Volcanic activities often take place over several life-cycles. The repose stage of a volcano can vary from days to tens of thousands of years (Passarelli & Brodsky, 2012;Schmandt et al., 2019). However, what controls the episodicity of volcanic activities and how a dormant volcano is re-activated still remain enigmatic. Knowledge of magma chamber geometry and melt fraction is important for understanding such magmatic activities and monitoring the unrest of volcanoes. The Quaternary Datong volcanoes locates at the eastern margin of Ordos block, which preserve an Archean craton keel, and northern end of the Shanxi rift in the Northern Trans-North China Orogen (TNCO).The Datong volcanoes, consisting of about 30 calderas, are one of the largest Quaternary intraplate volcanic groups in China (Chen et al., 1992) (Figure 1a), which can be divided into two different parts (Xu et al., 2005). The eastern Datong volcanoes, distributed along the Liulingshanqian fault (LLSQF, Figure 1b), are widely covered by basaltic lava flows with a thickness of ∼3-25 m. The volcanic rocks in the eastern group are mainly composed of tholeiitic basalts (Xu et al., 2005). The western Datong volcanic group, including at least 13 volcanic cones, are composed of volcanic clastic debris with lavas occurring at the base. Potassium-Argon dating suggests that the volcanism in the western Datong volcanoes began in the Late Pleistocene (∼0.4 Ma), which commenced