摘要
霍州矿区断层构造的分形特征与渭河盆地东区基本相同，都形成于张扭性的动力学环境；矿区内各井田的断层分维值以白龙井田最高，团柏井田最低；分维值的大小体现断层构造的复杂程度。
The fractal characteristics of fault structures in Huozhou Mining Area is similar to that in the eastern district of Weihe Basin,both formed in the tenso shear dynamic environment.The maximum fractal dimension occures in Bailong coal field and the minimum value in Tuanbai coal field.The magnitude of the tractal dimensions reflects complexity of the fault stractures.
出处
《西安矿业学院学报》
1997年第1期22-24,43,共4页
Journal of Xi'an University of Science & Technology
关键词
断层构造
分形特征
断层
霍州矿区
fractal fractal dimension fault Huozhou Mining Area
