Fault is the main factor controlling the tectonic evolution in Dongying depression.
断裂是控制东营凹陷构造演化的主要因素。
The formation and evolution of the fault is discussed as well.
最后,讨论了该断裂带的形成与演化。
Junchuan fault, a magor fault, controlled the formation and evolution of the depression.
军川断裂是绥滨坳陷的主要控盆断裂,控制了其形成和演化。
The evolution of major fault zones is analysed with the forward modelling method.
利用正演模拟方法,分析了主要断裂带的发育演化。
The evolution of major fault zones is analysed with the forward modelling method.
利用正演模拟方法,分析了主要断裂带的发育演化。
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