摘要
利用山门银矿包裹体的测试数据,在分析研究其成矿热液理化特征的基础上,得出山门银矿床是在浅成低温、低压环境中,由以贫硫、低盐度,酸性大气降水为主的含矿热液,在低还原条件下形成的结论。
Based upon the testing results of the inclusions and through the study on hydrothermal physical-chemical characteristics, a conclusion on the formation ore-bearing hydrothermal fluids S-poor, low saltness, acid precipitated water dominated by the lower reducicing condition, with hypabyssal lower temperature-pressure was drawn from the Shanmen silver deposit, Jilin province.
出处
《吉林地质》
1992年第1期53-59,共7页
Jilin Geology
关键词
银矿
成矿
物理化学条件
Minerogenetic physical-chemical condition Mineral inclusion Minerogenetic hydrothermal fluid Plysical-chemical parameter value Silver precipitation mechanism
