Foreshock and aftershock sequence of the 1998 M 5.0 Sendai, northeastern Japan, earthquake and its implications for earthquake nucleation

Norihito Umino, Tomomi Okada, Akira Hasegawa

Research output: Contribution to journalArticlepeer-review

22 Citations (Scopus)

Abstract

We investigated foreshock and aftershock sequences of a M 5.0 earthquake that occurred on 15 September 1998 near the Nagamachi-Rifu fault, an active fault crossing the urban area of Sendai city, northeastern Japan. The focal mechanism of this event was a reverse-fault type with a nearly horizontal P axis parallel to the plate conversion direction. Aftershock distribution located by the homogeneous-station method delineates the fault plane of this event, dipping to the northwest at an angle of ∼30° in the depth range of 10-12 km. The location of the fault plane and the slip direction thus estimated suggest that this event was a slip at a deep portion of the Nagamachi-Rifu fault. Three days prior to the mainshock, many foreshocks with similar waveforms started to occur very close to the mainshock hypocenter. We estimated relative locations of these similar foreshocks based on cross-spectrum analyses of waveforms recorded at nearby stations. They are located at the deepest portion of the mainshock fault plane and just above the mainshock hypocenter. Migration of the foreshocks is observed from deeper to shallower depths. Cumulative Coulomb stress changes caused by preceding events show negative values at hypocenters of similar waveform foreshocks. Our results do not support the cascade model for the process of foreshock generation. Nucleation phase prior to the high-speed rupture of the mainshock is observed in seismograms at nearby stations. The initial point of the nucleation phase is located on a deeper extension of the foreshock area. The high-speed breakout point is located in the area where a large amount of seismic moment release was estimated from waveform inversions. These observations probably reflect an underlying aseismic nucleation process preceding the main dynamic rupture of the M 5.0 event.

Original languageEnglish
Pages (from-to)2465-2477
Number of pages13
JournalBulletin of the Seismological Society of America
Volume92
Issue number6
DOIs
Publication statusPublished - 2002 Aug

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology

Fingerprint Dive into the research topics of 'Foreshock and aftershock sequence of the 1998 M 5.0 Sendai, northeastern Japan, earthquake and its implications for earthquake nucleation'. Together they form a unique fingerprint.

Cite this