Japan Geoscience Union Meeting 2019

Presentation information

[J] Oral

S (Solid Earth Sciences ) » S-SS Seismology

[S-SS10] Seismicity

Tue. May 28, 2019 1:45 PM - 3:15 PM A10 (TOKYO BAY MAKUHARI HALL)

convener:Kei Katsumata(Institute of Seismology and Volcanology, Hokkaido University), Chairperson:Aitaro Kato(Earthquake Research Institute, University of Tokyo), Shinji Toda(東北大学)

2:45 PM - 3:00 PM

[SSS10-05] Aftershock sequence of the 1847 Zenkoji earthquake: Temporal decay presented in four historical materials and best fit values of paramaters for Omori-Utsu law

*Kentaro Hattori1, Ichiro Nakanishi1 (1.Kyoto Univ.)

Keywords:the 1847 Zenkoji earthquake, aftershock sequence, Omori-Utsu law

Seismic intensities estimated from damage caused by earthquakes have been most commonly used to locate earthquake epicentral area since Irish seismologist Mallet used degree of damage by the great Napoli earthquake of 1857 to locate earthquake source area. However, the scales of seismic intensity are different among countries. The seismic intensities are somewhat subjective and are affected by ground conditions.

Matsui and Oike (1997) proposed the use of the numbers of felt aftershocks right after large historical earthquakes to locate source area. A problem in their approach is that it is usually difficult to count the number of aftershocks in epicentral area or places close to the area.

We attempt to fit Omori-Utsu law (Utsu, 1961) to aftershock sequences of a historical large earthquake to overcome the above mentioned problem of the location of epicentral area. The value from counting aftershocks is integer, and seems to be more robust than the estimation of ground motion from the description in historical materials. The temporal decay of the number of aftershocks n(t) is described by the empirical Omori-Utsu law as n(t) = K (t+c)-p, where t is the lapse time after the mainshock, p is an exponent showing the decay rate, c is a time scale, and K is a parameter showing aftershock activity.

We use aftershock sequence data of the 1847 Zenkoji earthquake presented in four historical materials owned in Matsushiro, Suwa, Fujinomiya, Gifu, in order of the distance from the epicentral area. We assume c=0.1 and p is common in four data, and obtain the best fitting p and four K. The result is shown in Fig.1. In the figure, it is clear that Omori-Utsu law does not fit the time range right after the earthquake occurrence for Matsushiro, Gifu, Suwa data, but fits Fujinomiya data. Another clear feature in Fig.1 is that the parameter K for Gifu data is 300. This value is much larger than those for Suwa (K=80) and Fujinomiya (K=6), both places are located closer to epicental area than Gifu. Fig.1 may suggest that the data preserved in Gifu were not written in Gifu, but in a place much closer to epicentral area.