While most volcanoes on Earth occur at plate boundaries, some volcanoes are located far from plate boundaries and are called intraplate volcanoes. Beyond the volcanism of upwelling hot mantle plumes, some mechanisms, including edge-driven convection (Ballmer et al., 2015;King & Ritsema, 2000), shear-driven upwelling of the asthenosphere (Conder et al., 2002;Conrad et al., 2010), and dehydration and big mantle wedge convection associated with the deep subduction and stagnation of slabs (Yang & Faccenda, 2020;Zhao et al., 2004), are invoked to explain intraplate volcanism. However, for most intraplate volcanoes, the exact mechanisms are still elusive due to insufficient constraints on structures related to deep magma chambers and channels.Northeast China is an ideal place for studying intraplate volcanism. There are more than 590 Cenozoic intraplate volcanoes that are mostly covered by alkaline basalts and are widely distributed as part of the circum-Pacific volcanic belt to the west of the Japan Sea back arc basin (Liu et al., 2001), including Changbaishan volcano, Wudalianchi volcano, etc (Figure 1). Among them, Wudalianchi volcano, located ∼1,800 km