首页|赣南兴国—宁都萤石成矿带分形结构及成矿与找矿前景

赣南兴国—宁都萤石成矿带分形结构及成矿与找矿前景

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萤石是一种重要的非金属战略性关键矿产资源,其成矿规律及找矿预测广受矿床学界关注.赣南兴国—宁都萤石成矿带地处NE向武夷山成矿带与EW向南岭成矿带交汇复合部位,发育一系列萤石矿床.虽然前人对该区萤石矿床进行过较为系统的研究,认为其主要受断裂构造控制,但区内断裂构造和萤石矿床空间分布的定量表征及两者之间的耦合关系鲜有报道.本文基于分形理论刻画赣南兴国—宁都成矿带断裂构造和萤石矿床之间的分形结构特征,并探讨重点成矿与找矿区域.结果显示:研究区NE-NNE向断裂容量维、信息维和关联维分别为1.609 0、1.608 9、1.594 7,说明本区成矿地质条件优越,NE-NNE向断裂与研究区萤石成矿关系密切.萤石矿床容量维、信息维、关联维分别为0.937 9、0.921 5、0.926 2,含统计中心矿床时,萤石矿床数量分形分维值为0.784 1,密度分形分维值为0.784;未含统计中心矿床时,萤石矿床数量分形分维值为1.129 6,密度分形分维值为1.130.根据研究区断裂分维值与萤石矿床空间分布的耦合特征、萤石矿床数量及密度分形特征综合圈定了 3级有利成矿区,其中Ⅰ级有利成矿区为成矿条件最佳、成矿潜力最大的区域.根据断裂分维值与矿床空间分布的耦合特征、矿床数量及密度分形特征,可快速有效圈定受断裂体系控矿的萤石矿集区或成矿带内的重点找矿区域.
Fractal Structure and Application Prospect of Xingguo-Ningdu Fluorite Metallogenic Belt in Southern Jiangxi,China
As one of the important non-metallic strategic mineral resources,the metallogenic regularity,ore prospecting and exploration of fluorite are widely investigated byeconomic geologists.The Xingguo-Ningdu metallogenic belt in southern Jiangxi Province,located at the intersection of the NE-trending Wuyishan metallogenic belt and EW-trending Nanling metallogenic belt,develops a series of fluorite deposits.Previous studies have primarily attributed the deposits to fault control,but the quantitative characterization of the coupling relationship between fractures and the spatial distribution of the fluorite deposits is seldom reported.Based on fractal theory,this paper aims to describe the fractal textural characteristics between fractures and fluorite deposits in Xingguo-Ningdu metallogenic belt to identify key ore-forming and prospecting areas of fluorite.The results show that:1)The NE-NNE-trending fracture capacity dimension,information dimension and correlation dimension of the study area are 1.609 0,1.608 9,and 1.594 7,respectively,indicating superior metallogenic geological conditions and a strong relationship between NE-NNE faults and fluorite mineralization in the study area;2)The capacity dimension,information dimension and correlation dimension of fluorite deposits are 0.937 9,0.921 5 and 0.926 2,respectively.When there is a statistical center deposit,the fractal dimension of the number fractal distribution of fluorite deposits is 0.784 1,and the fractal dimension of the density fractal distribution is 0.784.When there is no statistical center deposit,the fractal dimension of the number fractal distribution of fluorite deposits is 1.129 6,and the fractal dimension of the density fractal distribution is 1.130;3)According to the coupling characteristics of the fractal dimension value of fracture and the spatial distribution of fluorite deposits in the study area,as well as the fractal characteristics of the number and density of fluorite deposits,the three-level favorable metallogenic areas are comprehensively delineated,in which the I-level favorable metallogenic area is the area with the best metallogenic condition and the largest metallogenic potential;4)According to the coupling characteristics of fracture dimension value and spatial distribution of deposits,the number and density fractal characteristics of deposits,the key ore forming and prospecting areas in the fluorite ore concentration area or metallogenic belt controlled by fracture system can be quickly and effectively delineated,which is expected to provide important reference information for the resource exploration of fluorite.

Xingguo-Ningdu metallogenic beltfracture structurefluorite depositfractal textureapplication prospect

崔中良、周家喜、罗开

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江西应用科技学院光华宝石与艺术设计学院,南昌 330100

云南大学地球科学学院,昆明 650500

云南省高校关键矿产成矿学重点实验室,昆明 650500

兴国—宁都成矿带 断裂构造 萤石矿床 分形结构 应用前景

江西省教育厅科学技术研究项目云南大学科研启动项目

GJJ213014YJRC4201804

2024

吉林大学学报(地球科学版)
吉林大学

吉林大学学报(地球科学版)

CSTPCD北大核心
影响因子:1.062
ISSN:1671-5888
年,卷(期):2024.54(1)
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