地震断裂带

对富蕴地震断裂带9处不同地段的平板地质测量结果表明：北部引张段地震断裂带宽约220m，断坎平均高0.4m；

The geological surveying was made with plane table at 9 different sections along Fuyun seismic fault zone , and the result shows : In north part of the seismic fault zone , tension section is as wide as 220 m ; the height of fault scarps averages 0.4 m.

富蕴地震断裂带北部细部结构特征

Detailed structural features in the north of Fuyun earthquake fault zone

福建长乐&诏安地震断裂带闽南段地下水水化学特征

Chemical characteristics of groundwater of Changle & Zhaoan Fault Zone in southern Fujian

中国富蕴地震断裂带的研究

Research on the Fuyun Earthquake Fault Zone in China

地震断裂带上船闸闸位的选择

Selection of Lock Site on Earthquake Fracture Zone

汶川地震断裂带科学钻探（WFSD）项目钻探和测井课题的组织实施与管理

Implementation and Management of Drilling and Logging Engineering of Wenchuan Earthquake Scientific Drilling Project

各类构造应变场的最高值都出现在喜马拉雅构造带与昆仑山地块内（地震断裂带南侧），鲜水河安宁河断裂带次之。

The maximum of strain rate exists in the Himalaya tectonic zone and Kunlun mountain block .

地震断裂带的间距

The distance between seismic faulting belts

用滑动方向拟合法反演富蕴地震断裂带应力场

Stress field in the fuyun , Xinjiang earthquake fracture zone determined by fitting fault slip vector data

热储构造与长期活动的地震断裂带及逆冲推覆构造有关，属传导对流型地热田。

It is a conductive and convective type of geothermal field related to long-active seismic fractures and overthrust structures .

中元古代与新元古代两个不同方向的地震断裂带分别控制着两个时期的盆地边界。

Two seismic fault belts with different directions in Mesoproterozoic and Neoprotertozoic control the basin boundaries of the two stages respectively .

豫北地区处于地震断裂带上，地震活动频繁且剧烈，但有些生土建筑经历了几百年的风雨侵蚀和地震震撼，依然完好无损。

North Henan province is located in the earthquake belt , where earthquakes happen frequently and violently . But some earth buildings are still in perfect condition after thousands of years of wind and rain erosion and earthquakes .

发展中的地震断裂带和震前断裂蠕滑段，作为一个两维导电沟，可以引起邻近区域视电阻率，阻抗相位、维系数的可分辨的变化；

The earthquake fault during the development and the creep portion of fault before earthquake , as a conductive dike , can lead to distinguishable variations of the apparent resistivity phase of impedance , dimensional coefficients in its nearby region ;

震源位置分布表明，北京西北地区存在两条主要的地震活动断裂带。

The distribution of hypocenters shows that there are two major seismic active belts in the northwestern Beijing .

浅层地震在复杂断裂带探测中的应用研究

Application of Shallow Seismic Survey to the Prospecting of Complicated Fault Zone

在30分钟或更短的时间内，他们就能完整地追踪到地球上任何一处导致地震的地壳断裂带。

Within 30 minutes or less , they can trace the entire crustal rupture that produces a quake anywhere in the world .

古浪地震滑坡及其与断裂带的关系

The relation between the Gulang Seismic Landslides and fault belts

指出水库诱发地震易发生在断裂带及其附近；

Some other conclusions are as follows : it is easy to induce earthquake inside and near fault ;

用大地测量资料反演滇西地震预报实验场断裂带的活动段

Inversion of active segments on the fracture belts in experimental field for earthquake prediction in West Yunnan Province ( efepwyp ) by geodetic data

滑坡变形主要受新构造运动、地震活动、断裂破碎带、软弱地层影响，同时受降水、江水冲淘和人类活动作用。

The deformation of the landslide is mainly caused by new tectonic movement , earthquake , fracture zone and influence from soft stratum , and as well as by rainfall , river erosion and human activities .

断裂带自晚更新世晚期以来一直在活动，1842年与1914年发生了2次7.5级地震，并沿断裂带形成地震破裂带。

The faults have been active all the times since late Late Pleistocene . Two earthquakes with magnitude 7.5 occurred on the zone in 1842 and 1914 , and formed rupture belts along the fault zone .

结果表明，在昆仑山口西8.1级地震后东昆仑断裂带南北两侧邻近地区较大地震一般发生在8.1级地震产生的科里奥利力引起的库仑破裂应力增加地区。

The results show that the greater earthquakes on the two sides of eastern Kunlun fault belt after M_S 8.1 earthquake generally take place in the area of increased Coulomb failure stress caused by the Corioli force of 8.1 Kunlun mountain earthquake .

我国是一个地震频发的国家，有十分发育的地震断裂带。

China which is well developed in the earthquake fault zone is an earthquake-prone country .

在地震时断层水平位错分布研究的基础上，结合地震破裂在断裂带内的分布认为沿鲜水河断裂在乾宁南北两侧存在两个长度不大的地震破裂空区。

Based on a study of the horizontal displacement distribution during earthquakes and combined with the co - seismic fractures layout along the fault belt , two different length gaps without seismic fractures have been suggested at north and south sides of Qianning .

为了研究地震的发震机理以及进行地震监测和预报，国土资源部会同科技部和中国地震局组织实施汶川地震断裂带科学钻探工程。

In order to study the mechanism of the earthquake and seismic earthquake monitory and prediction , ministry of land and resources joint China Seismological Bureau to organize the earthquake fault scientific drilling project .