Apatite Fission Track Thermochronology of Granite from Xiazhuang U Ore Field, South China: Implications for Exhumation History and Ore Preservation

Abstract Xiazhuang uranium (U) ore field, located in the southern part of the Nanling Metallogenic Belt (NMB), is considered one of the largest granite‐related U regions in South China. In this paper, we contribute new apatite fission track (AFT) data and thermal history modeling to constrain the exhumation history and evaluate preservation potential of the Xiazhuang U ore field. Nine Triassic outcrop granite samples collected from different locations of Xiazhuang U ore field yield AFT ages ranging from 43 to 24 Ma with similar mean confined fission track lengths ranging from 11.8 ± 2.0 to 12.9 ± 1.9 μm and Dpar values between 1.01 and 1.51 μm. The robustness time‐temperature reconstructions of samples from the hanging wall of Huangpi fault show that the Xiazhuang U ore field experienced a time of monotonous and slow cooling starting from Middle Paleocene to Middle Miocene (∼60–10 Ma), followed by relatively rapid exhumation in the Late Miocene (∼10–5 Ma) and nearly thermal stability in the Pliocene‐Quaternary (∼5–0 Ma). The amount of exhumation after U mineralization since the Middle Paleogene was estimated as ∼4.3 ± 1.8 km according to the integrated thermal history model. Previous studies indicate that the ore‐forming ages of U deposits in the Xiazhuang ore field are mainly before Middle Paleocene and the mineralization depths are more than 4.4 ± 1.2 km. Therefore, the exhumation history since Middle Paleocene plays important roles in the preservation of the Xiazhuang U ore field.