叶城盆地属于塔里木盆地的西南坳陷，在晚新生代沉积了巨厚的磨拉石建造。
The Yecheng foreland basin is a part of the southwest sag of the Tarim Basin and contains late Cenozoic molassic deposits with great thickness.
经断裂分析，太原盆地不是裂谷盆地，而是晚新生代的沉积盆地。
Fault analysis show that Taiyuan basin is sedimentary basin of Late Cenozoic rather than rifted one.
应用推荐