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波多罗什涅恩斯克自然硫露天矿位于苏联德涅斯特河河谷的右岸,它有两个支流通过矿床。矿床的地质构造是从上白垩纪到第四纪的沉积岩,与矿床邻接区域的矿床水文地质条件
The Podolochenyansk natural open-pit mine is located on the right bank of the Transnistria Valley of the Soviet Union, with two tributaries passing through the deposit. The geological structure of the deposit is the sedimentary rock from the Cretaceous to the Quaternary. The hydrogeological conditions of the deposit adjacent to the deposit