Seismic dynamite source is one of the key techniques in seismic data acquisition.
震源是地震勘探野外数据采集中的一个关键技术问题。
Theoretical reflection seismograms in dynamite source condition are formed by using anisotropic reflectivity method.
本文用各向异性反射率法计算爆破源反射地震的理论地震图。
Theoretical reflection seismograms in dynamite source condition are formed by using anisotropic reflectivity method.
本文用各向异性反射率法计算爆破源反射地震的理论地震图。
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