首页|大兴安岭南段莲花山铜银矿床钨矿化的发现及找矿指示意义

大兴安岭南段莲花山铜银矿床钨矿化的发现及找矿指示意义

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大兴安岭成矿带是中国北方重要的铅、锌、银、铜、锡多金属成矿带,内蒙古莲花山矿床是该成矿带南段东坡的一个中型的热液脉型铜银矿床.文章在详细的研究矿床成矿系列和成矿规律的基础上,采用"全位成矿"和"缺位找矿"的思路,提出该矿床存在中高温钨多金属成矿作用的可能,并通过实施找矿勘查示范研究工作,新发现了白钨矿体,确认钨矿化的存在.该发现不仅对莲花山地区新一轮找矿突破战略行动实施提供指导,同时也对大兴安岭南段东坡钨矿潜力评价及成矿规律研究具有重要意义.
Newly discovered tungsten mineralization in Lianhuashan copper-silver deposit from southern Great Xing'an Range and its significance for prospecting
The Great Xing'an Range area is an important lead-zinc-silver-copper-tin polymetallic metallogenic belt in northern of China.The Lianhuashan copper-silver deposit is a typical hydrothermal vein-type medium copper ore deposit on the eastern slope of this belt.Based on the series of metallogenic studies and analysis of metallogenic regularity the authors adopt the ideas of'geospatial mineralization'and'absence prospecting',and believe that there is a possibility of midium-high temperature tungsten mineralization in this area.Through the implementa-tion of demonstration research work on prospecting and exploration,new scheelite was discovered and the tung-sten ore bodies was confirmed.It not only provides important guidance for a new round of strategic action in the Lianhuashan area,but also has important significance for the study of tungsten deposits and metallogenic regulari-ty on the East slope of the southern Great Xing'an Range.

tungsten mineralizationscheeliteLianhuashan copper-silver ore depositeastern slope of the southern Great Xing'an Range

陈郑辉、牛之建、黄宇、王岩、马旭东、尤俊杰、铁朋、范建福、王刚、李嘉宝

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中国地质科学院矿产资源研究所自然资源部成矿作用与资源评价重点实验室 北京 100037

钨成矿 白钨矿 莲花山铜银矿 大兴安岭南段东坡

2024

矿床地质
中国地质学会矿床地质专业委员会 中国地质科学院矿床地质研究所

矿床地质

CSTPCD北大核心
影响因子:2.163
ISSN:0258-7106
年,卷(期):2024.43(6)