摘要
湖北通城县鸡笼山萤石矿为江南陆块Au-Ag-Pb-Zn-W-Mn-V-萤石成矿带(Ⅲ-70)的一处萤石矿床。通过区域地质背景、矿床地质特征分析等手段对矿床进行研究,查明与成矿有关的地质体、控矿构造、矿化带、蚀变带等的分布和特征,总结成矿条件和成矿规律,探讨该矿床的类型和成因,分析找矿标志,研究认为鸡笼山萤石矿为中低温热液裂隙充填型矿床。为后续研究工作提供一定的借鉴。
The Jilongshan fluorite deposit in Tongcheng County,Hubei Province is a fluorite deposit in the Au-Ag-Pb-Zn-W-Mn-V-fluorite metallogenic belt(Ⅲ-70)of the Jiangnan block.In this paper,the ore deposit is studied by means of regional geological background and the analysis of the geological characteristics of the ore deposit,and the distribution and characteristics of the geological body,ore-controlling structure,mineralization zone,and alteration zone related to mineralization are identified.The authors explore the type and genesis of the deposit,analyze the signs of prospecting,summarize the mineralization conditions and mineralization ore rules.The study believes that the Jilongshan fluorite mine is a medium-low temperature hydrothermal fracture-filled deposit,which provides a certain reference for subsequent research work.
作者
钟温
尹近
王艺霖
陈卓
杜胜
Zhong Wen;Yin Jin;Wang Yilin;Chen Zhuo;Du Sheng(Fourth Geological Brigade,Hubei Geological Bureau,Xianning,Hubei 437100;The geological environmental station in wuhan,hubei province 430034)
出处
《资源环境与工程》
2020年第4期525-528,共4页
Resources Environment & Engineering
基金
湖北省自然资源厅地质勘查基金项目——湖北省通城县鸡笼山矿区萤石矿普查(编号[2019]22)。
关键词
萤石矿
地质特征
矿床成因
通城
湖北
fluorite
geological features
genesis of ore deposits
Tongcheng
Hubei
