摘要
矿体垂向分带特征及其变化规律，是成矿规律研究的重要内容，其对矿化露头的工业评价与隐伏—半隐伏矿体预测，具重要的指导意义。本文以浙江武义盆地中段萤石矿床为例，从矿脉形态、矿石组构、矿物组合、元素组分、蚀变类型及矿物包裹体等方面，对萤石矿体的垂向分带特征与变化规律进行了研究和总结。
Study on the vertical zonality of ore-body is very important to revealing mineralization low and chalculating orebody.Taking the fluorite ore deposit in the middle part of Wuyi basin as an axample,the present paper mainly studies the vertical zonality of fluorite ore-body from its vein shape,ore texture,mineral assemblage,element component,wall-rock alteration and mineral inclusion,ect.
出处
《西南工学院学报》
CAS
1997年第4期52-59,共8页
Journal of Southwest China Institute of Technology
关键词
萤石矿体
垂向分带
盆地
Fluoreite ore-body
vertical zonality
the middle part of Wuyi basin
