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1·Focal mechanisms demonstrate that most are of thrust fault and next the normal.

几百次单个地震的震源机制解显示出以逆断层和正断层机制为主。

2·The south Qinling has formed an imbricated thrust fault at low angle from the north to the south.

南秦岭自北向南产生低角度叠瓦状逆冲断裂。

3·The tear fault intersected with low angle normal fault or thrust fault can form some traps, e. g. trap-door structure trap.

撕裂断层与低角度正断层或逆冲断层相交时常形成有利圈闭，如活板构造等。

4·It was considered that method of equilibrium profile is the best method to recognize and quantitatively study active thrust fault and underlying fault.

而平衡剖面法乃是识别和定量研究活动逆断层，特别是隐伏断层的最好方法。

5·The trend of the high anomaly in south west area of the study region is basically same with the thrust fault, so we infer that the anomaly is caused by it.

研究区内西南部区域高异常在剖面图上其走向与逆冲推覆构造走向基本一致，推测异常是由逆冲构造引起，也可能是盖层中侵入岩引起。

6·The Changpo reverse anticline controls the location of Changpo-Tongkeng deposit, while the bed-parallel shear fracture zone and thrust fault control the ore bodies.

长坡倒转背斜控制长坡-钢坑矿床的产出，层间剪切破碎带和逆掩断层控制着矿体的空闻位置。

7·Structural characteristics of inversion structure, fold association style, thrust fault zone upright strata developed belt shown in great profiles were also discussed.

对剖面中反映的构造反转、褶皱组合样式、逆冲断裂带、直立地层发育带的构造特征进行了探讨。

8·There is a normal deposition sequence stratigraphy beneath the lower wall of over-thrust fault, such as Jurassic, Triassic, Permian-Carboniferous, Cambrian-Ordovician system.

在逆冲断裂的下盘，是一套正常沉积层序的地层，分别为侏罗系、三叠系、石炭—二叠系、寒武—奥陶系等地层。

9·The stress fields are compression ones, in that conditions, the structure styles are folds, Fault-bend folds, Fault-Propagation folds, Detachment folds, imbrications-thrust faults and so on.

研究区构造应力场主要为挤压应力场，区内主要形成褶皱、断弯褶皱、断展褶皱、叠瓦逆冲构造、冲起构造和逆冲三角构造等构造样式。

10·The Luochen Copper Mine is situated at the composite part of the protruding south front of the large scale thrust( slip) nappe and the NNE-trend strike-slip thrust fault in the south edge of Jiuling.

罗城铜矿区处于九岭南缘大型推（滑）覆构造往南突出的前锋与NNE向走滑冲断带复合部位。