Hefei basin, closely near to the west of Tan-lu fault, is a Mes-Cenozoic compound superposition basin. Its generation and evolution have a close relationship with the activities of Tan-lu fault zone.
合肥盆地是紧邻郯庐断裂带苏皖段西侧发育的一典型的中新生代复合叠加盆地，合肥盆地的成生、演化与郯庐断裂带的活动有着密切的联系。
Ordos basin is a polycyclic superposition basin that is formed in an earlier geological history and has experienced a longer evolution.
鄂尔多斯盆地是一个多旋回叠合型盆地，其形成历史早、演化时间长。
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