Ratio of radiated seismic energy and moment to determine source mechanism of the 2010 Mentawai tsunami earthquake

Sugeng PribadiNanang T. PuspitoAfnimar and Gunawan Ibrahim

Abstract: The 25 October 2010 Mentawai earthquake has magnitude Mw 7.7 and shallow depth (12 km). Although the local people of Sikakap - the closed island near epicenter (78.33 km) only felt low shaking (II-III Mercally Intensity), it rised tsunami 7.4 m height causing casualties 447 people died. We suggested the phenomenon is the tsunami earthquake. Therefore we calculate the source mechanism by using W-phase method to determine its parameter. The result yield good value due to reference of GCMT solution with strike 340.3°, dip 8.3°, and slip 116.9°. The cross section diagram of hypocenter show the event located on the beginning of subduction. We obtain the values of seismic radiated energy 1.76×1014 Nm, seismic moment5.37×1027 Nm, and its ratio is Θ = −6.1 . It counted as the threshold of tsunami earthquake. The rupture process has long duration 82 s. The facts proved that the 2010 Mentawai as a tsunami earthquake.

http://scitation.aip.org/content/aip/proceeding/aipcp/10.1063/1.4730711

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