We show that portable X-ray fluorescence can be used to rapidly (ca. 90 s) estimate the rate of background radioactivity in sediment used to calculate burial ages in trapped charge dating studies. This procedure involves inputting a measurement of potassium concentration into a set of simple regression equations, defined by a large radionuclide dataset. Results show good agreement with high-precision methods. Our rapid method will help to quickly generate burial age estimates.

We developed a faster and simpler method to measure helium gas in targeted minerals within whole rocks to determine how long they have been exposed at Earth's surface. Instead of manually separating minerals, our method uses heat to release gas from the specific minerals of interest. This reduces time, cost, and physical effort, making it easier to collect large amounts of data when studying landscape change or when only small rock samples are available.

In this study, Optically Stimulated Luminescence (OSL), Electron Spin Resonance (ESR) and Laser Ablation-Induced Coupled Plasma-Mass Spectroscopy (La-ICPMS) trace element (TE) analyses shows that TE composition may influence OSL and ESR-Ti sensitivities in quartz, which vary with bedrock type. Pressure may take a part in OSL/ESR-Ti sensitivities variability while ESR-Al intensities could be linked to initial fluid composition and crystallization conditions

To improve U-Th zircon dating, we optimized a U-Th-Pb double-dating strategy for young zircon (150–300 ka). We found that the overall U-Th age spectrum is consistent whether assuming a constant melt composition or constant U/Th fractionation between zircon and melt, but testing the representability of the measured glass with the youngest isochron intercept proved essential. A Bayesian model with a uniform prior distribution gave the most accurate estimates of eruption timing for U-Th datasets.