摘要
介绍了太原盆地的地层概况和基本构造格局的形成,论述了晚新生代沉积过程,指出太原盆地的现代地貌面是区内外应力长期以来相互作用后达到平衡状态或趋向平衡状态时某一阶段的产物。
This paper introduces the general situation of the formation of Taiyuan Basin and the forming of basic structure layout of Taiyuan Basin, expounds the sedimentation process of late Cenozoic formation, and points out that the modern morphologic unit of Taiyuan Basin is the result of a certain stage when the internal and external stresses reach or incline to the equilibrium state after a long-term interaction.
出处
《科技情报开发与经济》
2008年第29期116-117,共2页
Sci-Tech Information Development & Economy
关键词
地质结构
地层概况
太原盆地
geological structure
general situation of formation
Taiyuan Basin
