摘要
本文以浙东南遂昌湖山萤石矿田为例，对此类浅成低温热液矿床成矿构造地球化学特征，进行了初步研究与探讨；进一步揭示了萤石矿成矿物质组分的分配、迁移、分散、富集特征与控矿构造之间的内在联系。
Ore formation has an intimate relationship with fault structures.Study on tectonogeochemical characteristics of ore components has become one of the most popular topics of geoscientists.Taking the Suichang Hushan fluorite ore field as an example,the present paper mainly studies the tectonogeochemical characteristies of epithermal doposits of this kind,and further discusses the bearing of ore control faults on the distribution,transportation,dispersion and enrichment of fluorite ore components.
出处
《矿物岩石》
CAS
CSCD
北大核心
1998年第S1期50-55,共6页
Mineralogy and Petrology
关键词
控矿断裂
构造地球化学
萤石矿成矿
遂昌湖山矿田
ore control fault tectonogeochemistry fluorite ore formation the Suichang Hushan ore field
