首页|探析湖北随县黑龙潭金矿地质特征、矿床成因与成矿模式

探析湖北随县黑龙潭金矿地质特征、矿床成因与成矿模式

扫码查看
黑龙潭金矿是湖北随县发现的一重要金矿床,其矿化类型主要为蚀变岩型和石英脉型,其中破碎带蚀变岩型又有早期和晚期之分.通过研究了解到,早期破碎带蚀变岩型矿化主要在印支期形成,而成矿的物质来源是有变质地层所提供.同时在燕山期阶段形成了石英脉型矿化,成矿物质来源主要为岩浆岩.而晚期阶段形成的破碎带蚀变岩型矿化,是将上述两期矿化相互叠加而形成.通过这些不难看出,该矿成矿是将上面三种不同时期矿物化相互叠加所形成.该文中主要对黑龙潭金矿的地质特征、矿床成因与成矿模式进行分析和探讨,以期能对同类矿床找矿工作提供一些借鉴和参考.
Exploring the geological characteristics,genesis,and mineralization model of the Heilongtan gold deposit in Suixian County,Hubei Province
The Heilongtan gold deposit is an important gold deposit discovered in Suixian County,Hubei Province.Its mineralization types are mainly altered rock type and quartz vein type,among which the altered rock type in the fractured zone can be divided into early and late stages.Through research,it has been found that early mineralization of altered rock types in fractured zones was mainly formed during the Indosinian period,and the material source of mineralization was provided by metamorphic strata.At the same time,quartz vein type mineralization was formed during the Yanshan period,with the main source of ore-forming materials being magmatic rocks.The fractured zone altered rock type mineralization formed in the late stage is formed by superimposing the above two mineralization periods.It is not difficult to see from these that the mineralization of the mine was formed by superimposing the three different periods of mineralization mentioned above.This article mainly analyzes and discusses the geological characteristics,genesis,and mineralization model of the Heilongtan gold deposit,in order to provide some reference and guidance for the exploration of similar deposits.

Heilongtan Gold MineGeological characteristicsOrigin of mineral depositsMetallogenic model

吴松、许涛、牛志勇、张涛、曾琳

展开 >

湖北省地质局第八地质大队,湖北 襄阳 441000

黑龙潭金矿 地质特征 矿床成因 成矿模式

2024

世界有色金属
有色金属技术经济研究院

世界有色金属

影响因子:0.138
ISSN:1002-5065
年,卷(期):2024.(3)
  • 5