摘要
我国的萤石矿床主要产于火山岩系和硅酸盐岩石中。空间上多与中生代火山岩和酸性侵入岩有关，少部分产于沉积碳酸盐岩地区。成矿方式多为热液脉状充填（交代）式。重点讨论了与花岗岩有关的我国萤石矿床的地质特征及其成矿作用。
In China,fluorite deposit is mainly located in volcanic rocks and silicate rocks,in space,for most parts of it,related to Mesozoic volcanic rocks and acid intrusive rocks.A small part of it occurred in sedimentary carbonate rock.Metallogenic mode is generally vein fill ( metasomatic).In this paper,the geological featureandits mineralization of fluorite deposit related to granite are emphasized.
出处
《地质与勘探》
CAS
CSCD
北大核心
1994年第5期1-6,13,共7页
Geology and Exploration
基金
国家自然科学基金
