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  1. 防災科研関係論文

Performance test of an automated moment tensor determination system for the future “Tokai” earthquake

https://nied-repo.bosai.go.jp/records/5000
https://nied-repo.bosai.go.jp/records/5000
9498df9e-202c-417b-a7b2-f6fbc2d478de
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 ja
タイトル Performance test of an automated moment tensor determination system for the future “Tokai” earthquake
タイトル
言語 en
タイトル Performance test of an automated moment tensor determination system for the future "Tokai" earthquake
言語
言語 eng
著者 Fukuyama E

× Fukuyama E

ja Fukuyama E

en E Fukuyama

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Dreger D

× Dreger D

ja Dreger D

en DS Dreger

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抄録
内容記述タイプ Other
内容記述 We have investigated how the automated moment tensor determination (AMTD) system using the FREESIA/ KIBAN broadband network is likely to behave during a future large earthquake. Because we do not have enough experience with a large (M > 8) nearby earthquake, we computed synthetic waveforms for such an event by assuming the geometrical configuration of the anticipated Tokai earthquake and several fault rupture scenarios. Using this synthetic data set, we examined the behavior of the AMTD system to learn how to prepare for such an event. For our synthetic Tokai event data we assume its focal mechanism, fault dimension, and scalar seismic moment. We also assume a circular rupture propagation with constant rupture velocity and dislocation rise time. Both uniform and heterogeneous slip models are tested. The results show that performance depends on both the hypocentral location (i.e. unilateral vs. bilateral) and the degree of heterogeneity of Slip. In the tests that we have performed the rupture directivity appears to be more important than slip heterogeneity. We find that for such large earthquakes it is necessary to use stations at distances greater than 600 km and frequencies between 0.005 to 0.02 Hz to maintain a point-source assumption and to recover the full scalar seismic moment and radiation pattern. In order to confirm the result of the synthetic test, we have analyzed the 1993 Hokkaido Nansei-oki (M(J)7.8) and the 1995 Kobe (M(J)7.2) earthquakes by using observed broadband waveforms. For the Kobe earthquake we successfully recovered the moment tensor by using the routinely used frequency band (0.01-0.05 Hz displacements). However, we failed to estimate a correct solution for the Hokkaido Nansei-oki earthquake by using the same routine frequency band. In this case, we had to use the frequencies between 0.005 to 0.02 Hz to recover the moment tensor, confirming the validity of the synthetic test result for the Tokai earthquake.
言語 en
書誌情報 ja : earth, planets and space
en : EARTH PLANETS AND SPACE

巻 52, 号 6, p. 383-392, 発行日 2000
出版者
言語 en
出版者 TERRA SCIENTIFIC PUBL CO
ISSN
収録物識別子タイプ ISSN
収録物識別子 1343-8832
DOI
関連識別子 10.1186/BF03352250
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