卡兹克阿尔特断裂是青藏高原西北边缘的一条倾滑型性质的强震发生带。
The Kazikearte fault is a strong motion zone of dip slip type along the north-western edge of the Qing-Zang plateau.
火山活动为新构造活动的响应，受控于青藏高原隆升过程中产生的走滑断裂。
Volcanic activities were the response to the neotectonic activities and were controlled by strike-slip faults produced during the uplift of the Qinghai-Tibet Plateau.
长期的构造活动形成了一系列规模宏大的活动断裂，这些不同性质的断裂又将高原地壳切割成大小不同、形状各异的活动地块。
The long-term tectonic activity formed a series of great scale active faults that divided plateau crust into blocks in different size and shape.
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