一些盐壳覆盖的干涸湖泊 （西班牙语：salars） 占据了普纳地区主要逆冲断层之间的地势低洼地（盆地）。

Several salt-crusted dry lakes (known as salarsin Spanish) occupy the basins between major thrust faults in the Puna.

youdao

北东东向和北北东向断层带形成较早且长期活动，控制了盆地的形成；

NEE and NNE fault belts controlling the formation of the basin had developed well and early and had acted for a long time.

youdao

盆地沿走向的变化由传递断层加以调整，并被间隔为不同的块段。

Variations along the strike of-extensional basin are accommodated by transfer faults which compartmentalize the basin into different segments.

youdao