黔西南赖子山背斜地区金矿构造控矿规律研究  

Study on the regularity of tectonic control of gold deposits in Laizishan anticline area of Southwest Guizhou

作　　者：赵明峰[1] 罗建均[1] 陆建宝 周克林 王伟[1] Zhao Mingfeng;Luo Jianjun;Lu Jianbao;Zhou Kelin;Wang Wei(The 117 Geological Team,Guizhou Bureau of Exploration and Development of Geology and Mineral Resources)

机构地区：[1]贵州省地质矿产勘查开发局117地质大队

出　　处：《黄金》2023年第4期63-68,74,共7页Gold

基　　金：贵州省地质矿产勘查开发局地质科研项目(黔地矿科合〔2021〕08号);中国地质调查局地质调查项目(DD20190159-30)。

摘　　要：赖子山背斜地区是贵州册亨—望谟金矿集区的重要组成部分,该地区已发现一处超大型金矿床和多处小型金矿床或金矿点,目前该区仍然具有很好的找矿前景。通过系统总结地质特征和金矿构造控矿规律,认为赖子山背斜地区具有明显的三级构造控矿特点,深源成矿流体的运移及富集与三级构造的关系密切,晚古生代的隐伏同生断裂+区域性赖子山背斜、层间滑脱构造+矿床级的断裂、褶皱组成的构造系统对金矿的形成具有明显的控制作用,并建立了赖子山背斜地区的构造控矿模式。The Laizishan anticline area is an important part of the Ceheng-Wangmo high gold concentration area in Guizhou province.In the area,a super large gold deposit and many small gold deposits and gold spots are dis-covered.At present,the area still has a good prospecting prospect.This paper systematically summarizes the geological features and tectonic ore control law and points out that Laizishan anticline area has obvious three-stage tectonic ore control characteristics,and that the migration and enrichment of deep-sourced ore-forming fluids are closely related to the three-stage tectonics.The tectonic system composed of hidden syngenetic faults of late Paleozoic+regional Laizishan anticline,interlaminar slip structure+mineral-grade faults and folds has an obvious control effect on gold deposit formation.The study established the ore-controlling model of the Laizishan anticline area.

关 键 词：赖子山背斜 金矿 控矿构造 成矿流体 三级构造 黔西南 

分 类 号：TD15[矿业工程—矿山地质测量]