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METHOD FOR ACCENTUATING SPECULAR AND NON-SPECULAR SEISMIC EVENTS FROM WITHIN SHALLOW SUBSURFACE ROCK FORMATIONS

机译:浅层地下岩石地层中分形和非分形地震活动的方法

摘要

A method for evaluating subsurface formations includes deploying at least two intersecting seismic transducer lines above an area of the subsurface to be surveyed. Each line includes spaced apart seismic transmitters on one side of the intersection and spaced apart seismic receivers on the other side. On each line, one of the transmitters is actuated and signals are detected at one of the receivers. The foregoing is repeated for each of the remaining receivers. The foregoing is then repeated for each of the remaining transmitters on each line. The detected signals are processed to enhance both specular and non-specular seismic events in the subsurface. The enhanced events may be stored and/or displayed.
机译:一种用于评估地下地层的方法,其包括在要勘测的地下区域上方部署至少两条相交的地震换能器线。每条线在交叉路口的一侧包括间隔开的地震接收器,在另一侧包括间隔开的地震接收器。在每条线上,启动一个发射器,并在其中一个接收器处检测信号。对于其余的接收器中的每一个重复上述步骤。然后针对每条线路上的每个其余发射机重复上述步骤。处理检测到的信号以增强地下的镜面和非镜面地震事件。增强事件可以被存储和/或显示。

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