The maximum cumulative strike-slip displacement of the Altyn Tagh Fault-900 km?
阿尔金断裂带最大累积走滑位移量——900km?。
The Altyn Tagh fault zone is an important strike-slip fault zone in northwestern China.
阿尔金断裂带是西北地区一条重要的走滑断裂带。
The west edge of the basin overlapped on bedrock, there is not any substantive relation with the Altyn Tagh fault.
盆地的西部边缘超覆在基岩之上，不受断裂控制。
This paper concludes that the Altyn Tagh Fault, in a form of "arborization", disappeared in the Jiuxi Basin and Huahai Basin.
通过研究得出，阿尔金断裂带以“树枝状”的型式消失在酒西盆地和花海盆地内。
This paper concludes that the Altyn Tagh Fault, in a form of "arborization", disappeared in the Jiuxi Basin and Huahai Basin.
通过研究得出，阿尔金断裂带以“树枝状”的型式消失在酒西盆地和花海盆地内。
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