摘要
金-羊盆地西缘断裂是辽西一系列北东向逆冲推覆构造的典型代表,对金-羊盆地的形成演化和盆内沉积地层分布具有重要的控制作用。本文通过野外地质调查并结合有关资料,论述了该断裂的构造特征、演化历史和对其东侧金-羊盆地形成发展的控制作用。
The Fault zone on the west edge of Jin-Yang Basin,being a typical representation of a series of NE nappe structures in West Liaoning,controlled the formation and evolution of Jin-Yang Basin, and the distribution of sedimentary strata According to geological investigation and information,the structure characteristic and evolution history of the fault zone and its controlling on the formation and evolution of Jin-Yang Basin is discussed
关键词
盆缘断裂
控盆作用
断裂构造
沉积地层
构造演化
West Liaoning
Jin-Yang Basin
fault zone on the edge of a basin
controlling on a basin
