摘要
浙江东阳木杓湾萤石矿地处浙中萤石矿矿集区,共有4条矿脉。其矿化与周边岩体及构造关系密切,矿体的赋存形态明显受断裂构造控制,岩浆岩是成矿物质的重要来源,岩浆活动是矿液运移的热动力源。属中低温火山期后热液裂隙充填型萤石矿床。该区域成矿地质条件较好,萤石矿找矿潜力较好。
Mushaowan fluorite mine in Dongyang,Zhejiang province is located in the fluorite ore concentration area in central Zhejiang province,with a total of 4 ore veins.Its mineralization is closely related to the surrounding rock mass and structure,and the occurrence form of ore bodies is clearly controlled by fault structures.Magmatic rocks are an important source of mineral materials,and magmatic activity is the source of thermal power for mineral fluid migration.It belongs to the post volcanic hydrothermal fissure filling type fluorite deposit with medium to low temperature.The geological conditions for mineralization in this region are good,and the potential for fluorite ore exploration is good.
作者
沈徐睿
闫攀攀
SHEN Xu-rui;YAN Pan-pan(Zhejiang Branch of China National Geological Exploration Center of Building Materials Industry,Hangzhou 330022,China)
出处
《中国非金属矿工业导刊》
2023年第5期41-45,共5页
China Non-Metallic Minerals industry
关键词
萤石矿
断裂构造
物质来源
热液裂隙充填型
fluorite deposit
fault structure
material source
hydrothermal fissure filling type
