新生代的

1.Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

断裂带控制了福建地区新生代地壳变形和现今地壳运动的南北差异。

2.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.

民和盆地是发育在中祁连隆起带前武系变质岩基底之上的一个中、新生代山间盆地。