From earthquake centroid to spatial-temporal rupture evolution: Mw 6.3 Movri Mountain earthquake, June 8, 2008, Greece

We propose a new strategy to reveal the spatial‐temporal evolution of the earthquake rupture process from near‐regional data, without assuming a constant rupture velocity. The approach is based on a conjugate gradient method, for which we express analytically the required waveform‐misfit derivative...

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