Simple and reliable finite fault solutions for large earthquakes using the W-phase: The Maule (M w = 8.8) and Tohoku (M w = 9.0) earthquakes
We explore the ability of W-phase waveform inversions to recover a first-order coseismic slip distribution for large earthquakes. To date, W-phase inversions for point sources provide fast and accurate moment tensor solutions for moderate to large events.
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|Source:||Geophysical Research Letters|
|01_Benavente_Simple_and_reliable_finite_2013.pdf||700.36 kB||Adobe PDF|