研究结果认为：鄂尔多斯中生代盆地具有多物源区。
It suggested that there were multiple sediment source areas in the Mesozoic Ordos basin.
利用平衡深度法研究了鄂尔多斯盆地中生代地层的流体剩余压力分布特征。
The distribution of fluid residual pressure of Mesozoic strata in Ordos basin is studied based on the equilibrium depth method.
根据地震、地质等资料，结合野外地质及前人研究成果，对鄂尔多斯盆地北部中生代晚期以来后期改造特征进行了研究。
The structural characteristic of the North Ordos basin in the Late Mesozoic and the Cenozoic is researched with the data of seismic, geological and former achievements.
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