萨迪莫拉矿床是在里海盆地地区对钾盐进行有计划的勘探工作而于1963年发现的。在1963—1972年间,在Satimla盐丘构造区打了486口勘探井,其中有74口构造井,深度达1000—1200米。盐体中的勘探井加深25—30米。 根据地质勘探工作结果,可以确定 The Diamora deposit was discovered in 1963 on a planned exploration of potash in the Caspian Basin. Between 1963 and 1972, 486 exploration wells were drilled in the Satimla salt structure area, of which 74 were constructed well depths of 1,000-1200 meters. Exploration wells in salt bodies deepen 25-30 meters. According to the geological exploration work results, can be determined