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甘肃北山东小泉金矿床类型及成矿构造模式

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东小泉金矿床位于中国西北地区重要的金属矿床富集区甘肃北山区,是近年新发现的含金石英脉型和破碎带蚀变岩型组合型矿床.通过分析该矿床地质特征、控矿构造期次、金矿体与构造空间关系,总结该区的成矿构造模式.结果表明,该区的石英脉型矿床和蚀变花岗岩型矿床严格受断层及其次级断裂控制.东小泉金矿成矿期次分为两期,一期与F1断层形成有密切关系,另一期与NE-SW向断层关系密切.东小泉金矿的蚀变岩型金矿规模较石英脉型规模大,应加强不同方向断层交汇处的勘查.
Types and metallogenic tectonic model of the DongXiaoquan gold deposit in Beishan,Gansu
The Dongxiaoquan gold deposit located in the Beishan area of Gansu,is an important metal deposit enrichment area in Northwest China.It is a newly discovered gold-bearing quartz vein type and fracture zone altered rock type combination deposit in recent years.By analyzing the geological characteristics of the depos-it,the period of ore-controlling structure,the spatial relationship between gold ore body and structure,the metallogenic tectonic model of this area is summarized.The results show that the quartz vein type deposits and altered granite type deposits in this area are strictly controlled by faults and their secondary faults.The mineralization period of Xiaoquan gold deposit is divided into two periods,one is closely related to the forma-tion of F1 fault,and the other is closely related to the NE-SW trending fault.The scale of altered rock type gold deposit in the Dongxiaoquan gold deposit is larger than that of quartz vein type,and the exploration of fault intersection in different directions should be strengthened.

gold depositmetallogenic structureDong xiaoquanBeishanGansu

郭晓

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灵宝金源矿业股份有限公司,河南灵宝 472500

河南黄金产业技术研究院有限公司,河南灵宝 472500

金矿床 成矿构造 东小泉 北山 甘肃

2024

矿产与地质
桂林矿产地质研究院

矿产与地质

CSTPCD
影响因子:0.42
ISSN:1001-5663
年,卷(期):2024.38(5)