Its common structural forms are the shovel-like normal fault and spoon-like normal fault.
常见的构造形态为铲式正断层和勺状正断层。
The paper focus on the horizontal and vertical characters of tensional normal fault formed in the early Caledonian.
着重分析了加里东早期张性正断裂的平面和剖面特征。
The normal fault zone with NEE trending are cut by some NNW faults with left-lateral dislocation in the north of the basin.
盆地北缘的北东东向正断层被北北西向断裂左旋错动。
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。
A discussion on the distribution law of outburst seam in the two walls of the normal fault has a certain apocalypse to the geology.
讨论正断层两盘突出煤体的分布规律对于构造地质学也具有一定的启示。
The MCT1 was originally a south-vergent ductile thrust, which was later transformed into a normal fault after it underwent NNE-trending folding.
MCT1原为向南逆冲的韧性断层，后遭受北北东向褶皱作用而转变为正断层。
On the basis of granulometric analysis of samples from colluvial wedge sediments caused by normal fault, the sedimentary environment is discussed.
通过对崩积楔沉积物进行粒度特征分析，研究崩积楔形成时的沉积条件和环境特征。
The Xinding basin in the north of Shanxi rift system is a normal fault-controlled extensional graben and has a strong neotectonic process during the Quaternary.
忻定盆地是山西地堑系北部的一个张性断陷盆地，第四纪构造运动活跃。
The structural pattern of the normal fault assemblage that occurred in the Early and Middle Jurassic may have initiated some small-scale petroleum and gas pools.
早、中侏罗世形成的正断层组合构造样式，可形成一些小规模油气藏。
The extension of the continental lithosphere that gives rise to extensional basins is generally considered as a shear process on major, gently dipping normal fault.
形成拉伸盆地的大陆岩石圈伸展构造作用，一般认为是沿大型缓倾角正断层（滑脱断层）的剪切作用过程。
Extensional fold is an important component part of tectonic deformation in tensional basins, which distributes widely, and mostly belongs to normal fault-related folds.
伸展褶皱是张性盆地区构造变形的重要组成部分，其分布相当普遍，多属于与正断层相关的褶皱。
The third phase deformation is normal fault that developed along the formation interface from different times or the same stratum with different lithology in the basin.
第三期变形为沿盆地内不同时代地层界面或同一地层不同岩性界面发育的伸展拆离构造；
The reversal of features, particularly structural features such as faults, by reactivation. For example, a normal fault might move in a direction opposite to its initial movement.
一些特征，尤其是构造特征的逆转，如断层的再活化。如一条正断层在运动方向上可以与它最初运动的方向相反。
This study shows that the formation of antithetic normal fault is controlled by NE WS strike tensile stress and dextral shear stress and the strike is nearly vertical to the tensile stress.
研究认为，北北东向反向正断层的形成受北东—南西向张应力及右旋剪切力控制，反向正断层的走向与张应力方向基本垂直；
This study shows that the formation of antithetic normal fault is controlled by NE WS strike tensile stress and dextral shear stress and the strike is nearly vertical to the tensile stress.
研究认为，北北东向反向正断层的形成受北东—南西向张应力及右旋剪切力控制，反向正断层的走向与张应力方向基本垂直；
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