摘要
The Lishu fault depression in the south of Songliao Basin formed in the Indo-Yanshan movement and developed on the basis of the NE-NNE and NW-NNW direction basement rifts.Based on the 1∶50 000 high-precision gravity and magnetic data processing and combined with drillings,the authors reveal that the basement lithology is mainly metamorphic rock,with carbonate outcropped locally,there are roughly intrusive rocks of Hercynian and Indosinian-early Yanshan periods in the area and infer that the Sauron-Linxi suture zone passes from here.The basement structure and basement fault of this region established the structural form of the basin prior to late Jurassic and influenced the stratigraphic framework and filling pattern of the late basin.