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1 Géosciences Azur, IRD
250
avenue Albert Einstein
06560 Valbonne, France
Empirical greens function (EGF) analysis has remained
little used to
image the rupture properties of the giant 26 December 2004 Sumatra earthquake.
The 2 November 2002 foreshock (Mw 7.2), close to the
mainshock epicenter, gives
us the opportunity to use its waveforms to empirically simulate the
Rayleigh-wave
propagation of the Sumatra earthquake. We first show that the exceptional size
of
the Sumatra earthquake does not prevent use of the EGF technique.
Four aftershocks
(Mw 5.96.1), distributed along the
SumatraAndaman trench, are shown to have
consistent Rayleigh waves for periods between 100 and 200 sec. At a lower
frequency,
we present two large earthquakes of the Mexican subduction zone
(Mw 7.2
7.3, close to the selected EGF magnitude) for which long-period
Greens functions
(1002000 sec) remain very similar, even if event epicenters are separated
by about
650 km. This justifies the possibility of using the 2002 foreshock as an
EGF for the
whole rupture process of the Sumatra earthquake and shows more generally the
very
broad range of application of EGF technique. Then, a specific
analysis reveals that
seismic moment magnitude is close to 9.1 (seismic moment equal to 5.6 x
1022 N m).
Moment release analysis along the SumatraAndaman trench shows two main
slip
episodes: one next to the northern extremity of Sumatra (
20-m slip) and the
other
one along the Nicobar Islands (
10-m slip), with a global extent of
11501200 km.
Rupture velocity varies between values around 2.5 km/sec in the first half of
the
rupture and values closer to 2 km/sec in the second half. Total duration imaged
by
Rayleigh waves is 580 sec (±20 sec) and no activity of the fault is found
in the time
scale between 600 and 2000 sec. In the hypothesis of even longer timescale slip,
this
phenomenon would be of the order of 10%20% of the global moment and
likely
restricted to the Andaman Islands.
This article has been cited by other articles:
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S. L. Bilek, K. Satake, and K. Sieh Introduction to the Special Issue on the 2004 Sumatra-Andaman Earthquake and the Indian Ocean Tsunami Bulletin of the Seismological Society of America, January 1, 2007; 97(1A): S1 - S5. [Full Text] [PDF] |
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S. Lambotte, L. Rivera, and J. Hinderer Constraining the Overall Kinematics of the 2004 Sumatra and the 2005 Nias Earthquakes Using the Earth's Gravest Free Oscillations Bulletin of the Seismological Society of America, January 1, 2007; 97(1A): S128 - S138. [Abstract] [Full Text] [PDF] |
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M. Chlieh, J.-P. Avouac, V. Hjorleifsdottir, T.-R. A. Song, C. Ji, K. Sieh, A. Sladen, H. Hebert, L. Prawirodirdjo, Y. Bock, et al. Coseismic Slip and Afterslip of the Great Mw 9.15 Sumatra-Andaman Earthquake of 2004 Bulletin of the Seismological Society of America, January 1, 2007; 97(1A): S152 - S173. [Abstract] [Full Text] [PDF] |
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