大同盆地是一受北东向主干断裂控制的不对称地堑盆地。
The Datong Basin is an unsymmetrical graben, the main controlling fault of which runs north east.
舒兰盆地位于依兰—伊通裂谷中段，为半地堑盆地，依兰—伊通裂谷为盆地的边缘断裂，控制了盆内白垩系及新近系含煤地层沉积。
The Shulan basin is located in the middle sector of Yilan-Yitong rift, and is a semi-graben basin.
此文证明了半地堑理论的实用性与优越性，是盆地分析工作中的一种新思路、新方法。
This paper proves the practicality and advantages of the half-graben theory which is a new thinking and a new method in basin analyses.
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