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马林诺夫斯基铀矿床产于西伯利亚地台南西部的中新生代陆相沉积盆地。该盆地为地台型的大型沉积盆地，铀矿床产于盆地东南缘，铀矿化受切割古生代基底的古河谷控制。文中概述了该矿床的地质与矿化特征。
The Malinowski uranium deposit was produced in the Mesozoic-Cenozoic continental depositional basin in the western part of Siberia. The basin is a terrace-type large-scale sedimentary basin. Uranium deposits are produced on the southeast margin of the basin and uranium mineralization is controlled by ancient valleys of the cut Paleozoic basement. The paper summarizes the geological and mineralization characteristics of this deposit.