摘要
本文以大溶溪白钨矿床为研究案例,首先阐述了该矿区(床)地质特点,接着详细阐述大溶溪白钨矿床三大形成因素,分别包括热、构造事件、碱(钠)交代作用以及矿床形成因素。希望对于相关从业人员研究地质方面,提供参考与见解的作用。
This article takes the Darongxi scheelite deposit as a case study,first describes the geological characteristics of the deposit (bed),and then details the three major formation factors of the Darongxi scheelite deposit,including thermal,tectonic events,and alkali (sodium) metasomatism.And formation factors.It is hoped that relevant practitioners will provide reference and insights in the study of geology.
作者
陈宇鹏
CHEN Yu-peng(Hunan Institute of Geological Survey,Changsha 410000,China)
出处
《世界有色金属》
2020年第5期119-120,共2页
World Nonferrous Metals
关键词
白钨矿床
地质特征
成矿原因
大溶溪
scheelite deposit
geological characteristics
metallogenic reasons
darongxi