在山麓地带，阶地与麓原面联合成一级地貌面，二者在空间上连续、在高度上可比。
In the piedmont zone the terrace and pediment surface jointly formed a geomorphic surface; they were contiguous in space with comparable elevation.
在断块山地的山麓地带，同一期构造运动形成的麓原面与构造阶地有一定的共生关系。
In the piedmont zone of fault-block mountains the pediments and tectonic terraces developed during the same tectonic movement are possessed of a certain paragenetic relation.
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