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在滨贝加尔西北部的前寒武纪杂岩中赋存有两种含矿建造类型的层状矿床:①产于碳酸盐岩中的含萤石和重晶石的铅锌矿床(塔博尔、卢戈、希宾等);②黄铁矿一多金属矿床(霍洛德尼克)。研究矿床的多元和多种成因首先必须确定容矿建造形成时的含矿构造发育情况,阐明矿床古构造的位置,这两种类型矿床的现代构造格架是综合了原始沉积构造及后来迭加其上的较晚期多次的变形确定的,解释原始容矿构造变化的特征是研究控制矿床构造的又一项重要任务。滨贝加尔西北部隶属于贝加尔地槽区,西伯利亚地台的南缘。在萨洛普著作
There are two types of ore-bearing stratiform deposits in the Precambrian complex in the northwestern part of Binbaikal: ① Pb-Zn bearing fluorite and barite beds in carbonate rocks (Tabor , Lugo, Hibbing, etc.) ② pyrite-polymetallic deposits (Holodnik). To study the multiple and multi-genesis of ore deposits, we must first determine the development of ore-bearing structures during the formation of the ore-bearing construction and elucidate the paleotectonic location of the ore deposits. The modern tectonic framework of these two types of deposits integrates the original sedimentary structures and the subsequent superposition The later deformation of the last several times, to explain the characteristics of the original ore-bearing structural changes is to study and control the structure of the deposit is another important task. The northwestern part of Bin Baikal belongs to the Baikal Trough area, the southern edge of Siberia platform. Works on Salop