At 3:42 a.m. (UTC+8) on July 28, 1976, a magnitude (M s ) 7.8 earthquake hit Tangshan, an industrial city in North China just 150 km east of Beijing, causing a surface rupture >47-km long (Figure 1) (Guo et al., 2017). About 15 h later, a second shock, of M s 7.1, occurred ∼40 km to the east-northeast on a different fault and ruptured surface >6-km long (Guo et al., 2017). These two events, together referred to as the Great Tangshan earthquake, obliterated the city of Tangshan and killed >240,000 people, making it the deadliest earthquake of the 20th century (Chen et al., 1988). More than 40 years have passed, but the memory of the devastation remains fresh. Thus, a series of moderate (M ≥ 4.5) earthquakes in recent years near the 1976 Tangshan earthquake rupture zone, including an M s 5.1 event on July 12, 2020, have raised social concern and scientific debate: are these events aftershocks of the Great Tangshan earthquake? Or are they indicators of stress buildup for future large earthquakes in Tangshan or somewhere in North China? North China, or the geologically defined North China block, includes the North China Plain and the mountain ranges and the Ordos Plateau to the west. It is an Archean craton that was reactivated during the