Turpan—Hami basin is an important insitu leachable sandstone type uranium deposits metallogenic basin. Based on synthetical geologic investigations, boreholes evaluation, and data analyse, Aiding lake slope, Danan lake area, Shaer lake area, Shandaoling area and Takequan tectonic belt are affirmed as uranium metallogenic prospective areas of insitu leachable sandstone type uranium deposits. Because of specialities and differentialities of tectonization, in these uranium metallogenic prospective areas, 4 structural styles, i.e. fault—overlying folding style, fault—uplift style, fault—terrace style and monocline—fault style（monoclinal strata） can be distingguished. Having synthetically analyzed, writers conclude that the Aiding lake slope, Danan lake area have the best metallogenic structural conditions for sandstone type uranium deposit; the Shandaoling area and Shaer lake area, although have partial stable structural clinoform，but for tectonization influences，have less potential for oreforming of insitu leachable sandstone type uranium deposits.