摘要
实际地质资料和模拟实验都表明 ,在滥木厂铊矿床中存在成矿元素分异和矿物分带现象。造成这种现象的原因是由区域热事件、成矿元素的地球化学行为、有机质的作用。
Geological data and experiment all demonstrat that: it has ore-forming elements separating and mineral zoning.This result is made by regional hot-event; geochemical action of ore-forming elements; organism; metallogenesis; and stagnant time of ore-forming fluid flowing through crack system.
出处
《贵州教育学院学报》
2004年第4期54-57,共4页
Journal of Guizhou Educational College(Social Science Edition)
关键词
矿物分带
元素分异
成矿流体
铊矿床
滥木厂
mineral zoning
elements separating
ore-forming fluid
thallium deposit
system of fluid
Guizhou
