罗马尼亚层控铅锌矿床产于上元古界中部的碳酸盐建造中,主要分布在东喀尔巴阡山中段的罗德纳(Rodna)山区。已知矿床有伐来亚、布拉兹内(Valea Blaznei)和伐来亚、塞奇(Valea Sacii),此外在东喀尔巴阡山的南段伏斯莱别尼(Voslabeni)和南喀尔巴阡山的弗格拉斯(Fagaras)等地也发现产于相同层位中的铅锌矿化。布拉兹内矿床位于罗马尼亚北部的罗德纳山区,大地构造位置属东喀尔巴阡褶皱带 The Romanian stratabound lead-zinc deposit was produced in carbonate formations in the middle Proterozoic, mainly in the Rodna mountains in the middle of the Eastern Carpathians. The known deposits are Valais, Valea Blaznei and Valais, Valea Sacii, and in the southern section of the Eastern Carpathians Voslabeni and Southern Carr Lead-zinc mineralization in the same horizon was also found in places such as Fagaras in the Carpathians. The Brazione deposit is located in the northern part of Romania Rhodna mountains, the tectonic position of the Eastern Carpathians fold belt