Citation

Furumura T, Takemura S, Noguchi S, Takemoto T, Maeda T, Iwai K, Padhy S. Landslides 2011; 8(3): 333-338.

Copyright

(Copyright © 2011, Holtzbrinck Springer Nature Publishing Group)

DOI

10.1007/s10346-011-0279-3

PMID

unavailable

Abstract

The dense recordings of the K-NET and KiK-net nationwide strong motion network of 1,189 accelerometers show clearly the radiation and propagation properties of the strong ground motions associated with the 2011 off-the-Pacific Coast-of-Tohoku, Japan (Mw = 9.0) earthquake. The snapshots of seismic wave propagation reveal strong ground motions from this earthquake that originate from three large slips; the first two slips occurred over the plate interface of off-Miyagi at the southwest and the east of the hypocenter, and the third one just beneath the northern end of Ibaraki over the plate interface or in the crust. Such multiple shocks of this event caused large accelerations (maximum 1-2 G) and prolonged ground shaking lasting several minutes with dominant high-frequency ( T < 1 s) signals over the entire area of northern Japan. On the other hand, ground motions of relatively longer-period band ( T = 1-2 s), which caused significant damage to wooden-frame houses, were about 1/2-1/3 of those observed near the source area of the destructive 1995 Kobe, Japan (M = 7.3) earthquake. Also, the long-period ( T = 6-8 s) ground motion in the Kanto (Tokyo) sedimentary basin was at an almost comparable level of those observed during the recent Mw = 7 inland earthquakes, but not as large as that from the former M = 8 earthquakes. Therefore, the impact of the strong ground motion from the present M = 9 earthquake was not as large as expected from the previously M = 7-8 earthquakes and caused strong motion damage only to short-scale construction and according to instruments inside the buildings, both have a shorter ( T < 1 s) natural period.