Rupture process of the 2004 great Sumatra-Andaman earthquake estimated from tsunami waveforms View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2006-02

AUTHORS

Yuichiro Tanioka, Yudhicara, Tomohiro Kususose, S. Kathiroli, Yuichi Nishimura, Sin-Iti Iwasaki, Kenji Satake

ABSTRACT

Rupture process of the 2004 Sumatra-Andaman earthquake is estimated using tsunami waveforms observed at tide gauges and the coseismic vertical deformation observed along the coast. The average rupture speed of the 2004 Sumatra-Andaman earthquake is estimated to be 1.7 km/s from tsunami waveform analysis. The rupture extends about 1200 km toward north-northwest along the Andaman trough. The largest slip of 23 m is estimated on the plate interface off the northwest coast in the Aceh province in Sumatra. Another large slip of 21 m is also estimated on the plate interface beneath the north of Simeulue Island in Indonesia. The other large slip of 10–15 m is estimated on the plate interface near Little Andaman and Car Nicobar Inlands. The total seismic moment is calculated to be 7.2 × 1022 Nm (Mw 9.2) which is similar to the other studies using seismic waves (Park et al., 2005; Ammon et al., 2005). More... »

PAGES

203-209

Identifiers

URI

http://scigraph.springernature.com/pub.10.1186/bf03353379

DOI

http://dx.doi.org/10.1186/bf03353379

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1011585283


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