基本释义:

走向滑动微断层

网络释义

1)strike-slip microfault,走向滑动微断层

2)strike-shift fault,strike-slip fault,走向滑动断层(地)

3)strike-slip thrust,走向滑动冲断层

4)flaw fault,走向滑断层

5)dextral strike-slip fault,右旋走向滑动断层

6)dog-legged strike-slip fault,折线形走向滑动断层

用法和例句

dog-legged strike-slip fault

折线形走向滑动断层

The strike-slip-thrust fault strikes to 280-305°and the fault plane dips to southwest with angle of about 30°.

走滑逆断层走向为280°—305°。

Sudden rupture and displacement occurs with normal, reverse, strike-slip, or oblique-slip faulting.

突然破裂和位移伴随正、逆、走向滑动或斜向滑动断层作用而发生。

If the relative movement of hanging wall and footwall is parallel to the strike of fault plane, it is a strike slip fault.

如果断层上盘和下盘的岩石相对位移运动是平行断层面走向的，这种断层称为走滑断层。

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。

second group,strike 195°,dip 80°,rake -165°

第二条断裂,走向195°,倾角80°,滑动角—165°。

A Concept Model of Determination of Shear Sense of Strike-Slip Faults in Seismic Profiles:An Example from the Alaganbei Fault in the Eastern Tarim Basin

地震剖面中走滑断层旋向判断模型——以塔东阿拉干北断层为例

The de-yelopment of the new down-warped basin at Quaternary at the north segment of Beijing down-warped basin may be related to the left-lateral strik-slip movement of the west-north faults.

北段第四纪时新发育的断陷盆地可能与北西向断层的左旋走滑活动有关。

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。

Strike-slip seismic fault and mainshock-aftershock earthquake sequences are dominant in Whole Yunnan area.

总体上云南全区地震断层以走向滑动为主，地震序列以主余震型为主。

One mode is slippage along the discontinuity provided by the lubricated fault plane.

其中一种方式是沿着润滑的断层面所形成的间断面而发生滑动。

Fold line plane was more suitable than the circular slip plane for the shallow slide.

对于膨胀土边坡的浅层滑动面，采用折线滑动面比圆弧滑动面更接近于实际情况。

For instance, a strike fault is one which strikes essentially parallel to the trend of adjacent rocks.

例如，走向断层就是指那些断层走向与围岩走向一致的断层;

Dextral strike-slip evidence on seismic slice for Tanlu strike-slip fault

郯庐走滑断层右旋走滑的地震切片证据

SLIP DISPLACEMENT AND ITS RATE ABOUT ZEMUHE FAULTS

则木河断裂带的走滑位移及滑动速率

rhegmatic pattern

区域性走向滑移断裂模式

At the same time, the creep rate of the fault in the strike and dip directions are found to be 18.6 cm/year and 1.4 cm/year respectively.

同时得到断层走向、倾向蠕动速度分别为18.6厘米/年及1.4厘米/年.

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;