Kikuchi method is applied for teleseismic body-waveform modeling.
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Transcript of Kikuchi method is applied for teleseismic body-waveform modeling.
Kikuchi method is applied for teleseismic body-waveform modeling
• 154 teleseismic body-waveforms (only P) is used.
• Magnitude 6.4• Strike/dip/rake: 168/53/130• The fault is dipping W-SW• 2 main peaks in the source-
time-function (STF), about 7 and 13 seconds after the rupture initiation.
• Total STF about 16 seconds.
Kikuchi method is applied for teleseismic body-waveform modeling
• Max slip about 90 cm.• 2 different fault segments moved during the
earthquake. That is why the GCMT solution shows substantial non-double-couple (NDC) component; better to say CLVD component.
• Segment 1 (between -6 and 10km along strike) was almost pure reverse.
• The slip contours of the first segment was deeper compared to that of segment 2.
• This is equivalent to the first peak (at 7 seconds) in the STF.
• Segment 2 (between 10km and 30km along strike) was behind the main energy release. It was a shallow reverse subevent with substantial strike-slip component.
• Slip contours of 0.1 m• The slip-distribution is
very dependent on the epicenter location. It can be shifted based on the correct epicenter location.
• Slip contours of 0.2 m.
• Slip contours of 0.1 m with aftershocks recorded by IGTU.