摘要
荒沟山金矿床明显受构造控制，矿体多呈复杂的脉状充填于大理岩开放空间中，成矿为多期次、热液角砾岩化多期次的特点，成矿流体以大气水为主，具有浅成、低温、低盐度和近中性的成矿环境，属于浅成低温热液成因金矿床。
It is quite obvious that the Huanggoushan gold deposit is controlled by the structures,and the ore bodies as the complicated veins are mostly filled in the open-spaces of marble,showing the metallogenic characteristics of multiple stages with multiple hydrothermal brec-ciation. The ore-forming fluid is mainly meteorological water,having epithermal,low salini-ty near intermediate mineralizing setting and belonging to epithermal hydrothermal deposit.
出处
《吉林地质》
1995年第3期1-16,共16页
Jilin Geology
关键词
矿床特征
地球化学
成矿作用
金矿床
成因
Characteristics of ore deposit Geochemistry Ore-forming process Ori-gin of ore deposit The Huanggoushan gold deposit
