昆仑褶皱系
昆仑褶皱系-
结果表明：在塔里木地台及西伯利亚地台边缘，Q0值较高，为300~450；而在南部的西昆仑褶皱系、松潘甘孜褶皱系，Q0呈现出低值，在150~250的范围内变化；
The results indicate that Q 0 was higher ( 300 ~ 450 ) in the Tarim platform and the edges of Siberian platform , while Q 0 was lower ( 150 ~ 250 ) in the southern regions as west Kunlun fold system and Songpan Ganzi fold system .
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新疆地区有五个大地构造单元，它们是阿尔泰褶皱系、准噶尔褶皱系、天山褶皱系，塔里木地台和西昆仑褶皱系。
There are five tectonic units in this region , i.e.Altay fold system , Jungar fold system , Tianshan fold system , Tarim Platform , and western Kunlun fold system .