSAN, Ellen, Chevron Technology Company, Houston, TX 77022

Zircon U-Pb geochronology is a commonly used dating technique with widespread application to many geologic systems. Laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) and chemical abrasion-isotope dilution-thermal ionization mass spectrometry (CA-ID-TIMS) are among the most used methods for acquiring U-Pb dates from zircon. Although CA-ID-TIMS provides higher analytical precision, dates acquired via LA-ICP-MS are less expensive and may be acquired in sufficient quantity (i.e., >300 analyses per sample) for provenance characterization and identification of rare age modes (e.g., young zircon of near depositional age). However, recent case studies have demonstrated a tendency for the youngest LA-ICP-MS U-Pb dates from zircon to skew younger than the corresponding CA-ID-TIMS date, possibly a consequence of undetected Pb-loss that is mitigated in CA-ID-TIMS via chemical abrasion.

We conducted a systematic characterization of the degree of agreement between dates acquired via LA-ICP-MS and CA-ID-TIMS from the same zircon crystals. Our dataset consists of 1528 date pairs analyzed from 16 laboratories and 48 published studies. The lithologic makeup is 49% igneous, 40% sedimentary, and 11% metamorphic zircon. Excluding outliers and considering only < 1 Ga grains, ~69% of LA-ICP-MS 206Pb/238U dates are younger than their CA-ID-TIMS dates, with a typical shift of ~2.0-2.5%. Conversely, the 207Pb/206Pb dates from grains >1 Ga show no significant shift. These results highlight the potential effects of variable degrees of cryptic Pb loss on non-chemically abraded LA-ICP-MS measurements, although other complexities (e.g., inheritance, matrix mismatch effects) may also play a role. Studies using grains that were chemically abraded before LA-ICP-MS should be able to discern whether Pb-loss is a major effect. Ultimately, this research highlights a need for further research into potential effects of Pb loss on non-chemically abraded LA-ICP-MS datasets.