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In this study, we first estimated the source process of this event using the kinematic joint earthquake source inversion with near-field waveforms, teleseismic waveforms, and geodetic data.
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But it could not be used as a school, because it did not comply with the state mandates, applicable to schools only, that among other things require inspectors to be present continuously during construction to ensure that each hidden joint is earthquake-proof.
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The arrival times of 434 local earthquakes, two vibroseis shots and eleven explosive shots were used in a joint inversion to determine earthquake locations and a 3-D velocity structure of the crust.
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CEO of Professional Science Editing for Scientists @ prosciediting.com