Premium
Rupture process of the 2011 Tohoku‐oki earthquake and absolute elastic strain release
Author(s) -
Yagi Yuji,
Fukahata Yukitoshi
Publication year - 2011
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2011gl048701
Subject(s) - seismology , hypocenter , geology , aftershock , trench , slip (aerodynamics) , seismic moment , waveform , fault (geology) , geodesy , materials science , induced seismicity , composite material , physics , layer (electronics) , quantum mechanics , voltage , thermodynamics
On 11 March 2011, the Tohoku‐oki earthquake in eastern Japan and the devastating tsunami that followed it caused severe damage and numerous deaths. To clarify the rupture process of the earthquake, we inverted teleseismic P‐wave data applying a novel formulation that takes into account the uncertainty of Green's function, which has been a major error source in waveform inversion. The estimated seismic moment is 5.7 × 10 22 Nm ( Mw = 9.1), associated with a fault rupture 440 km long and 180 km wide along the plate interface. The source process is characterized by asymmetric bilateral rupture propagation, but we also found continuous slips up‐dip from the hypocenter, which led to a large maximum slip (50 m), long slip duration (90 s), and a large stress drop (20 MPa). The long slip duration, large stress drop, extensional (normal faulting) aftershocks in a previously compressional stress regime, and low‐angle normal slips at approximately the depth of the plate interface suggest that the earthquake released roughly all of the accumulated elastic strain on the plate interface owing to exceptional weakening of the fault. The stress accumulated on the plate interface was about 20 MPa near the trench and 0–10 MPa in the down‐dip source region.