摘要
///Based on the comparative analysis of various well data and 3D seismic sections,the impact of various factors is studied on the geometry of the Kaijiang-Liangping trough and the distribution of reef-banks,such as the Late Permian regional palaeogeomorphologic framework,tectonic extension,system tracts of the Changxing-Feixianguan formations.The following conclusions were drawn: 1) at the end of Late Permian,the palaeogeomorphologic framework of the Sichuan Basin was “three depressions separated by three uplifts”; 2) the unevenness of extension caused the differences in the angles of slope on platform margin around the Kaijiang-Liangping trough; 3) the evolution of sequences reveals that transgressive systems tract(TST) deposits dominated the Longtan period and highstand system tract(HST) deposits dominated the mid-late Changxing period; and 4) the change of system tracts made it possible to develop multistage reefs near the platform margin.