摘要
民乐—双凤断裂带是罗浮山—灵山近东西向断裂系西段中一条重要的断裂带。沿带或其附近历史上曾发生过3次。和多次有感地震,是一条活动断裂带.研究发现。断裂的运动学特征为右旋剪切,多处出现断错沟谷,有些在地形地貌上显示为断头沟谷与断尾沟谷。
As west section of Luofushan-Lingshan system, Minle-Shuangfeng fault zone is a important active fault zone.Three earthquakes and many felt earthquakes occurred in the fault zone and vicinity of it in history. The kinetics characteristic of it is rightlateral shear.There are some dislocation trench-valleyes at some site of the fault zone. In the midst of dislocation trench-valleyes, some dislocation trench-valleyes is shown as the beheaded or betrunked trench-valleyes.
出处
《华南地震》
1996年第1期48-51,共4页
South China Journal of Seismology
基金
国家地震局合同制项目
关键词
断裂带
新构造运动
断层位移
广西
Active fault Zone, Neofecfonic movenent, Fault displacement,Guang Xi