酒泉盆地群是由两期不同性质、不同世代盆地叠加而成的。
Jiuquan basin group is formed by the stacking of two stage basins with different property and different generation.
酒泉盆地青西凹陷和营尔凹陷是两个富油凹陷，具有较大的勘探潜力。
Qingxi sag and Ying 'er sag are the two oil-enriched sags in Jiuquan basin with large potentials for exploration.
酒泉盆地普遍发育了晚白垩世-始新世的不整面合，该期构造变形在花海地区表现尤为明显。
The late Cretaceous-Eocene unconformity is widely developed in the Jiuquan Basin, especially in Huahai area where the tectonic deformation is very prominent.
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