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Stations used for source inversion analysis of foreshock are gray-filled, and stations used for source inversion analysis of mainshock are bordered by thick lines.
This is an accurate method, but time-consuming because of the large number of subsources used for source inversion and forward ground-motion simulation.
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Line-of-sight deformations were derived from the processed InSAR images (Lindsey et al. 2015) and are used for the joint source inversion.
High-and low-pass filters for source inversions were set at 0 and 48 Hz respectively, although a standard and a tight filter had already been applied to the data prior to the source inversion.
Figure 1 Broadband seismic stations used in the source inversion.
Fig. 2 The stations used in the source inversion and waveform comparisons between synthetics and observations.
The methodology used has been designed to be extremely flexible, in order to be easily applied to different datasets and, eventually, used for the inversion of any other seismic source with a complex source time function.
First, source rupture process analysis is carried out using joint source inversion.
To understand the mechanisms of the 0420 earthquake, the rupture processes were investigated using joint source inversion.
The inversion times used for the 3D inversion recovery sequence of both early and late CE-CMR were determined with a Look Locker sequence.
Therefore, only the determinant of the impedance tensor was used for 2D inversion whereas all elements of the impedance tensor were used for 3D inversion.
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