首页|期刊导航|世界核地质科学|苗儿山矿田中段红桥地区断裂构造特征及对铀矿找矿的指示意义

苗儿山矿田中段红桥地区断裂构造特征及对铀矿找矿的指示意义OA

Characteristics of faults and their implications for uranium prospecting in Hongqiao area,central Miao'er shan ore field

中文摘要英文摘要

广西苗儿山矿田是华南重要的花岗岩型铀矿集中区之一,矿体产出严格受断裂构造控制.通过对红桥地区开展系统的野外地质调查,梳理各构造期次断裂发育特征,对喜马拉雅期节理统计分析,反演该期对应的古应力场,总结了各构造期次的断裂特征及对成矿的作用.研究结果表明:研究区加里东期受SE-NW向挤压应力控制,形成了NE向展布的苗儿山复式岩体;印支期区域应力场转为近SN向,随着断裂作用的持续,地壳抬升导致变形机制由韧性向脆性转变;燕山期应力场由挤压体制转换为伸展,含铀热液在不同方向 断裂的交会部位发生运移,随后沉淀富集,最终形成铀矿体.在成矿特征方面,大型断裂构造带通常不具备成矿条件,规模适中的次级断裂是主要赋矿空间,区内花岗岩型铀矿主要受三、四级断裂构造控制.此外,矿体厚度受后期热液蚀变作用显著影响,强烈的蚀变作用可使矿体进一步加厚.综合分析认为:不同方向断裂构造交会,叠加含矿热液脉体侵入、热液蚀变强烈区域,具有较大找矿潜力,可作为后续勘查工作的重点部署区域.

The Miao'ershan ore field in Guangxi is one of the important granite-type uranium deposits in South China,where ore bodies are strictly controlled by fault zones.Systematic field geological surveys were carried out in the Hongqiao area.By analyzing the development characteristics of faults across various tectonic stages and conducting a statistical analysis of joints from the Himalayan period,we can reconstruct the paleostress field corresponding to that period,and the fracture characteristics of each tectonic stage as well as their metallogenic effects were summarized.The results indicate that during the Caledonian orogeny,the area was controlled by southeast-northwest compressional stress,leading to the formation of the northeast-trending Miao'ershan composite intrusion.During the Indosinian orogeny,the regional stress field shifted to a near-north-south orientation.With continuous fault activity and crustal uplift,the rock deformation mechanism transitioned from ductile to brittle.During the Yanshanian stage,the regional stress field switched from a compressional tectonic regime to an extensional one.Uranium-bearing hydrothermal fluids migrated toward the intersections of multiorientation faults,precipitated and concentrated at these structural sites,and ultimately formed uranium ore bodies.In terms of mineralization characteristics,large-scale primary fault zones generally fail to form ore deposits,moderately sized secondary faults are the primary ore-hosting zones.Granitic uranium deposits in this study area are mainly controlled by third-and fourth-order fault structures.In addition,late-stage hydrothermal alteration exerts a prominent control on ore body thickness,and intense hydrothermal alteration can significantly increase ore body thickness.A comprehensive analysis indicates that structural domains characterized by intersecting multi-orientation faults,superimposed emplacement of orebearing hydrothermal veins and intense hydrothermal alteration possess excellent prospecting potential,this area can be designated as a priority for future exploration efforts.

蒋征林;罗远红;杨海军;罗桥花;王建文

广西壮族自治区三一〇核地质大队,广西 桂林 541213广西壮族自治区三一〇核地质大队,广西 桂林 541213广西壮族自治区三一〇核地质大队,广西 桂林 541213广西壮族自治区三一〇核地质大队,广西 桂林 541213广西壮族自治区三一〇核地质大队,广西 桂林 541213

天文与地球科学

苗儿山矿田红桥地区断裂构造构造应力场找矿方向

Miao'er shan ore fieldHongqiao areafault zonetectonic stress fieldprospecting target area

《世界核地质科学》 2026 (4)

724-734,11

广西铀矿资源勘查关键技术研究人才小高地,广西地质矿产勘查开发局项目(编号:2025016,2026057,2026058)联合资助 Supported jointly by the Talent Highland for Key Technology Research of Uranium Resource Exploration in Guangxi and projects Supported by the Bureau of Geology and Mineral Resources Exploration and Development,Guangxi Zhuang Autonomous Region(Grant No.2025016,2026057,2026058).

10.3969/j.issn.1672-0636.2026.04.007

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