According to the study of the mineral evolving, origin analysis etc. , it is considered that the source of minerals etc 认为含矿岩系的物源主要来自海底火山喷发作用形成的黄铁矿化矿源层。
By the time of Yanshanian structural hydrothermal superimposed caused the ore-forming chemical element of the pyritizati经燕山期构造热液的叠加，驱使矿源层中的成矿元素活化、迁移，在有利的构造部位富集成矿。