摘要
浅层地震反射法是工程地质勘察中的一种重要手段,其特有的高分辨率特性有利于确定地层界面,基起伏变化的形态。在地震断裂带上具有明显地表特性的地点实施浅层地震勘探工作,并借数据反映断裂带的形态、范围与隐伏深度,为进一步解释地震产生的原因提供数据支持。
Shallow seismic reflection method is an important means of engineering geological investigation, the characteristics of high resolution to determine the formation interface, ups and downs change form. The location of the surface features on Ihe earthquake fault zonte has olwious implementation of shallow seismic exploration, and data reflect the form and scope of the fault zone and the buried depth, provider data support for further explain the causes of the earthquake.
出处
《科技视界》
2014年第15期10-10,54,共2页
Science & Technology Vision
关键词
浅层地震反射法
地震
断裂带
Shallow seismic reflection method
The earthquake
Fault
