Journal of Japan Society of Civil Engineers, Ser. B2 (Coastal Engineering)
Online ISSN : 1883-8944
Print ISSN : 1884-2399
ISSN-L : 1883-8944
The Source Mechanism of the 2009 Samoa Earthquake and Tsunami
Hideomi GOKONShunichi KOSHIMURAKentaro IMAI
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2011 Volume 67 Issue 2 Pages I_211-I_215

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Abstract
The tsunami that accompanied with a magnitude-8 earthquake attacked the Samoan and northern Tongan islands on 29 September 2009. Since the event occured, two scenarios ascertain the mechanism of the earthquake that a series of normal and thrust faults caused the large earthquake and tsunami. However, it is still uncertain which one was the first rupture. In this paper, the authors focus on the tsunami waveforms of Deep-ocean Assessment and Reporting of Tsunamis(DART), and proposed the tsunami source scenario that is the most consistent with the observed tsunami. The scenario is that, the rise time of the thrust fault rupture is 480 seconds, which starts from 3 minutes before the normal fault rupture, and the rise time of the normal fault rupture is 60 seconds.
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© 2011 by Japan Society of Civil Engineers
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