Japan Geoscience Union Meeting 2018

Presentation information

[EJ] Evening Poster

S (Solid Earth Sciences) » S-CG Complex & General

[S-CG57] Dynamics in mobile belts

Wed. May 23, 2018 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall7, Makuhari Messe)

convener:Yukitoshi Fukahata(Disaster Prevention Research Institute, Kyoto University), Toru Takeshita(Department of Natural History Sciences, Graduate School of Science, Hokkaido University), Hikaru Iwamori(海洋研究開発機構・地球内部物質循環研究分野)

[SCG57-P19] Detailed hypocenter distribution and fault structure in the 2017 M 5.3 Kagoshima Bay earthquake sequence

*Yoshiaki Matsumoto1, Keisuke Yoshida1, Toru Matsuzawa1, Akira Hasegawa1 (1.Research Center for Prediction of Earthquakes and Volcanic Eruptions, Tohoku University)

Keywords:earthquake sequence in Kagoshima Bay, hypocenter relocation, fault structure, seismic gap, fluid

On 11 July 2017, an MJMA 5.3 earthquake occurred at approximately 10 km depth in Kagoshima Bay, Kyushu, SW Japan. This earthquake caused intense ground shaking in the surrounding regions. Japan Meteorological Agency (JMA) seismic intensity was upper five at Kagoshima city, which is located in close proximity to the hypocenter.

Near the mainshock hypocenter, seismicity had been activated since December 2016. Most of hypocenters of this precursory activity were distributed within ~5 km from the mainshock hypocenter and, according to the JMA unified catalogue, they did not form planar structures but a cloud-like scattered distribution. This cloud-like distribution might merely reflect hypocenter errors (e.g. Yoshida & Hasegawa, 2018). On the other hand, such a cloud-like distribution can be explained by the hydraulic diffusion model (Shapiro et al., 1997; Rothert & Shapiro, 2003). Information on precise hypocenter locations is important for understanding the generation mechanism of this seismic activity. In this study, we improved relative locations of hypocenters of this earthquake sequence by using waveform cross correlation to investigate the fault structures in detail.

Firstly, we got precise differential arrival times by calculating cross correlations of the pair of waveforms out of the 11,105 earthquakes that occurred after March 2003 in the Southern Kagoshima Bay region. We used waveform data observed at 20 stations located around the mainshock hypocenter. We applied a bandpass filter between 5 and 12 Hz to the data, and computed cross-correlation functions for all event pairs whose horizontal distances are < 3.0 km. We adopted 2.5 s and 4.0 s starting 0.3 s before the onsets for the P- and S- wave windows, respectively. For the P- and S-wave onsets, we used arrival time data listed in the JMA unified catalogue if available; otherwise, we used theoretical arrival times computed by assuming the JMA velocity model (Ueno et al., 2002).

Secondly, using the obtained differential arrival time data, we relocated hypocenters. We applied the double-difference location method (Waldhauser and Ellsworth, 2000) to differential arrival data listed in the JMA catalog in addition to the data obtained by cross correlations. Hypocenters were updated using 50 iterations. In the first 10 iterations, we gave more weight to the catalogue data to constrain relative locations with a large scale. In the latter 40 iterations, more weight was given to the data derived by the cross correlations to delineate shorter scale.

As a result, hypocenters are concentrated on several thin planes, although the original JMA hypocenters were scattered and showed a cloud-like distribution. Hypocenters of the precursory activity are concentrated on one thin plane. Hypocenter distribution on this plane shows a clear seismic gap adjacent to the mainshock hypocenter, which might suggest that the mainshock rupture is located on this seismic gap.

Aftershock hypocenters are also concentrated on several thin planes. Their hypocenters tend to move upward with time. This spatial and temporal feature is similar to those observed in the earthquake swarms in central Tohoku that were triggered by the 2011 M9 Tohoku-Oki earthquake. Those earthquake swarms are estimated to be caused by the upward fluid movements (Yoshida & Hasegawa, 2018). The present observation suggests that the reduction in frictional strength due to the upward fluid movements plays an important role in the occurrence of the 2017 seismic activity in Kagoshima Bay.