辽河盆地是中、新生代发育起来的裂谷盆地。
Liaohe basin is a rift basin developed in the Mesozoic and Cenozoic.
二期构造运动导致了辽河盆地复杂断裂体系的形成和演化。
Two phases of the structural movement lead to forming and evolution of complex fault system in the Liaohe basin.
应用构造分析理论和方法，对辽河盆地构造断裂，进行了系统、深入的研究。
The paper makes a systemic and thorough studies to the structure fracture in Liaohe Basin by using the theory and method of structure analysis.
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