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不久前,在美国亚利桑那州喀斯特塌陷构造中发现了富铀矿床——新型淋积(水成)铀矿床。与这种新类型相近的有乌兹别克斯坦的矿床。中亚和前乌拉尔地区这种类型矿床的前景尚未评估,寻找它们是迫切的课题。 角砾岩筒喀斯特-淋积型富铀矿床是80年代在美国科罗拉多最先发现的一种独特新类型富铀矿床。俄罗斯最近开始重视这种新类型铀矿的寻找工作。文中所述的矿床分布于天山山脉西段的乌兹别克境内。在我国新疆和北方是否存在这种新类型的富铀矿是值得思考和在今后找铀工作中值得注意的问题。
Not long ago, a uranium-rich deposit, a new type of leaching (hydrothermal) uranium deposit, was discovered in the karst subsidence structure of Arizona, USA. Uzbekistan’s deposits are similar to this new type. The prospects for this type of deposit in Central Asia and the former Urals have not yet been evaluated and finding them is a pressing issue. The breccia karst karst-stratum-rich uranium deposit is a unique new type of uranium-rich uranium deposit first discovered in the United States in the 1980s. Russia has recently begun to value the search for new types of uranium deposits. The deposits described in the article are distributed in the territory of Uzbekistan in the western section of the Tianshan Mountains. The existence of this new type of uranium-rich uranium deposits in Xinjiang and northern China is a question that merits consideration and future work in finding uranium.