热水矿区断裂构造与金矿化特征的关系  

The Relationship Between Mining Fault Structure in Reshui and Characteristics of Gold Mineralization

作　　者：林长慧 

机构地区：[1]广东省有色金属地质局九三八队,广东惠州516023

出　　处：《甘肃冶金》2017年第4期36-41,共6页Gansu Metallurgy

摘　　要：在热水矿区,不同级别和序次的构造表现出分级控矿的特征,矿体的位置、形态、产状则取决于北西向断裂、南北向断裂和近东西向断裂。分析金矿化与构造演化相关的矿化类型、矿化形式、成矿阶段、富集特点、蚀变特征等,表明了北西向断裂与金矿化比较密切。In Reshui area, construction of different levels and orders shows the different characteristics of classification con- trol.The location, shape and occurrence of ore bodies depend on northwest trending fault and southwest trending fault , arid near eastwest fault.Analyzing the similar Mineralization type, Mineralization formation, Metallogenic stage, enrichment char- acteristics, alteration characteristics of gold mineralization and tectonic evolution shows the relevant relationship between northwest trending fault and gold mineralization.

关 键 词：热水矿区 控矿构造 矿化特征 断裂构造 

分 类 号：P612[天文地球—矿床学] P618.51[天文地球—地质学]