如何控制陆相地层横向不稳定性，是盆地分析的难点。
The difficulty for analysing basin sedimentation is how to control the horizontal variation of continental strata.
榆木山是位于河西走廊前陆盆地系中张掖盆地和酒东盆地之间的横向隆起山地。
The Yumu mountain is a transverse highland between the Zhangye basin and Jiudong basin in the system.
通过对塔里木盆地地震资料的层析反演取得了较好的结果，揭示了浅部地震速度具有较大的横向变化。
The tomographic inversion of seismic data is better shown in the Talimu Basin and it revealed obvious lateral velocity variation in shallow levels.
应用推荐