“…The boundaries between these rift segments typically exhibit a variety of structural styles, such as transfer faults/zones, accommodation zones and basement highs (Clemson et al., 1997; Heilman et al., 2019; Meisling et al., 2001; Zhong & Escalona, 2020). As documented in previous studies, most continental rifts are segmented along strike regardless of whether they are incipient rifts (East African Rift, Corti et al., 2018; Hayward & Ebinger, 1996; Kolawole et al., 2021; Lao‐Davila et al., 2015; Scholz et al., 2020; Upcott et al., 1996); failed rifts (Bohai Bay Basin, Wu, Zhang, et al., 2022; Jianghan Basin, Wu et al., 2020); or fully evolved passive margins (Atlantic margin, Franke et al., 2007; Gouiza & Naliboff, 2021; Gouiza & Paton, 2019; Meisling et al., 2001; Pereira & Alves, 2011; Peron‐Pinvidic & Osmundsen, 2018; Soto et al., 2011; Tasrianto & Escalona, 2015; Gulf of Aden, Fournier et al., 2004; Leroy et al., 2010; northern South China Sea margin, Yang et al., 2022; Zhang et al., 2021; Zhao et al., 2020).…”