Method for measuring and determining micro-seismic focus
A micro-earthquake and source technology, which is applied in the fields of disasters, resources and environment, and can solve the problems of frequency characteristic variation, amplitude and energy distortion, and failure to achieve superposition.
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[0037] image 3It is the measured surface and well Z component data of hydraulic fracturing microseismic. The data has been filtered and normalized. It can be seen that the S-wave field data in the well is basically similar to the P-wave field data on the ground in terms of frequency characteristics, and the frequency range is roughly between 25-70Hz. The frequency of the P wave component in the well is relatively high, and due to the receiving direction of the geophone, the energy of the P wave is lower than that of the S wave; the surface data is also due to the Z component, and the energy level of the S wave is very low.
[0038] Figure 4 The arrangement of the above data after NMO is given. The best sign of microseismic event location is the first arrival alignment. It can be seen in the figure that the first main lobe of the peak corresponding to the surface and downhole data has been aligned; since the frequency characteristics of the surface P wave and downhole S wav...
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