Kazkeaerte fault zone is recognized as an important boundary between Pamir and Tianshan Cenozoic Mountain belts in the west of Tarim Basin. It is an active thrust fault and can be divided into three segments from the ...Kazkeaerte fault zone is recognized as an important boundary between Pamir and Tianshan Cenozoic Mountain belts in the west of Tarim Basin. It is an active thrust fault and can be divided into three segments from the west to east: Jilekeroute fault zone, Wuqia earthquake fault zone, Mushi fault zone after geological investigating and mapping along Pamir piedmont. Based on the faulted landform as well as deformation and displacement of young deposit layers, the slip rates of Kazkeaerte fault zone since the late Quaternary are briefly studied. The result shows that the average slip rate of fault is differentiate along different segments.展开更多
文摘Kazkeaerte fault zone is recognized as an important boundary between Pamir and Tianshan Cenozoic Mountain belts in the west of Tarim Basin. It is an active thrust fault and can be divided into three segments from the west to east: Jilekeroute fault zone, Wuqia earthquake fault zone, Mushi fault zone after geological investigating and mapping along Pamir piedmont. Based on the faulted landform as well as deformation and displacement of young deposit layers, the slip rates of Kazkeaerte fault zone since the late Quaternary are briefly studied. The result shows that the average slip rate of fault is differentiate along different segments.
