Three stages of Meso Cenozoic evolution in the Tan Lu fault zone were all associated with volcanic activities.
在郯庐断裂带中生代以来的三期演化中，都伴生了火山活动。
This paper discusses the geometrical style, formation and evolution of deformed structures in the large scale Meso Cenozoic sedimentary basins in the west of China.
重点讨论了中国西部中新生代大型沉积盆地变形构造的几何结构样式、形成与演化模式。
The formation and evolution of the Meso-Cenozoic basins in the middle and southern part of southern North China was mainly controlled by the Tanlu fault system and the Dabie orogenic belt.
南华北中南部中新生代盆地的形成演化主要受郯庐断裂带、大别造山带构造运动的制约。
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