摘要
地质雷达是一种广泛应用于地质探测的高频电磁脉冲波技术,利用高频电磁波在岩体传播中遇到地质界面产生反射的特性探测异常地质体的一种方法。通过地质雷达探测方法具有高精度、连续无损、经济快速、抗干扰强、图像直观等特点,将其应用于金州断裂探测中。
GPR, a high-frequency electromagnetic pulse technology, is widely used in geological exploration and abnormal geologic body detection by using the characteristics reflected from uhe geological interface, which was met with the high frequency electromagnetic waves. According to the research in this paper, so many advantages of geological radar detection method are introduced, such as high accuracy, continuous non-destructive, rapid and economical feature, better anti-interference and intuitive image, which will be applied in the fault detection in Jinzhou.
出处
《防灾减灾学报》
2013年第2期22-27,共6页
Journal of Disaster Prevention And Reduction
关键词
地质雷达
断裂
探测
Ground Penetrating Radar
fault
detection
