DEVELOPMENT OF A U-TH-PB MONAZITE DATING PROCEDURE USING EPMA AT VIRGINIA TECH
Because EPMA is a spectroscopic method that performs elemental quantification using characteristic X-rays, treatment of elemental interferences (e.g. Y Lγ vs Pb Mβ) and background fitting (e.g. curved vs linear background models) are fundamental considerations affecting our results. Wavelength scans were conducted around the peak and background collection points for Th, U, and Pb for each standard to check for possible interferences from higher-order X-ray lines. Background correction was done through linear interpolation on each point measured. This final procedure yields results that are generally accurate to 10s of Ma, though the discrepancy is generally lower for some Phanerozoic and late Proterozoic samples. We found limited improvement to the accuracy of the method from using longer analysis times at higher beam power, which suggests that methodological uncertainty provides a first order limitation on the accuracy of monazite ages obtained using EPMA, and errors introduced by X-ray counting statistics are less significant. Ongoing work aims to optimize sample throughput and minimize analytical error to provide the SE US petrologic community with another resource for the rapid and cost-effective dating of monazite at sufficient accuracy and precision to resolve major trends.