1、

This study is a basis on revealing the tectonic evolution and active pattern, deducing the strike-slipping history and forecasting the future behavior of a strike-slip fault.

这一研究是揭示走滑断裂的构造演化与活动习性,反演断裂走滑活动历史并预测其未来行为的基础。

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2、

Experimental study on rupture propagation along Buried strike-slip fault

隐伏走滑断层破裂扩展特征的实验研究

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3、

On the Strike-Slip Fault of Coalfield and Its Research Significance

煤田走滑断层及其研究意义

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4、

Haiyuan strike-slip fault zone and its compressional structures of the end

海原走滑断裂带及其尾端挤压构造

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5、

A typical strike-slip extensional duplexes with a characteristic tulip flower structure are developed along the east-west oriented F fault ( PDZ) in Punda dextral strike-slip faults.

沙捞越Punda走滑构造为一典型的右旋走滑构造形式,是沿近东西向F断裂(PDZ)发育特征的负花状构造或郁金香构造,并构成走滑伸展双重构造。

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6、

Bozhong 34-1 complex fault-blocks zone is located in Yanlu strike-slip fault zone.

渤中 34-1 浅层复杂断块区处于郯庐走滑断裂带内,受其影响和控制该区断层较发育.

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7、

The Altyn Tagh fault zone is an important strike-slip fault zone in northwestern China.

阿尔金断裂带是西北地区一条重要的走滑断裂带。

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8、

in this case, the damage was caused by movement with of a'strike-slip fault. "

在此次事件中, 是走滑断层的运动造成了破坏.

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9、

in this case, the damage was caused by movement of a'strike-slip fault. "

这种情况下, 破坏是由走向平移断层的运动引起.

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10、

normal fault, reverse fault and strike-slip fault.

正断层 、 逆断层和走滑断层.

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11、

Karayulgun dextral strike-slip fault, which is a thin-skinned structure, adjusted the deformation difference located at frontal range of Quele area.

喀拉玉尔滚右旋走滑断层为薄皮构造,调节了却勒地区东、西段前缘的变形差异。

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12、

The main faults are the thrust fault in its northern margin and the strike-slip fault in its southern margin.

最主要的两条大断裂分别是北缘和南缘断裂,北缘为逆冲断裂,南缘为走滑断裂。

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13、

The extensive development of the basin into the east-west fault structure, has gone through the region of fracture dynamics tensile, Extrusion, regional depo-sition, squeezing the strike-slip tectonic evolution stage.

盆地内广泛的发育有近东西向的断裂构造,在断裂动力学上先后经历了区域的拉张,挤压,区域沉积,挤压走滑等构造演变阶段。

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14、

Summarized that synclines are open, anticlines are tightly closed, and plane distribution pattern of folds was parallel and juxtaposition. The faults were mostly thrust fault, and tectonic types can be divided into 3 styles: compression tectonic style, strike-slip style and extending tectonic style.

认为研究区内向斜开阔、背斜紧闭,褶皱构造的平面展布以平行并列式为主,断裂多为逆冲断层,构造样式可划分为压缩构造样式、走滑构造样式和伸展构造样式三大类型。

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15、

This paper proposed that Xiangyun nappe was formed at the regional tectonic settings of the Paleogene India-Eurasian plate subduction, collision resulted in the Jinsha River-Red River fault zone and Chenghai fault zone strike-slip movement.

提出祥云推覆构造是在古近纪印度欧亚板块俯冲、碰撞导致金沙江红河断裂带和程海断裂带走滑运动的区域构造背景下形成的。

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16、

Jiaolai Basin is a strike-slip and pull-apart basin controlled by the Yishu Belt and Wulian-Jimo-Muping Fault.

胶莱盆地是中生代走滑拉分盆地,其形成与发育受到沂沭断裂和五莲 - 即墨 - 牟平断裂的控制.

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17、

The Indochina-Sumatra block, delimited by East Vietnam Fault, East Andaman sea Fault, Red River Fault and Sumatra Fault, appears as a lozenge-shaped dextral strike-slip duplex.

印支&苏门答腊地块是被东越南断裂、东安达曼海断裂、红河断裂和苏门答腊断裂等四条断裂围限的呈菱形的右行走滑双重构造。

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18、

Jiaolai Basin is a strike-slip and pull-apart basin controlled by the Yishu Fault Belt and Wulian-Jimo-Muping Fault.

胶莱盆地是中生代走滑拉分盆地,其形成与发育受到沂沭断裂和五莲-即墨-牟平断裂的控制。

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19、

Processing about quantitative study of large-scale strike-slip movement on Red River Fault Zone

红河断裂带大型右旋走滑运动定量研究的若干问题

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20、

the research results indicate that the liyang earthquake was caused by a right lateral strike-slip dislocation with some normal dip-slip component along the east branch of the maoshan fault belt under the action of the nee compression stress field.

研究结果表明,该地震是在北东东向挤压应力作用下,沿着茅山断裂带东支发生了右行走滑错动兼有正断层性质的倾滑分量。

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