“…The original CRTBP was proposed in the 1770s with applications to the Trojan asteroids (Hou et al 2014), the Sun-Earth system and similar dynamical systems (Szebehely 1967), while the modified CRTBP with oblateness of primaries can be dated back to the 1970s. Many authors, such as Vidyakin (1974), Sharma & Rao (1976) and Idrisi (2014), have investigated this problem with theoretical discussions. In 2003, Oberti & Vienne (2003) successfully applied this theory to the Saturn system based on observed data, by considering the effect of Saturn's oblateness on the motions of Tethys and Dione's Lagrangian moons Telesto, Calypso and Helene.…”