transform fault

TRANSFORM FAULT AND ITS GEOLOGICAL SIGNIFICANCE ——A study on the Altyn Tagh transform fault;

转换断层及其地质意义——以阿尔金转换断层为例

The strike slip fault can be divided into three different levels corresponding to the different scales of petroleum exploration targets, such as transform fault dominated the basin forming, transfer fault controlled the play, and tear fault charged the trap.

走滑构造体系盆山耦合常由于走滑断层弯曲所产生 ,结合油气勘探中盆地—区带—圈闭 3个层次 ,相应地划分为 3类走滑断层 :(1)转换断层为控盆断层 ;(2 )转移断层为控带断层 ;(3)撕裂断层为控藏断层。

In mid-late Paleozoic, it was a great intracontinental transform fault of right-lateral slip, and in Mesozoic and Neozoic it was revived in different parts.

在卫星遥感图像宏观解译和野外调查基础上,充分参考了近年来的区域地质调查和前人研究成果,分析了阿尔金山各边界断裂特征,结果表明南缘断裂形成于元古宙,早古生代中晚期是一条具有右行走滑性质的巨型陆内转换断层,中新生代分段差异复活;西北缘断裂系形成较晚,中新生代以来发生强烈的左行走滑,应属于亚洲共轭滑移系的组成部分;红柳沟-拉配泉断裂属于塔里木地块中央构造带系统,是一条蛇绿构造混杂带,早古生代属于陆缘或陆间裂谷。

Based on the transfer theory of fault, 11 fault transfer zones are identified, which belong to 4 types (collateral synthetic, collateral convergent, overlapping, and approaching transfer styles).

应用断层转换带的理论,识别出东辛油田的11个断层转换带,分为4种类型(平行同向断层型,平行对向断层型,叠覆断层型,趋近断层型)。

Tan-Lu is an intra-continental transform fault along with the continental collision between North China and Yangtze plate.

郯庐断裂带是中生代华北与扬子板块的碰撞造山带的陆内转换断层,大规模左行韧性剪切位移牵引胶北太古宙穹隆(栖霞复背斜)逆时针旋扭隆升,并且形成三山岛-仓上、焦家-黄县和招远-平度(破头青)等弧形右行剪切带和混合花岗岩。

In recent years,a new type of fault that cuts nearly vertically through the entire crust into the mantle is known from geophysical investigations and is named vertical transform fault by the authors.

近些年来，地震测深和重力测量方法揭示出大陆岩石圈内存在一组穿透地壳并延深到上地幔的高角度断裂，经厘定，被命名为垂直转换断层（ｖｅｒｔｉｃａｌｔｒａｎｓ－ｆｏｒｍｆａｕｌｔ）。

right-lateral ridge-arc transform fault

右旋脊-弧转换断层

arc arc transform fault

岛弧?岛弧转换断层

ridge-arc transform fault

海岭-岛弧转换断层

right-lateral arc-arc transform fault

右旋弧-弧转换断层

Through long terms of tectonic evolutions, it changed into a transform fault in the Cenozoic Era.

经长期构造演化于新生代转变为转换断层。

Transform fault earthquakes are most noticeable where the fault passes through a continent, rather than the sea floor.

转换断层地震是最值得注意的，在那里断层是通过陆地，而不是海底。

VERTICAL TRANSFORM FAULT A NEW TYPE OF FAULT IN HIGH ASIA AND ITS SIGNIFICANCE FOR GEODYNAMICS

高亚洲区内一种新类型的断层——垂直转换断层及其地球动力学意义

The plates are bounded by an interconnected network of ridges, transform faults, and trenches.

板块以一个由洋中脊、转换断层和海沟相互连接形成的网络为界。

Shallower, but equally severe earthquakes occur along transform faults where one plate is dragged sideways against another.

较浅的，但同样强烈的地震沿转换断层发生，在那里一个板块被向与另一个板块相反的一侧拖拉。

Linkages of Normal Faults and Transfer Zones in the Liaodongwan Depression,Offshore Bohai Bay Basin

渤海海域辽东湾坳陷正断层联接及其转换带特征

hand off-auto switch

手动-断开-自动转换开关

On the effects of the transfer story height on the twin-tower transfer structure with base block

转换层高度对大底盘双塔带转换层结构的影响

Study on Conversion from Surface-Layer Structure of a Chinese Sentence to Its Deep-Layer Structure

从中文表层句到深层结构的转换研究

Seismic Optimum Design for High-rise Building with Girder Transfer Floor;

带梁式转换层高层建筑抗震优化设计

The Construction Technology Research on High-rise Building with Thick Transfer Floor;

高层建筑厚板转换层的施工技术研究

Multi-tower High Building Structure with a Transfer;

多塔带转换层高层结构抗震性能研究

Analysis to the Limit Range of Side Shift Ratio for Transfer Story Structure;

转换层层间侧移角比界限值范围分析

Analysis of High-Rise Building Transfer Thick Slab;

高层建筑厚板结构转换层的内力分析