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Array-conditioned deconvolution of multiple component teleseismic recordings

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Academic year: 2021

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Figure

Table 1. The earthquake parameters of the four exemplary events. ∆ is epicentral distance from the event to the center of the POLARIS-MIT array
Figure 3. Summary of the synthetic experiments. (a) The synthetic array data of λ=1. The deconvolved data section using (b) waterlevel deconvolution with GCV-derived δ; (c) waterlevel deconvolution with the factor of 1%; and (d) array-conditioned deconvolu
Figure 4. Comparison of the amplitude spectra of the deconvolved SV signals of trace 3, derived from the array deconvolution and the waterlevel deconvolution, respectively
Figure 6. The raw data (P and SV components) of four exemplary earthquakes from (a) Honshu, Japan;
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