Distribution of the Metropolitan Seismic Observation network · 2021. 4. 8. · V 01–‚u˛™l4...

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57

Bull. Earthq. Res. Inst.

Univ. Tokyo

Vol. pp.

* e-mail : coco@eri.u-tokyo.ac.jp

:

Earthquake Research Institute, the University of Tokyo

The Special Project for Earthquake Disaster Mitigation in the Tokyo Metropolitan Area has

been ongoing ( ). Under this project, the Metropolitan Seismic Observation network

(MeSO-net), which consists of about observation sites, has been constructed. This network

consists of five dense linearly arrayed stations and evenly spaced stations. This five liner arrays

focus on observing highly active seismicity, many repeating earthquakes, slow slip area, and

historical large earthquakes. The correlations of waveform from local and teleseismic events are

high because observation points are deployed at about or -km intervals. In addition, identific-

ation of any stations of the later phase is easy even if artificial noise is very intense. These widely

developed stations have been used e ectively for the seismic tomography method. These dense

intervals of MeSO-net will induce a more highly resolved structure than previous studies. MeSO-net

has observed earthquakes of more than M . . Low-frequency waveforms of less than . Hz have

been observed by MeSO-net. The distribution of amplitudes observed at each station show

heterogeneous amplification of shaking motions.

Our study will lead to improved quality of plate structure, and contribute to a new assessment

of seismic hazards in the Tokyo Metropolitan Area, Japan.

: MeSO-net, dense seismic observation, seismic sensitivity, heterogeneous amplification

M .

:

M :

M M

*

Shin’ichi Sakai* and Naoshi Hirata

Abstract

Key words

Distribution of the Metropolitan Seismic Observation

network

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Table Fig.

km

MeSO-net M

km

Metropolitan Seismic Observation net-

work : MeSO-net km

km km

m

Fig.

km

km MeSO-net

SN

M

a

b

Table Fig.

km

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59

Fig. . Distribution of seismic stations of MeSO-net.

Color indicates year station was established. Dots indicate stations under development.

Large square and small squares indicate area of estimated Northern Tokyo-Bay

Earthquake and stations still to be developed within it.

Nakajima and Hasegawa,

Igarashi,

Table , Fig. Kimura

Fig.

P S

km

km

MeSO-net

a

Matsubara

et al.,

et al.,

+

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60

observed by the Tsukuba-Fujisawa line. Top is northern station and bottom is southern station.

Fig. . Distribution of earthquakes of more than M . are shown with MeSO-net.

Color indicates focal depth. Earthquakes were determined by MeSO-net ( . . . . ).

Fig. . Waveforms of earthquake (M . , depth km) occurring at northern Tokyo-bay on Oct.,

Fig.

MeSO-net

m

,**3

, , *

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- , / -* +1

-

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61

. . .

a . M .

win

P , S ,

, ,

Fig. M .

MeSO-net

Fig.

m

cm m

JA- GA

Hz

TS

M

M

Fig.

b

LAN

M .

RYGM M .

,**2 . + ,**3 3 -*

-/ +/ -0 ,/ +-2 2

,**3 +.+ 2 , *

03,

+33+ +03 ,,1 +/- 0/3

+2. -0/ 2* 3+,

, , *

.

,*

++ ,*

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+-2**

+31+

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* .

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,. * /-

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62

observed by the Tsukuba-Fujisawa line. Top is northern station and bottom is southern station.

Fig. . Waveforms of earthquake (M . , Depth km) occurring in Setagaya-ku, Tokyo on Jul.,

Waveforms are UD-component.

Fig. . Distribution of magnitude of amplitude of MeSO-net.

They obtained by the residual between the magnitude at each station and the averaged

magnitude. Red indicates larger than normal amplitude. Interval of counter is . .

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63

Fig. . Filtered waveforms observed at Tsukuba-Fujisawa line.

This earthquake (M . ) occurred at the Samoa Islands on Sep., .

Fig. . Distribution of magnitudes of amplitudes.

They obtained from the low-pass filtered waveform of the horizontal component. Interval

of counter is mgal.

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Table . List of the seismic stations of the MeSO-net that started in .+ ,**1

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66

Table . List of the seismic stations of the MeSO-net that started in ., ,**2

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Table . (Continued),

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68

Table . List of the seismic stations of the MeSO-net that started in .- ,**3

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M

dimensional P- and S-wave velocity structures beneath

the Japan Islands obtained by high-density seismic

stations by seismic tomography, ,

.

MeSO-net

ACT protocol

.

.

. a

Igarashi, T., , Seismic velocity discontinuities in the

crust and uppermost mantle beneath the Kanto district, P .

central Japan, identified from receiver function imag- b

ing and repeating earthquake activity,

, , . .

a Nakajima, J., F. Hirose, and A. Hasegawa, , Seismotec-

M tonics beneath the Tokyo Metropolitan area, Japan :

E ect of slab-slab contact and overlap on seismicity,

. , B , doi : . / JB .

b

.

.

MeSO-net

.

MeSO-

net .

MeSO-net

. .

Kimura, H., K. Kasahara, T. Igarashi and N. Hirata, , win

Repeating earthquake activities associated with the

Philippine Sea plate subduction in the Kanto district, No. .

central Japan : A new plate configuration revealed by

interplate aseismic slips, , , .

. (Received November , )

Matsubara, M., K. Obara, and K. Kasahara, , Three- (Accepted January , )

Tectonophysics,

Gondwana Re-search,

J.Geophys. Res.,

Tectonophysics,

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