地貌面 face
- 多个构造旋回可以形成一系列由河流阶地和麓原面组成的多级联合地貌面。
Multiple tectonic cycles may produce a multi - stepped landforms consisting of a series of pediments and corresponding river terraces. - 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. - 各级阶地面上发育了厚度不等的黄土-古土壤序列,为地貌面断代与区域对比提供了便利。
Each terrace is covered by a loess-paleosol sequence of different thickness, which facilitates dating the geomorphic surfaces and making a regional correlation.
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