“…The later tectonic uplift phase related to successive continental collisions, including the Indo-sinian, Yanshanian (Pacific subduction), and Himalayan Orogenies, extended from the Cretaceous to the present (Hao et al, 2008;Korsch, Mai, Sun, & Gorter, 1991;Ma et al, 2008). The associated palaeo-thermal regimes have changed accordingly (Liu, Tang, Chen, & Tang, 2017). These variations in structural evolution and thermal regimes were of great significance on the future of petroleum systems and main events (Yong, Fan, Lv, Tang, & Wang, 2018;Zhu, Qiu, Liu, Xiao, & Hu, 2019).…”