自流水盆地

早白垩世形成的鄂尔多斯东西不对称湖盆结构既控制当时含水层的发育和分布，又是现今自流水盆地结构形成的基础。

Asymmetrical lake-basin structure of Ordos basin in EW way , formed in early Cretaceous , not only control development and distribution of main water-bearing bed , but also is the basis of structure forming of artesian basin nowadays .

鄂尔多斯白垩系自流水盆地水文地质特征与岩相古地理

Hydrogeological Characteristics and Lithofacies Palaeogeography of Cretaceous Artesian Basin , Ordos

鄂尔多斯盆地是一个巨大的开启型自流水盆地。白垩系是其中含水最丰富的岩体，约有7.57亿m3／a天然水资源。

The Ordos Basin is a huge artesian one , where Cretaceous System is richest in water , bearing about 757 million m3 / a of water resources .

鄂尔多斯早白垩世自流水盆地沉积特征岩性分布与盆地演化

Sedimentary character , lithological distribution and evolvement pattern of cretaceous Artesian Basin in Ordos , China

通过对鄂尔多斯白垩系自流水盆地获得的钻孔地质分层资料及地质剖面图等地层结构的信息进行分析，认识地质结构，通过一定的技术手段，重现地质实体三维结构，建立可视化地质模型。

Analyze the structural information , such as the borehole and the geological profile ; build the three-dimensional geological structural model .