摘要
对于典型矿床而言,加强对其断裂构造的分维值的判定,能够加强研究人员对断裂分布的重视,这对于研究典型矿床控矿断裂的分形特征具有非常重要的作用。其作为一种典型的矿床分形特征,能够充分将断层数量、实际规模、发育程度、组合方式以及动力学等全面的表现出来。而本文主要是以江西九瑞地区为例,围绕当地典型矿床控矿断裂的分形特征进行了探讨分析,旨在为相关工作人员的后续研究提供一些参考意见。
For a typical ore deposit, strengthening the judgement of fractal dimension of its fracture structure can enhance the researchers' attention to the distribution of fractures, which is very important for studying the fractal characteristics of ore controlling faults in typical deposits. As a typical fractal feature of ore deposits, it can fully show the number of faults, the actual scale, the degree of development, the way of combination and the dynamics. This paper is mainly to the Jiangxi Jiujiang Ruichang area as an example, discusses on the fractal characteristics of ore controlling faults of local typical ore deposits, in order to provide some reference for future research related staff.
作者
李佳霖
LI Jia-Lin(Tong hua Geoligy &Mineral Resource Prospecting &Exploitation Institute Jilin Province,Tonghua 134001,China)
出处
《世界有色金属》
2018年第3期148-148,150,共2页
World Nonferrous Metals
基金
吉林省辉南县庆云金及多金属矿普查
关键词
典型矿床
控矿断裂
分形特征
typical ore deposits
ore control fracture
fractal characteristics