浙江省开化县鸡公岩地区萤石矿地质特征及成因探讨  

Geological characteristics and genesis of fluorite deposits in the Jigongyan area,Kaihua County,Zhejiang Province

作　　者：王鹏飞[1] 王富春 赵冰冰 王海宝 WANG Pengfei;WANG Fuchun;ZHAO Bingbing;WANG Haibao(No.327 Unit,Bureau of Geology and Mineral Exploration of Anhui Province,Hefei,Anhui 230011,China;Zhejiang Geological and Mineral Exploration Institute Co.,Ltd.,Hangzhou,Zhejiang 310012,China)

机构地区：[1]安徽省地质矿产勘查局327地质队,安徽合肥230011 [2]浙江省地矿勘察院有限公司,浙江杭州310012

出　　处：《安徽地质》2025年第1期24-27,共4页Geology of Anhui

摘　　要：鸡公岩萤石矿床位于浙西萤石矿带,通过对该矿床矿体特征、矿石特征研究并结合矿区地质成矿背景分析发现,鸡公岩萤石矿床属于碳酸盐岩中的充填交代型脉状、透镜状萤石矿床。区内北东向构造硅化蚀变带是主要的含矿构造,特别是构造带中的萤石矿化、硅化是主要找矿标志。The Jigongyan fluorite deposit is located in the western Zhejiang fluorite ore belt.Based on the geological and ore-forming background of the mineral district,through the study and analysis of the ore body and ore characteristics,it is suggested that the Jigongyan fluorite deposit belongs to the filling metasomatic veined and lenticular fluorite deposit in carbonate rocks.The northeast-trending structural silicification alteration zone in the area is the main ore-bearing structure,especially the fluorite mineralization and silicification in the structural zone are the main prospecting indicators.

关 键 词：鸡公岩萤石矿 矿体特征 矿床成因 找矿标志 

分 类 号：P611[天文地球—矿床学]