1、

Mesozoic Cenozoic continental strike slip fault system and its roles on uranium mineralization in Hunan and Guangxi, China

湘桂地区中新生代走滑断裂系统对铀成矿的控制作用

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2、

Earthquake nucleation with strike slip fault was analyzed by means of the variational boundary integral method and slip weakening friction law.

利用边界单元法和滑移弱化摩擦本构关系分析了平移断层上地震的产生。

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3、

Structural Characteristics of the Dien Bien Phu Strike Slip Fault Zone and Its Regional Tectonic Implication

奠边府走滑断裂带的构造特征、遥感解译及其区域构造意义

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4、

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。

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5、

Fula sub basin is a Mesozoic and Cenozoic continental rifted basin, which is controlled by the Center Africa Strike slip fault.

穆格莱德盆地福拉凹陷是一个在中非走滑断裂带控制下发育而成的中、新生代内陆断陷湖盆。

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6、

This earthquake mentioned in the paper occurred along NEE fault, with strike slip fault shifting and stronger P wave emission in the direction of S by W.

文中提出地震沿着北东东向断层发生,主要作走滑错动,在南偏西的方向上有较强的纵波发射。

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7、

On the other hand, the NW side of the granite dome is mainly manifested by a shallower-level normal fault and normal-strike slip fault.

而花岗岩穹隆的西北侧则主要表现为较浅层次的正断层及平移正断层。

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9、

The Cenozoic tectonic evolution mainly includes a series of tectonic activities of inland rift, strike slip fault movement, convergent tectonic belt formation, inland magmatism and strong uplifting, etc.

新生代构造演化主要经历了陆内裂陷、断裂走滑活动及会聚构造带的形成、陆内岩浆活动、强烈的抬升等一系列构造运动。

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10、

The results show that: ( 1) the earthquakes and hot springs are mostly located in the three main NEN trending strike slip fault zones and associated P, R ′ faults;

结果表明:1研究区地震和温泉主要集中在3条NNE向主走滑断裂带及其伴生的P、R′断裂带;

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11、

The rate for all strike slip fault system in the eastern Qinling Mountains is about 2.25~ 4.75mm/a. This rate value reveals the velocity difference for the North China block and the South China block in the late Quaternary Period.

估算出东秦岭地区活动断裂系左旋活动速率约为2.25~4.75mma,它大致反映了中晚第四纪华南与鄂尔多斯、华北平原活动地块向东滑动速率的差异。

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12、
13、

The results show that the velocity in dip slip of Qilianshan fault is larger than those in strike slip and tension, and the distribution of velocities along the fault are uneven.

结果表明,祁连山断裂活动速率在断层倾滑方向上明显大于走滑方向和张开方向,而且具有空间分布的不均匀性特征。

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14、

Study on a large ductile strike slip shear zone in the middle of the Shangnan Shangcheng fault zone

商南-商城断裂带中段大型韧性走滑剪切带研究

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15、

The buried hills mainly formed due to the differential rise and down which were caused by strike-slip extension fault of Mz and Cenozoic erathem ( Kz).

现今潜山山头主要受中、新生代走滑、伸展断层引起的差异升降来完成。

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16、

In the north is a strike slip fault;

北部为走滑型断裂;

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17、

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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18、

The tidal force may increase the shear stress on the fault plane and is favorable for earthquake happening if the direction of horizontal tidal force near the fault strike of the earthquake when the earthquake occurs;

地震发生时水平引潮力方位与地震断层面走向接近,可能增加断层面上的剪应力,有利于地震的发生;

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19、

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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20、

The result suggests that: ① The fault is about 390 km long and dips about 90 degree with the greatest left lateral strike slip distance of about 5-6 meters. The result of inversion reflects basically the overall characteristic of the seismic fracture.

结果表明:断层总长390(km)左右,呈直立走滑型,各断裂段左旋走滑量最大为5~6m,反演结果基本反映了地震破裂的总体特征;

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