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Subsurface imaging by seismic interferometry

机译:地震干涉测量次数成像

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The pseudo-reflection shot records can be generated by the cross-correlation of the transmission responses observed at the sensors located on the ground-surface, which is called "seismic interferometry" or "daylight seismic imaging." In this paper, we apply this technique to the field data observed by using several different types of micro-seismicity as seismic sources in order to appraise the practical applications of the seismic interferometry technology. Since this method requires a long record length, we newly developed a PC-based long-time seismic recording system with 96 channels. The experimental survey was carried out in a mountain area where two tunnels exists. Several micro-seismicity sources, for example running vehicles in the tunnel were adopted to make underground noise for the seismic interferometry. We acquired transmitted wave field generated by such sources moving in the tunnels. Obtained data were properly processed and it shows subsurface image clear enough to estimate underground structures and proved the seismic interferometry technology.
机译:可以通过在位于地面上观察到的传感器的传输响应的互相关来产生伪反射拍摄记录,该传感器被称为“地震干涉测量”或“日光地震成像”。在本文中,我们将该技术应用于通过使用几种不同类型的微地震性作为地震来源观察到的现场数据,以便评估地震干涉技术的实际应用。由于该方法需要长记录长度,我们新开发了一种具有96个通道的基于PC的长时间地震记录系统。实验调查在山区进行,其中存在两个隧道。采用了几种微地震源,例如在隧道中运行车辆来使地震干涉测量中的地下噪音。我们获取了由在隧道中移动的这种源产生的传输波场。获得的数据被正确处理,并显示出地下图像足够清除以估计地下结构并证明地震干涉测量技术。

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