This paper discusses some features of fractals and deformational decomposition of oblique strike-slip faults in the Jinshajiang plate junction, northwest Yunnan.
从分形和变形分解的角度讨论了滇西北金沙江结合带斜向走滑构造分形和变形分解的某些特征。
Most of the active faults are left-lateral oblique-slip ones and part of them are left-lateral strike-slip ones.
大部分活动断层属左旋斜滑断层，部分活动断层为左旋走滑断层。
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