摘要
在对浙江泰顺县白岩矿区叶腊石矿矿床地质特征描述的基础上,对该区的萤石矿矿床成因进行了分析,认为该区属于火山热液蚀变交代次生石英岩型矿床,其成矿模式为崩塌堆积型,成矿方式以顺层交代蚀变为主,成矿作用与富铝火山碎屑岩、潜火山岩侵入密切相关。
Based on the description of the geological characteristics of pyrophyllite ore deposit white rock in mining area, Taishun, Zhejiang province, the causes of deposit fluorite ore zone is analyzed. It is considered that the re- gion belongs to the volcano hydrothermal alteration and secondary quartz type deposit, and the mineralization model is collapse accumulation. Metallogenic mode is mainly consequent layer replacement; mineralization is closely relat- ed with rich aluminum volcano clastic rock and submarine volcanic intrusive rocks.
出处
《重庆科技学院学报（自然科学版）》
CAS
2016年第1期4-7,45,共5页
Journal of Chongqing University of Science and Technology：Natural Sciences Edition
基金
浙江省地质勘查基金项目"浙江省泰顺县洋溪-外岗地区银多金属矿地质普查"(〔省基〕2012004)
关键词
叶腊石
地质特征
成矿模式
崩塌堆积
pyrophyllite
geological features
metallogenic model
collapse accumulation
