Abstract—

The kinematic characteristics of faults included in the structure of the active Katun Fault in Gorny Altai have been determined by methods of structural–paragenetic and cataclastic analysis of disjunctives (faults). It is proven that the Katun Fault is a strike-slip fault developing in different areas under transpressive or transtensional conditions. The most recent grabens along the Katun fault were formed under conditions of strike-slip displacements and locally manifested horizontal extension or extension with shear.

中文翻译：

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根据结构和运动学数据的卡吞断层（戈尔尼阿尔泰）的地球动力学

摘要-

戈尔诺阿尔泰地区活动卡吞断层结构中所含断层的运动学特征已通过结构-共生和断层（断层）的碎裂分析方法确定。事实证明，卡吞断裂是在压扭或拉张条件下不同地区发育的走滑断裂。沿卡吞断层的最新地堑是在走滑位移和局部表现为水平延伸或剪切延伸的条件下形成的。