札达盆地与高喜马拉雅断块隆起存在盆&山耦合关系，藏南谷地基底断块的翘板式运动是形成盆地的主要控制因素。
There are a basin range coupling between the Zanda basin and the high Himalaya region . The seesaw type tectonic movement of the basement fault block in the south of the plateau is the primary control factor for the basin forming .
藏南谷地