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strike slip

网络走向位移；走向滑距；滑移断层

strike slip

网络释义

strike slip

走向位移

strick用法_百度知道 ... strike for 为…而罢工 strike slip [地理学]走向位移；走向滑距 general strike 大罢工 ...

走向滑距

strick用法_百度知道 ... strike for 为…而罢工 strike slip [地理学]走向位移；走向滑距 general strike 大罢工 ...

滑移断层

...1日，在印尼苏门达腊发生规模8.6级地震，该断层属滑移断层（Strike Slip），过去类似型态的断层，从未发生过如此强震。

平移

测量学专业词汇英语翻译... ... 平移 translation movement 平移，走向断距 strike slip 平移元素，转换元素 transitional element ...

例句：

strike-slip fault - a fault on which the two blocks slide past one another. The San Andreas Fault is an example of a right lateral fault .

走滑断层 -两个岩体顺断层面走向相对滑动的断层。圣安德烈斯断层是一个右旋断层的例子。

The pull-apart basin formed around the steps of the strike-slip fault refers to a low terrain area due to tensile force from the fault .

拉分盆地指沿着走滑断裂带弯曲部位，由于拉张而产生的地形上的低洼处，多形成于走滑断裂带次级断裂的间列部位。

Hydrocarbon in footwall and hanging wall distribute as "sine curve " is the result of the "silk ribbon effect" of strike slip fault .

走滑断层 “丝带效应 ”造成断层两盘油水呈 “正弦曲线 ”模式分布。

Analyses of the ductile fabrics and mylonitic microstructure suggest that strike - slip was sinistral in the early stage of collision .

岩石韧性组构和糜棱岩变形的微构造研究表明，碰撞前期走滑为左行。

the focal mechanism is mainly left - lateral strike - slip , with a very small normal fault slip component .

这次地震的震源机制基本上是左旋走滑，带有微小的正断层滑动分量。

Faults which move horizontally are known as strike -slip faults and are classified as either right-lateral or left-lateral .

水平移动的断层称为走滑断层并分类为右旋与左旋。

The secular GPS crustal deformation image has reflected the relatively complete left lateral strike slip movement of this active fault zone .

长趋势 GPS 地壳形变图像反映了这条活动断裂带相对完整的左旋走滑活动。

Local structural styles became more complicated due to the stacking of extensional structures and strike-slip structures of Meso-Cenozoic .

局部由于受到中、新生代时期的伸展构造和走滑构造的叠加，构造样式变得更加复杂。

The two boundaries of the Yili Block have been reworked by the Permian strike-slip faulting .

伊犁地块的南、北缘边界在二叠纪期间经受了走滑作用的强烈改造。

Since the Late Pleistocene, the tectonic regime has changed to strike slip and reverse faulting one.

晚更新世以来，构造体制转化为走滑 —逆冲机制。

the seismic isolation effect analysis for the pipe segment under strike slip faulting containing normal(reverse) fault component .

分析走滑断层含正（逆）滑分量时的隔震管段隔震效果。

The early fault zone was reconstructed and became dextral right-step "Z " -type fault during dextral strike-slip stage .

在右行走滑改造阶段，早期左行右阶断裂带被改造为 “Z ”型右行右阶断裂带。

Faults which show both dip-slip and strike-slip motion are known as oblique-slip faults .

断层既有倾滑又有走滑运动特征的被称为斜滑断层。

The lateral ramp fault is taken as an effective pathway of hydrocarbon migration in the strike-slip fault .

相对于走滑断层而言，侧断皮断层是有效的天脍气运移优势通道。

The strike slip structural style occurs vertically as flower structures and laterally as echelon faults and horse tail faults .

走滑构造样式主要表现为剖面上的花状构造、平面上的雁列断层及马尾状断层等；

Yitong basin is a strike-slip stretching basin which is controlled mostly by the strike-slip fault of the north-west boundary in Cenozoic .

伊通盆地主要是受西北缘走滑断裂控制的新生代走滑 -伸展盆地；

These suggest that the strike-slip movement lasted from the earliest to the latest Early Cretaceous .

这反映断裂带的走滑运动从早白垩世初期持续到早白垩世后期。

The deformation is characterized mainly by thrust compressing and dextral strike slip component .

变形特征以逆冲挤压为主兼具右旋走滑分量。

The main type of fracture are tensional fault , compressional fault and strike slip fault .

断裂的类型主要有拉张或张扭断层、拉压或压扭断层、走滑断层。

The strike-slip system is a "vertical belt-like " thick-skinned tectonics at the crust scale.

走滑构造是一种 “垂直带状的 ”厚皮构造。

The strike-slip faults have played a constructive role in the growth of both shallow and deep traps .

走滑断层在深浅层圈闭形成过程中起到了建设性作用。

The structural planes are controlled by right-lateral strike-slip structural belt .

综合分析认为，这些结构及其分布是受右行走滑剪切带的控制。

strike slip

strike slip

走向位移

走向滑距

滑移断层

平移

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