活动构造带

川滇块体北东边界活动构造带的构造转换与变形分解作用

Structural Transformation and Strain Partitioning along the Northeast Boundary Belt of the Sichuan-Yunnan Block

地震震中主要分布于活动构造带的边界断裂附近。

The epicentres are mainly located near the boundary faults along the active tectonic belts .

可可西里&东昆仑活动构造带强震活动研究

Strong earthquake activities in kekexili & east Kunlun Mountains active fault zone , Northwest China

凉山活动构造带晚新生代变形特征与位移规模

Deformation characteristics and displacement amount of the Liangshan active fault zone in Late Cenozoic Era

初析天水地区南北向活动构造带及其与地震的关系

Elementary analysis about the active South-North tectonic zone in Tianshui region ahd the relation between the zone and earthquakes

深入研究三马坊水温前兆异常特征与活动构造带间的关系，可能是突破该地区地震短临预报的有效途径。

It is significant to study the relationship between Sanmafang water temperature anomaly and the earthquakes in active tectonic zone .

这次地震的发震构造为尼木南北向活动构造带中的一条北北东向断裂。

The generating earthquake structure direction is a north-northeast which belongs to the active structural zone in the north-south in the Nimu .

兰州地区发育了北西西向和北北西向两组主导性活动构造带。

Lanzhou area developed two groups of dominant active tectonics : one group is NWW direction , another one is NNW direction .

本文分析了铁路经过的当雄-羊八井活动构造带的基本特征，讨论了其对铁路可能产生的严重影响。

In this paper , the author analyzed the basic characteristics of the Damxung-Yangbajain active tectonic zone and discusses the probable geological hazards .

张家口-渤海构造带是华北乃至我国东部地区一条非常重要的北西向活动构造带，也是我国著名的强震集中带。

The Zhangjiakou-Bohai tectonic zone is an important north-west tectonic zone in the North China and even in eastern China . It is also a famous strong earthquake zone .

另外，在强震震中沿活动构造带或沿块体边缘迁移时，迁移时间也有相隔5个月的现象。

In addition , when the epicenters of strong earthquakes migrated along the active tectonic zone or the edge of a block , a 5-month separation for the the migration was also observed .

长线工程场地一般都得穿经活动构造带，因而活动构造研究在该类场地的地震安全性评价工作中尤为重要。

Long line engineering sites usually have to pass through some active tectonics , so that the research of active tectonics is of great importance to seismic safety evaluation of this sort of site .

新的野外调查研究结果表明，六盘山东麓断裂是一条第四纪以来的活动逆断裂构造带。

New results of field investigations show that the eastern Liupanshan piedmond fault is an active reverse fault zone since late Quaternary .

矿床的主要控矿条件是：①矿体产于多次活动的断裂构造带之中；

The major ore-controlling conditions for the ore deposit are as follows : ① orebodies are present in and strictly controlled by the structural zone which has experienced repeated activities ;

由于地幔浮力和造山热的作用，一些山带具有高的海拔和薄而热的地壳，属于具有长期活动性的构造带。

As a result of mantle buoyancy and orogenic heat , a number of mountain belts have high elevation and thin and hot crust , and thus become long-lived active mobile belts .

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。

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.

结合地质构造分析研究，表明该构造带是一多期活动的重要构造带，具有伸展走滑的性质；

On the basis of the above study , combined with the tectonic analysis , the authors think that this tectonic belt is characterized by multi-stage activity and shows the extensional strike-slip characters .

盆地南北向张性断裂带是板块超碰撞期活动最强烈的构造带。

The north south trending tensional fault zone in the basin was the most active tectonic belt during the plate over collision .

矿泉水受构造断裂、活动断裂构造蚀变带及褶皱控制明显，或沿深大断裂深部循环，或沿褶皱层间裂隙、构造裂隙向倾伏方向富集、运移、承压出露。

The natural mineral springs are obviously controlled by fault , fold and structural alteration zone and the water circulates along deep fracture zone and moves along interlayer faults or tectonic fissures , finally , wells out under an artesian condition .

活动地块是被形成于晚新生代、晚第四纪（100～120kaB.P.）至现今强烈活动的构造带所分割和围限、具有相对统一运动方式的地质单元。

The active blocks are geological elements with similar motion modes , which were formed in Late Cenozoic and cut and enclosed by strong active tectonic belts from Late Quaternary to present-day .

根据晚新生代以来沉积建造、沉积环境、岩浆活动、岸线变迁、地貌及现代地震等资料判断，太仓&奉贤北西向断裂带是上海及邻近地区一条重要的活动性断裂构造带。

According to the sedimentary formation , sedimentary environment , magmatic activities , changes of shoreline , geomorphology and modern earthquakes etc. since the late Neozoic , the Nw & fault zone of Taicang-Fengxian is an important active fracture in Shanghai and its neighbourhood .