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广西富贺钟地区钨锡多金属矿的成矿规律及控矿因素分析

Metallogenic regularity and ore controlling factors of tungsten tin polymetallic deposits in fuhezhong area,Guangxi
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摘要 在不同的地质作用下每个矿区都有其自身的发展规律,通过研究广西富贺钟地区的钨锡多金属矿成矿规律及控矿因素,根据钨锡多金属矿成矿的时代和空间分布特征,发现了广西富贺钟地区的钨锡多金属矿具有相对成矿的规律。总结出构造、地层和岩浆岩这三种影响因素,均能对广西富贺钟地区的钨锡多金属矿成矿,产生不同程度的控制作用。此次研究更深层次的了解广西富贺钟地区的地质构造,为矿区有效开发提供科学依据。 Under different geological processes,each mining area has its own development law.By studying the metallogenic law and ore controlling factors of tungsten tin polymetallic ore in fuhezhong area,Guangxi,according to the metallogenic age and spatial distribution characteristics of tungsten tin polymetallic ore,it is found that the tungsten tin polymetallic ore in fuhezhong area,Guangxi has a relative metallogenic law.It is concluded that the three influencing factors of structure,stratum and magmatic rock can control the mineralization of tungsten tin polymetallic deposits in fuhezhong area,Guangxi.This study has a deeper understanding of the geological structure of fuhezhong area in Guangxi,and provides a scientific basis for the effective development of the mining area.
作者 路德寄 LU De-ji(271 geological team of Guangxi Zhuang Autonomous Region,Guilin 541000,China)
出处 《世界有色金属》 2021年第18期107-108,共2页 World Nonferrous Metals
关键词 岩浆岩热力作用 钨锡多金属矿 控矿因素分析 成矿规律 地质构造 广西富贺钟地区 magmatic rock thermal action Tungsten tin polymetallic ore Analysis of ore controlling factors Metallogenic regularity Geological structure Fuhezhong area,Guangxi
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