intermont

1.Minhe Basin is a Mesozoic-Cenozoic intermont basin grew on Precambrian metamorphic rock basement in middle Qilian uplift zone.Total thickness of Mesozoic-Cenozoic is about 7000 meters.

民和盆地在中祁连隆起带前寒武系变质岩基底之上的一个中、新生代山间盆地。

2.The basin tectonic model: it is intermont basin during late Jurassic to early Cretaceous, developed into faulted-lacustrine basin in Eogene, and evolved into depression in Neogene and Quaternary.

“盆地”构造模式为：晚侏罗世到白垩末期的山间“盆地”开始、展到早断陷湖盆的、再演化为晚及四地陷阶段。