• 责任者：Liao Jiafei (School of Earth Sciences ; Guilin University of Technology ; Guilin 541004 ; China) ; Feng Zuohai
• 刊名：Mineral Deposits
• 出版年：2012
• 卷期：31(3)
• 关键词：钨矿 ; tungsten ores ; 锡矿 ; tin ores ; 矿田构造 ; mine field structure ; 广西 ; Guangxi
• 页码：p.459-464
• 图表：3 illus., 19 refs.
• 分类号：1001
• issnNo：ISSN0258-7106
• isbnNo：CN11-1965/P

Systematic quantitative analyses of fault structures in the Shuiyanba ore field were conducted on the basis of the box-counting dimension method. It is found that the faults of different scales in the Shuiyanba ore field have good self-similarity. The fractal dimension of faults is 1.347 5, the average fractal dimensions of micro-cracks of joints and hand specimens in the Lantoushan deposit of central ore field are 1.784 1 and 1.331 0, respectively. In the figure of subinterval high fractal dimension, the fractal dimension of the overall extension of the high value area trends northwest, the overall trend of fault structures and the ore field is consistently spread.