“褶皱带”造句
塞德霍尔姆认为斯维科芬
褶皱带本身为一老的构造,被比较年轻的卡累利
褶皱带所截断.
Sederholm regarded the Svecofennide belt as an older structure truncated by a younger Varelide belt.
甘孜 - 理塘断裂带是义敦造山带与雅江
褶皱带的分界断裂.
Garze - Litang fracture zone separates Yidun orogenic belt from Yajiang folded belt.
壳内盆地带主要形成于印支—燕山期强烈的挤压
褶皱带内.
These crustal basin belts formed by strong basal compression folding in the Indosinian - Yanshanian period.