摘要
黎川县坊坪某矿属硅酸盐岩石中的热液充填型脉状萤石矿床。成矿构造为北东向断裂构造,成矿热液来自于深部辉绿玢岩脉侵入时形成的热液。本文通过对矿床的地质特征、矿床成因的分析,指出了本地区某矿的类型、规模、开采特性、找矿方向及标志。
A Fangping mine in Lichuan County belongs to hydrothermal filling vein fluorite deposit in silicate rocks.The ore-forming structure is a NE trending fault structure,and the ore-forming hydrothermal solution comes from the intrusion of deep diabase porphyrite vein.Based on the analysis of the geological characteristics and genesis of the deposit,this paper points out the type,scale,mining characteristics,prospecting direction and marks of a certain mine in this area.
作者
汪怀国
WANG Huai-guo(Energy Geological Survey Institute of 261 brigade,Jiangxi Nuclear Industry Geological Bureau,Nanchang 330100,China)
出处
《世界有色金属》
2020年第17期70-71,共2页
World Nonferrous Metals
关键词
某矿
热液
构造
矿床成因
找矿标志及方向
a deposit
hydrothermal solution
structure
ore genesis
prospecting criteria and direction