摘要
应用分形几何理论讨论了黄庄—高丽营断层的分段性。用分数维作为定量标志把断层分成了三段 (SW— NE) :第 段和第 段以良乡凸起为界 ,第 段和第 段以 NW向的南口—孙河断层为界。用地球物理资料、大地测量和断层位移测量资料、地震活动资料等对分段的合理性进行了验证。认为分数维较大、断层活动和地震活动性均较强的第 段应为地震危险重点监视区。
The Segmental Characteristics of the Huangzhuang gaoliying fault System are discussed according to the fractal theory.The fractal dimensions of each segments of the fault system are calculated.Based on the fractal dimensions,the Huangzhuang Gaoliying fault System is divided into three segments.The results show that fractal dimensions of each segments are consistent with both geophysical data and the characteristics of seismicity The most active segment that deserve extra attention in the fault system is the middle segment(from Lishuiqiao to Xiaoyouying).
出处
《华北地震科学》
2000年第1期9-13,共5页
North China Earthquake Sciences
基金
地震科学联合基金会资助课题!课题编号 :1980 87
