CAJ | 학술논문

黑龙江省小金山金矿赋存在中元古代黑龙江岩群联营岩组背形构造核部，矿体呈北西向等距分布，且受后期剪滑剪切作用形成的破碎带控制。矿体矿化集中，赋存深度较浅，其矿石矿物和金矿物特征由地表向地下逐渐改变并具有明显的氧化富集趋势，拥有裂隙型浅成低温热液矿床的基本特征。
흑룡강성소금산금광부존재중원고대흑룡강암군련영암조배형구조핵부，광체정북서향등거분포，차수후기전활전절작용형성적파쇄대공제。광체광화집중，부존심도교천，기광석광물화금광물특정유지표향지하축점개변병구유명현적양화부집추세，옹유렬극형천성저온열액광상적기본특정。
Heilongjiang province jinshan gold deposit occurred in antiform structure core of mesoproterozoic heilongjiang group lianying assemblage,The orebody equidistant distribution distributed in NW direction,and controlled by the late formation of the fracture zone through the action of shearing. The orebody mineralization concentration,occurrence depth is shallow,the features of ore minerals and gold content gradually change from surface to underground and has obvious oxidation enrichment trendwith the basic characteristics of crevasse epithermal deposit.