摘要
本文主要通过包裹体岩相学特征、测温及成分分析等几个方面,对锦屏县平秋金矿含金石英脉的包裹体进行研究。结果显示成矿流体主要表现为具岩浆热液性质的中低温、低盐度、低密度的热液。
Gold inclusions in quartz vein in Pingqiu,Jinping are researched in the paper in the aspects of petro-graphic features,thermometric and component analysis of inclusions.The result shows that ore-forming fluids in this area are mainly hydrotherm with medium-low temperature,low salinity and low density.
出处
《贵州地质》
2011年第3期194-199,236,共7页
Guizhou Geology
基金
贵州省地矿局重大科研项目[黔地矿科(2009)11号]资助
关键词
包裹体
石英脉型金矿
平秋
inclusions
gold in quartz vein
Pingqiu
