Abstract:In order to solve the problem of source-locating error caused by inaccuracy of velocity model, we propose a method to locate microseismic source and simultaneously invert velocity structures with arrival times recorded at surface and borehole receivers.The traveltime derivatives with respect to velocity, layer interface depth, and microseismic event parameters are derived, and the ray paths and arrival times are calculated with the shortest path algorithm.In combination with the conjugate gradient approach, damping minimum norm and constrained least square problem are solved.Numerical test results show that the inversion algorithm can not only recover velocity structure (interval velocity and interface depth) but also locate source positions, and it is not sensitive to random noise.
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