断层擦痕

柱状节理面上未见断层擦痕或任何移动的证据。

Joint surfaces of the columns do not show slickensides or any evidence of movement .

福州盆地断层擦痕构造解析及其应力场反演

Structural striation analysis and inversion of stress field in Fuzhou Basin

由断层擦痕反演构造应力场的新进展

On recent development in back-analysis of tectonic stress field from fault-slip data

初论断层擦痕和阶步的运用

A preliminary discussion on the application of fault slickensides and fault steps

太原东山矿区节理及断层擦痕的统计分析

The statistics and analysis of joints and fault-strias in Taiyuan Dongshan mine area

根据断层擦痕确定主应力方位的理论和方法

Theory and method in determining the orientation of principal stress by fault striation

用断层擦痕解析断层应力场的方法及计算机处理

Analysis stress fields of fault with slickensides

多期断层擦痕的硬划分：一种目标函数算法

Separation of polyphase fault / slip data : an objective function algorithm based on hard Division

确定古应力场的断层擦痕分析法力学原理

Theoretical basis of a method for the determination of paleotectonic stress field from fault striation analysis

利用共轭节理和断层擦痕反演，对矿区构造应力场进行了定向、定时研究，确定了各期构造应力场。

Inversion of the conjugate joints and striation is used to study orientation and timing of the tectonic stress field and define the stages of the field .

应力估测的准确度取决于断层擦痕数据的误差和不同构造期应力张量之间的相似性。

The accuracy of stress estimation is controlled by random errors in the orientation of fault striations and by similarity between prescribed stress vectors related to different tectonic phases .

柱状节理面上未见断层擦痕或任何移动的证据。我能根据手表背面的擦痕认出那块表是我的。

Joint surfaces of the columns do not show slickensides or any evidence of movement . I can identify that watch as mine by the scratches on the back .

通过野外现场观测，壁上绝大多数断层擦痕均呈东西走向，向东倾斜，倾角10-20°。还可以见到多组破劈理面，走向东西。

It is showed that most of the fault scratches on the walls from east to west , inclined to east , angle 10 ° - 20 ° by the field observations . It is developed multiple sets of cleavage break and NW trenching .

断层面上的断层擦痕与形成断层的主应力有一定的空间几何关系，据断层的产状、性质，断层面上断层擦痕方位，可以定量解析断层应力场。

Slickensides on the fault 's face have geometric relations with main stresses by which fault have been formed , the stress fields of fault can be analyzed quantitatively with attitudes and attributes of fault and orientations of slickensides on fault 's face .