“…Extensive studies have been conducted to understand the seismogenic structure and physical causes of large intraplate earthquakes (e.g., Campbell, 1978; Di et al., 2021; Iio & Kobayashi, 2002; Johnston & Schweig, 1996; Stevenson et al., 2006; Talwani, 1988, 1999). Several studies proposed to link their occurrence with the presence of localized weak zones forming from either the intersections of faults (Dentith & Featherstone, 2003; Gangopadhyay & Talwani, 2003; Gangopadhyay et al., 2004; Johnston & Schweig, 1996; Talwani, 1988, 1999; Zhu et al., 2022), oriented ancient rifts (e.g., Kato et al., 2009; Zoback & Richardson, 1996), fluid‐related weakening zone (Craig et al., 2017; Gardonio et al., 2018; Lin et al., 2022; Pavan Kumar et al., 2017; Umeda et al., 2011), or vicinity of booming plutons (e.g., Stevenson et al., 2006).…”