“…The recent development of laser ablation inductively coupled plasma‐mass spectrometry (LA‐ICP‐MS) calcite U–Pb dating provides unique advantages including in situ analyses of micron‐sized carbonate minerals and rapid data acquisition (Li, Parrish, Horstwood, & McArthur, 2014; Roberts et al, 2017; Yokoyama et al, 2018). This has been applied widely to constrain the absolute timing of various geological events, such as carbonate diagenesis (Brigaud, Andrieu, Blaise, Haurine, & Brarbarand, 2021; Godeau et al, 2018; Lawson et al, 2018; Macdonald et al, 2019; Mangenot, Gasparrini, Gerdes, Bonifacies, & Rouchon, 2018; Mueller et al, 2020; Pan et al, 2020; Shen et al, 2019), brittle deformation (Beaudoin, Lacombe, Roberts, & Koehn, 2018; Goodfellow, Viola, Bingen, Nuriel, & Kylander‐Clark, 2017; Hansman, Albert, Gerdes, & Ring, 2018; Karabacak et al, 2019; Nuriel et al, 2019; Roberts & Walker, 2016), hydrothermal alteration (Coogan, Parrish, & Roberts, 2016; MacDonald et al, 2019), hydrocarbon migration and charge in petroleum systems (Holdsworth et al, 2019; Rochelle‐Bates et al, 2020) and geofluid events (Brigaud et al, 2020; Parrish, Parrish, & Lasalle, 2018; Roberts & Walker, 2016; Yang, Liu, et al, 2021; Yang, Wu, et al, 2021).…”