strike-slip fault

In this paper, a method is proposed such that the strike, dip, dipping direction and fracture length of a fault plane can be determined using of isoseismal lines.

本文提出了利用等震线测定地震断层面的走向、倾向、倾角和破裂长度等震源参数的宏观方法。

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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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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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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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The conditons for groundwater are the tectonic unit, the strike, distance, position of the fault near wells, the depth of the well and lithologic property and groundwater type of the aquifer.

影响地下水类观测井映震能力的主要条件是构造单元、邻近断裂的走向、距离、部位、井深、含水层的地层岩性与地下水类型；

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The ore controlling structure is mainly NNE strike fault with double constructional surface.

控矿构造主要为NNE向断裂，具明显的双重结构面特征，金矿体严格受其控制。

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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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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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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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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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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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The gold deposit is controlled by NW strike fault, ore bodies all occurred in the near EW strike and NW strike fault and had same occurrence with fault, it is the classic tectonic belt altered rock type gold deposit.

总体受NW向断裂控制，金矿体无一例外地赋存于近EW，NW向断裂中，且与断裂产状一致，是典型的构造带蚀变岩型金矿床。

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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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Based on the Coulomb-Navier strength theory, the present author proposes in this paper the concept of fault with critical strike and discusses the physical mechanism forming the blocked segment of fault.

根据库伦-纳维强度理论，本文提出了临界走向断层的概念，探讨了形成闭锁段的物理机制。

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