The results show a depression trending E-W developed between the old Alabasitao mountain and the Kunlun mountain with the depocenter in the old Altyn tagh region.

• 结果表明，早、中侏罗世在古阿拉巴斯套山与古昆仑山之间发育一个大的近东西向展布的沉积坳陷（古泛茫崖坳陷）。