tectonic style meaning in Chinese

构造类型构造样式
构造型式

Tectonic styles and oil - gas distribution in yitong graben
伊通地堑构造样式及其油气分布规律
The tectonic style inside the basin is characterized by occurrence of anticlines from the margins to center of the basin , with two limbs mostly starting from reverse faults , developing a tectonic pattern of two faults sandwiching an uplift
盆地内部的构造样式以自盆地边缘至中心以此形成背斜构造为显著特徵，背斜两翼多发育逆断层，构成“两断夹一隆”的构造格局。
Different tectonic style exists in the upper and lower layers of the yanshanian boundary . the lower layers takes on the tectonic style of thrust fault and nappel . the upper layers hi step positive fault
2 、盆地燕山期构造界面上下不同构造层具有完全不同的构造样式，构造界面下伏构造层呈现冲断褶皱、推覆构造样式，构造界面上覆构造样式为阶梯状正断层，整体呈现“双层”结构型式。
The geological and geophysical studies show that there are large discrepancies for the distribution , strike - slip direction and tectonic styles of the faults in the southern and northern parts of the qinghai - xizang plateau , and for the deep crustal architectures in the eastern and western parts of the southern plateau
摘要青藏高原南部与北部的断裂带走滑方向不同，断裂带在高原东、西两侧的展布规律和构造运动方式也存在极大的差异。