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阐述了中新生代山间坳陷盆地——新疆和什托洛盖盆地的水文地质、水文地球化学特征,认为该盆地具有完整独立的地下水补给、径流、排泄系统,为正向水文地质、水文地球化学分带的渗入型盆地.盆地经历了长期的水文地质淋滤作用,存在含铀含氧水不断渗入补给,认为在地下水交替缓慢的水动力区有利于形成砂岩型铀矿,分析了盆地的铀成矿条件,并优选出铀成矿的有利地段.
The hydrogeological and hydrogeochemical characteristics of the Mesozoic-Cenozoic mountain depression basin-Xinjiang and Shittoruai Basin are described. It is believed that the basin has a complete and independent groundwater recharge, runoff and drainage system. It is characterized by positive hydrogeology, hydrology Geochemical zoning intrusive basin.The basin experienced long-term hydrogeological leaching, there uranium-containing water continued to infiltrate the supply, that alternating groundwater hydrodynamics is conducive to the formation of sandstone-type uranium deposits, the basin Of the uranium metallogenic conditions, and the preferred uranium metallogenic favorable location.