Permian, Permian and Triassic were the outset, peak and close stages of the Emei Taphrogenesis, respectively.
二叠纪前为地裂运动伊始期; 二纪为地裂运动高峰期; 三叠纪为地裂运动衰退期。
The structural framework, formed by Emei Taphrogenesis, controlled the sedimentation and diagenesis, thus more or less controlled the distribution of hydrocarbon in the a...
地裂运动形成的构造格局对沉积、成岩有一定的控制作用,进而在一定程度上控制了该区油气的分布。
The structural framework, formed by Emei Taphrogenesis, controlled the sedimentation and diagenesis, thus more or less controlled the distribution of hydrocarbon in the area.