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Inverted model after an iteration |
Inverted model after 2 iterations |
Misfit function and step length:
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Waveform comparison between observed and simulated seismograms after one iteration for source 6 at station A1. Here, sources 6 and 7 have been used as reference sources for misfit calculation.
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The same test configuration of 16 sources and 49 stations has been used for inversion. The second run finished after 2 iterations.
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Cross sections of the final inverted model
y=100km |  z=25km |
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Misfit function and step length:
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