层状地貌

贵州高原层状地貌与高原抬升

Step-like landforms and uplift of Guizhou Plateau

中国华北山地的层状地貌与喜马拉雅构造运动

Stratiform Geomorphology and Himalayan Tectonic Movement on the North China Mountains

长江三峡地区层状地貌研究

Study on the Steeped Landform in the Yangtze Gorges Area

贵州高原喀斯特层状地貌发育，至上而下主要有三级：Ⅰ级夷平程度高，称夷平面；

The karst bedded geomorphology development of Guizhou plateau involves three grades from upper to lower : I-grade is high level planation and is named for planation surface ;

利用卫星遥感影像，结合实地调查和测年结果，对共和盆地层状地貌系统进行了解译、分析。

Based on the satellite images , combined with field surveys and thermoluminescence dating of Quaternary sediments , the authors explain and analyze the step-like landform system of the Gonghe basin .

深入研究贵州高原的各种层状地貌的形成、变形及时代，可以弥补缺乏沉积记录等代用指标的不足，具有重建贵州新生代地质、环境演化历史的重大意义。

Therefore , studies on the features , formation , distortion and ages are very important to reconstruct ages and amplitudes of the Guizhou Plateau , whose Cenozoic evolution history is unclear because of the lack of sedimentation records .