In Situ Monazite U-Pb Ages in Thin Sections from the Giant Bayan Obo Fe-REE-Nb Deposit, Inner Mongolia: Implications for Formation Sequences

The Bayan Obo deposit is the largest REE resource in the world. Although many isotopic dating methods have been applied, ages based on petrography and closure temperatures still lack discussion. In this study, three digital petrographic images were created based on full-scanning microscopy, BSE, and TESCAN integrated mineral analysis (TIMA), providing a more scientific method for analyzing the mineral types, distributions, and content of the Bayan Obo deposit. By combining the full-scan images, monazites were selected in thin sections and dated in situ. The monazite in the body ores sample yields three Pb-207 intercept ages of 657 +/- 25 Ma (MSWD = 1.06), 763 +/- 16 Ma (MSWD = 1.3), and 689 +/- 22 Ma (MSWD = 8.1), and the monazite in one section yields maximum and minimum ages of 1393 +/- 142 Ma and 429 +/- 24 Ma, respectively. Combined with previous studies, the earliest and major stages of carbonatites, REE, and dikes in the Bayan Obo deposit area were dated at similar to 1.4 Ga and similar to 1.3 Ga, respectively. Due to the multiple subduction and accretion events related to the Paleo-Asian Ocean and North China Craton, the Bayan Obo deposit is intensely overprinted, with a tectonic-thermal event recorded at similar to 1.0-0.2 Ga. The multiple or protracted isotopic similar to 1.4-0.4 Ga ages in the Bayan Obo deposit account for five reasons. First, the separate thermal events and the partial recrystallization of monazite. Second, the diffusion of daughter products from the host mineral over time. Third, differences in the closure temperatures of different minerals and isotopic chronologies. Four, resetting of the closure system due to high temperature and hydrothermal alteration. Five, the minerals and transformed ores that formed in the Paleozoic. The in situ monazite U-Pb ages in thin sections provide insight into formation sequences from the giant Bayan Obo Fe-REE-Nb deposit.