白银厂硫化物矿床形成的物理—化学条件及矿床成因  

Metallogenic Physicochemical Conditions and Origin of the Baiyinehang Sulfide Deposit

作　　者：岳东生 

机构地区：[1]中南工业大学

出　　处：《地质与勘探》1991年第3期1-8,共8页Geology and Exploration

摘　　要：通过估算矿区主要热力学参数、硫同位素等,并与日本黑矿进行对比,结合矿床地质条件分析,认为该矿床既具有同生特征,又存在后生性质,应属复生矿床,从而提出一个理想成矿过程.Based on the major thermodynamic parametres and sulfur isotope compositions cstimated for the mining district, and by a comparison with kuroko depcsits in Japan and an analysis of the local geological setting of the deposit, it is considered that the Baiyinchang sulfide depcsit has both syngenetic and epegenetic orlgins. It is a polygenetic deposit. An ideal metallogenic process for the deposits put forward by the author.

关 键 词：硫化物 矿床 成矿作用 成因 

分 类 号：P619.216[天文地球—矿床学]