摘要
通过对广东小家岭银金多金属矿地区的成矿地质背景和矿体地质特征的研究,阐明了矿体特征,分析了矿床的物质来源、矿化蚀变和矿石矿物成分特征,分析研究认为该区矿床成因是历经构造作用、热液蚀变到富集成矿的过程。
Based on the study of metallogenic geological setting and geological characteristics of ore body in Xiaojialing Ag-Au polymetallic ore area,Guangdong Province,this paper clarifies the ore body characteristics,analyzes the material source,mineralization alteration and ore mineral composition characteristics of the deposit,and gets the conclusion that the formation cause of the deposit in this area is a process from tectonism,hydrothermal alteration to enrichment mineralization.
作者
罗君
LUO Jun(No.5 Geological Team of Geological Bureau of Guangdong Province,Zhaoqing 526020,China)
出处
《矿业工程》
CAS
2021年第2期11-14,共4页
Mining Engineering
关键词
银金多金属矿
地质特征
矿床成因
Ag-Au polymetallic deposit
geological characteristics
depoisit formation cause
