Method for explaining active fault moving strength and growing directions through artificial earthquake
A technology of activity intensity and artificial earthquake, applied in the direction of seismic signal processing, etc., can solve the problems of unreported, no comprehensive analysis of seismic geological information, and uncertainty of the change process and growth trend of active fault activity intensity, so as to promote development, Reliable geological basis and the effect of improving scientificity
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[0013] Such as figure 1 , 2 The shown method for artificial seismic interpretation of activity intensity and growth direction of active faults, the steps include:
[0014] 1. Determine the growth trend of active faults: collect and process ultra-shallow seismic data, connect the breakpoints of each seismic horizon in sequence on the time profile, and then obtain a continuous section of active faults; record the faults on the seismic time profile 0 drop point time, the 0 drop point of the section is counted in different sections of space, and the latest activity time limit of different sections of the active fault is obtained, that is, the shallowest part reached by the latest activity of the active fault, and the envelope connecting these shallowest points As the front line of the fault plane, the reactivation of the active fault will continue along the vector direction of the front end point; according to the vector direction of the front line, the spatial growth and develop...
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