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走向断层

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Sahnto toward the eastern side of the formation of nearly 10 meters fault scarp, looking from the North China Plain, the situation is magnificent.

山土东侧的走向断层形成近10米的断层崖,从华北平原仰望,形势雄伟。

Based on systematic structural interpretation with 3D seismic data and analysis on regional geology and drilling data, the fault system and tectonic style of the Yitong Graben are studied.

通过对三维地震资料进行系统的构造解析,结合区域地质和钻井资料的分析表明,伊通地堑的断层系统在平面上主要由近东西向的张性正断层和北东走向的张剪性断层组成,反映盆地具右旋走滑的应力体制;断层在演化序列上分为4个类型,与盆地的形成和演化之间存在良好的对应关系。

Finally, the controlling role of structure to sedimentary was analyzed. It is showing that time-transgressive different structural zone developed different sedimentary system; the thickness of sedimentary formation and lithic facies were different on the simultaneous lateral layer of growth fault; the expansive orientation of sedimentary system was controlled by the strike of fault; the sedimentary system developed differently became of the tectonic activity was differently; step thrust slip fault can built-up multistage fault fans.

最后分析构造对沉积的控制作用,主要表现在:不同时期不同的构造带发育不同的沉积体系;生长断层造成断层两侧同期地层沉积厚度与岩相的明显差异;断层的走向控制沉积体系的展布方向;构造活动导致沉积体系的发育有显著的差异;阶梯式逆冲断层可形成多级断崖扇。

An oblique fault is one that strikes obliquely or diagonally to the strike of the adjacent rocks.

斜向断层是指断层走向与围岩走向斜交的断层。几个相邻的建筑物合并表示成一个完整的建筑区。

An oblique fault is one that strikes obliquely or diagonally to the strike of the adjacent rocks .

斜向断层是指断层走向与围岩走向斜交的断层。

If the strike of a fault is parallel to the general trend of regional structures, it is called longitudinal fault

如果断层走向与区域构造的总体走向相平行,就称之为纵向断层

If the strike of a fault is perpendicular or diagonal to the trend of regional structures, it is refer to transverse fault.

如果断层走向与区域构造线走向相垂直或斜交,则称之为横向断层。

Many ultrabasic bodies in the orogenic association occur along strike faults, which gives a simulated concordant relationship

与造山运动共生的许多超基性岩体沿着走向断层出露,表现出假的整合关系。

We conducted high-density resistivity surveying combining with boring data across F1 and F3. The results show that F1 cut the 3rd terrace which formed in late Pleistocene, and the last activity was extensional normal slip by echelonment falling down toward the basin. F3 stroke zigzag and cut the 1st alluvial-proluvial terrace and Holocene stratum with large displacement of fault and wide fracture zone in bedrock, and the last activity is the continuous falling around the fault.

结果表明,F1断层错断了盆地区内晚更新世晚期至全新世早期的Ⅲ级阶地;受拉分构造的影响,该断层最新活动显示了向安远拉分盆地方向迁移的阶梯状递减的张性正断裂性质。F3断层在走向上呈锯齿状,错断了山前Ⅰ级冲洪积阶地及全新统至上更新统地层,断距大,基岩破碎带宽,新活动主要表现为断层附近原地连续沉降。

A dip fault strikes essentially parallel to the direction of dip of the adjacent beds, that is to say, its strike is perpendicular to the strike of the adjacent beds.

顺层断层是指断层面平行岩层层理的断层;倾向断层的走向是平行于围岩的倾向的,也就是说,它的走向是垂直于围岩的走向的

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