The shape, thickness, stretch direction and bend type of the texture on both sides of the shear belt were observably different.
剪切带两侧的纹理在形状、粗细、延伸方向和弯曲类型上均表现为明显的不一致。
It is pointed out that, the number, scale and migration direction of fans were controlled by palaeogeomorphology, periods and strength of fault movement, and the development of slope-bend belt.
古地貌形态、断裂活动期次、强度及坡折带的发育控制了扇体的数量、规模与迁移方向。
The monocline observed in the field is the forelimb of fault-bend foldings. The second anticline belt inherits the first belt's displacement forming structure wedges.
第二排构造带继承第一排由侏罗系煤层传递而来的位移量，在中段由于受阻而发育构造三角楔，形成背斜。
The monocline observed in the field is the forelimb of fault-bend foldings. The second anticline belt inherits the first belt's displacement forming structure wedges.
第二排构造带继承第一排由侏罗系煤层传递而来的位移量，在中段由于受阻而发育构造三角楔，形成背斜。
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