The Kazikearte fault is a strong motion zone of dip slip type along the north-western edge of the Qing-Zang plateau.
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。
2
To the north of the Kunlun fault is the Qinghai Plateau, which is a basin and range area with contiguous gravity highs and gravity lows.
青海高原位于昆仑山脉以北，是重力高和重力低毗连出现的盆山结构。
3
This plateau possesses the following excellent conditions for sabfication; 1, the enclosed inland lake basin controlled by the subsidence of the fault;