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阿尔金走滑断裂带主要由阿尔金主干断层与几条近于平行的左行走滑断层和斜交断层组成，其空间分布规律可用左行走滑简单剪切模型解释。索尔库里盆地是阿尔金断裂带中一个新生代断陷盆地，属于典型松弛分叉型走滑拉分盆地。索尔库里盆地扩张开始于上新世，至今扩张量约为４０ｋｍ，其扩张速率约为０．８ｃｍ／ａ。按相同的位移速率，本文估算了阿尔金主干断层自始新世晚期以来的走滑量，大约为３２０ｋｍ。
The Altun strike-slip fault zone is mainly composed of the main Al-Din fault and several parallel left-lateral strike-slip faults and diagonal faults. The spatial distribution can be explained by the left-slip simple shear model. The Soolcuri Basin is a Cenozoic rift basin in the Altyn Tagh fault zone, belonging to a typical slack-divergent strike-slip basin. The expansion of the Soolcuri basin began in the Pliocene, with an expansion of about 40 km and an expansion rate of about 0.8 cm / a. At the same displacement rate, this paper estimates the strike-slip of the main fault of the Altun since the late Pleistocene, about 320 km.