Strong motion records at K-NET and KiK-net stations for earthquakes which occurred in the mid Niigata area are analyzed to examine the relationship between the amplitude of the short-period source spectrum and the seismic moment. Large earthquakes radiate more short-period seismic energy per unit seismic moment than small ones, which suggests a deviation from the similarity of earthquake source. Appropriate correction for the deviation from the similarity should be made when we synthesize strong ground motion for future large earthquakes by the empirical Green's function method.ArticleEARTH PLANETS AND SPACE. 59(4): 301-305 (2007)journal articl
We analyzed four pairs of a large (M_w ≈ 6) and a small (M_w ≈ 3.5 to 4) shallow strike-slip earthqu...
We analyzed four pairs of a large (M_w ≈ 6) and a small (M_w ≈ 3.5 to 4) shallow strike-slip earthqu...
Earthquake (Mw 9.0) is estimated from a comparison of the observed records of the mainshock and synt...
Strong motion records at K-NET and KiK-net stations for earthquakes which occurred in the mid Niigat...
Strong motion records at K-NET and KiK-net stations for earthquakes which occurred in the mid Niigat...
The Mid Niigata earthquake of October 23, 2004, is a shallow reverse-faulting event with M-w = 6.6. ...
The Mid Niigata earthquake of October 23, 2004, is a shallow reverse-faulting event with M-w = 6.6. ...
Main-shock earthquakes are followed by numerous aftershocks which aggravate damages to structures an...
A two-stage scaling relationship of the source parameters for crustal earthquakes in Japan has previ...
We determined m^b, the body-wave magnitude calculated from the maximum amplitude of short-period P w...
We considered the large ground motion Japanese database and statistically analyzed the differences b...
We determined m^b, the body-wave magnitude calculated from the maximum amplitude of short-period P w...
We analyzed four pairs of a large (M-w approximate to 6) and a small (M-w approximate to 3.5 to 4) s...
The relationship between the S-wave spectrum and earthquake magnitude can be obtained by analysis of...
In this integrated study, ground-motion characteristics of one of the most devastating earthquakes i...
We analyzed four pairs of a large (M_w ≈ 6) and a small (M_w ≈ 3.5 to 4) shallow strike-slip earthqu...
We analyzed four pairs of a large (M_w ≈ 6) and a small (M_w ≈ 3.5 to 4) shallow strike-slip earthqu...
Earthquake (Mw 9.0) is estimated from a comparison of the observed records of the mainshock and synt...
Strong motion records at K-NET and KiK-net stations for earthquakes which occurred in the mid Niigat...
Strong motion records at K-NET and KiK-net stations for earthquakes which occurred in the mid Niigat...
The Mid Niigata earthquake of October 23, 2004, is a shallow reverse-faulting event with M-w = 6.6. ...
The Mid Niigata earthquake of October 23, 2004, is a shallow reverse-faulting event with M-w = 6.6. ...
Main-shock earthquakes are followed by numerous aftershocks which aggravate damages to structures an...
A two-stage scaling relationship of the source parameters for crustal earthquakes in Japan has previ...
We determined m^b, the body-wave magnitude calculated from the maximum amplitude of short-period P w...
We considered the large ground motion Japanese database and statistically analyzed the differences b...
We determined m^b, the body-wave magnitude calculated from the maximum amplitude of short-period P w...
We analyzed four pairs of a large (M-w approximate to 6) and a small (M-w approximate to 3.5 to 4) s...
The relationship between the S-wave spectrum and earthquake magnitude can be obtained by analysis of...
In this integrated study, ground-motion characteristics of one of the most devastating earthquakes i...
We analyzed four pairs of a large (M_w ≈ 6) and a small (M_w ≈ 3.5 to 4) shallow strike-slip earthqu...
We analyzed four pairs of a large (M_w ≈ 6) and a small (M_w ≈ 3.5 to 4) shallow strike-slip earthqu...
Earthquake (Mw 9.0) is estimated from a comparison of the observed records of the mainshock and synt...