Microseismic first arrival acquisition method based on shear wave and Akaike information criterion
A microseismic and shear wave technology, applied in seismology, seismic signal processing, geophysical measurement, etc., can solve the loss of amplitude-frequency characteristics of microseismic records, complex background noise components and properties, and difficulties in automatic picking of microseismic first arrivals and other problems, to achieve the effect of avoiding energy loss, retaining amplitude-frequency characteristics, and fast automatic pick-up speed
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[0056] Include the following steps:
[0057] 1) Acquisition of microseismic two-dimensional records:
[0058] Microseismic monitoring is divided into two methods: borehole monitoring and surface monitoring. The spatial and temporal distribution of microseismic events induced during injection operations is complex, but not Random, within 1Km range can be received with appropriate sensitive equipment. The frequency range of most microseismic events is between 50 and 1500 Hz, and the duration is less than 1 second, which generally appear as clear pulses on the microseismic records; the weaker microseismic events have higher frequency and shorter duration; energy The smaller it is, the shorter the length of the rupture. Therefore, the microseismic signal is easily affected or obscured by the surrounding noise, and it is more difficult to pick up the first arrival of the microseismic record with low SNR, and the error is also larger.
[0059] 2) Frequency division processing of...
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