文章摘要
唐代文,韦俊杰,刘松兵,赵志坚,谭梦林,邹利群,肖亮明.锡矿山锑矿田北倾伏端重要找矿突破及地质特征新认识[J].矿产勘查,2021,12(8):1750-1757
锡矿山锑矿田北倾伏端重要找矿突破及地质特征新认识
Important prospecting breakthrough and new understanding of geological characteristics in North dipping end of Xikuangshan antimony ore.eld
投稿时间:2021-01-06  
DOI:
中文关键词: 锡矿山  北倾伏端  老矿山  Ⅳ号矿体  地质特征
英文关键词: Xikuangshan  north dip tip  Laokuangshan  ore body Ⅳ  geological characteristics
基金项目:本文受中国地质调查局“湖南省冷水江市锡矿山锑矿接替资源勘查”项目(12120113083200)和湖南省矿业权价款地质勘查项目“湖南省冷水江市锡矿山锑矿田飞水岩矿区边深部锑矿普查”(20150326)联合资助。
作者单位
唐代文 湖南省有色地质勘查局二总队湖南湘潭 411101 
韦俊杰 湖南省有色地质勘查局二总队湖南湘潭 411101 
刘松兵 湖南省有色地质勘查局二总队湖南湘潭 411101 
赵志坚 湖南省有色地质勘查局二总队湖南湘潭 411101 
谭梦林 湖南省有色地质勘查局二总队湖南湘潭 411101 
邹利群 锡矿山闪星锑业有限责任公司湖南冷水江 417500 
肖亮明 锡矿山闪星锑业有限责任公司湖南冷水江 417500 
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中文摘要:
      锡矿山锑矿田是世界级的超大型矿床,由北往南,由稻草湾、老矿山、童家院、物华、飞水岩五个矿床组成。以往工作的重点放在飞水岩矿床,对矿田北倾伏端Ⅳ号矿体未开展系统研究工作,导致对含矿层位及矿体屏蔽层的认识不足。近年施工的钻孔在北倾伏端——老矿山矿床取得重要突破,首次揭露了赋存于佘田桥组龙口冲砂岩段与棋梓桥组灰岩层间破碎带内富、厚的Ⅳ号工业矿体。通过详细的钻探地质编录、镜下鉴定、岩矿测试等工作,对Ⅳ号矿体含矿层位沉积相及矿体顶部的屏蔽层开展研究,对主要控矿构造产出特征及控矿关系展开讨论,表明Ⅳ号矿体严格受层位及断裂控制,对明确矿田北倾伏端下一步找矿方向有重要指导意义。
英文摘要:
      Xikuangshan antimony ore field is a world-class super large deposit, from north to south, by Daocaowan, Laokuangshan, Tongjiayuan, Wuhua, Feishuiyan five deposits. Previous work focused on the Feishuiyan deposit, but no systematic research was carried out on the Ⅳ orebody at the north dip tip of the ore.eld, resulting in insu.cient understanding of ore-bearing horizon and orebody shielding layer. Drilling in recent years has made an important breakthrough in the Laokuangshan deposit at the north dip tip, and revealed for the .rst time the rich and thick industrial orebody Ⅳ occurring in the broken zone between the Longkouchong sandstone member of Shetianqiao Formation and the Qiziqiao limestone layer. Through detailed drilling geological record, microscopic identi.cation, testing, etc, to Ⅳ ore body of ore-bearing bed, the orebody at the top of the shielding layer and sedimentary facies research, the main ore-controlling structure output characteristics and the controlling relationship discussion, suggests Ⅳ ore bodies are strictly controlled by the strata and fracture, it has important guiding signi.cance to de.ne the prospecting direction of the north dip tip of ore .eld.
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