摘要
萤石是一种战略性非金属矿产,其主要成分是氟化钙,应用广泛。本文以融水苗族自治县(简称融水县)孟公山萤石矿为例,结合矿区地质背景,分析矿床地质特征,揭示矿床成因,明确找矿标志。初步研究认为,根据矿床成因类型,该萤石矿属于中低温热液型萤石矿床。
Fluorite is a strategic non-metallic mineral,mainly composed of calcium fluoride,which is widely used.Taking the Menggongshan Fluorite Deposit in Rongshui Miao Autonomous County(referred to as Rongshui County)as an example,combined with the geological background of the mining area,this paper analyzes the geological characteristics of the deposit,reveals the genesis of the deposit,and clarifies the prospecting indicators.Preliminary research suggests that based on the genetic type of the deposit,the fluorite deposit belongs to a medium-low temperature hydrothermal fluorite deposit.
作者
吴特赟
覃兴涛
WU Teyun;QIN Xingtao(Guangxi Institute of Geophysical Prospecting,Liuzhou 545005,China)
出处
《中国资源综合利用》
2024年第2期89-91,共3页
China Resources Comprehensive Utilization
关键词
孟公山萤石矿
地质特征
矿床成因
找矿标志
融水县
Menggongshan Fluorite Deposit
geological characteristics
deposit genesis
prospecting indicators
Rongshui County