The middle(early Himalayan)is the main deformation, characterized by the imbricate thrust structure system, whose west zone shows thrusting from SW toward NE.
中期(喜马拉雅早期)是主变形期,西带显示由SW向NE逆冲,以叠瓦状逆冲构造系统为其特征。
It shows sinistral strike-slip movement in western and middle segment, sinistral strike-slip and thrust in eastern segment.
西段和中段表现为左旋走滑,东段表现为左旋走滑逆冲运动。
Structures in middle zonation are simple and coal-controlled structural style is characterized by fold-thrust pattern, coal measures distributed stable in favor of exploration and development.
煤田中部地质构造相对简单,控煤构造样式以褶皱-断裂型为特征,含煤岩系赋存稳定,是有利的勘查开发区段。
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