Strong Ground Motion Attenuation Relationships for Subduction Zone Earthquakes

1997 ◽  
Vol 68 (1) ◽  
pp. 58-73 ◽  
Author(s):  
R. R. Youngs ◽  
S.- J. Chiou ◽  
W. J. Silva ◽  
J. R. Humphrey
2011 ◽  
Vol 382 ◽  
pp. 7-11
Author(s):  
Zheng Ru Tao ◽  
Xia Xin Tao ◽  
Xi Wei Wang

For regions without adequate strong ground motion records, a method is developed to establish strong ground motion attenuation relationships, based on the stochastic method. Sendai area of Japan is selected as the target, since there are enough data from seismographic observation for calculation, and those from strong ground motion observation and some empirical relationships for result testing. Three parameters related to regional source and crustal medium are inversed by the micro-Genetic Algorithm. Total of 240 records from 77 small events, recorded by F-net, are adopted for the inversion. Fourier spectra are adopted as the objective function. These parameters are then taken into the stochastic method to estimate PGA. The regional ground motion attenuation relationships are compared with some strong ground motion records from K-NET and some empirical relationships to illustrate the reliability of this method.


2006 ◽  
Vol 62 (4) ◽  
pp. 877-890
Author(s):  
Atsushi NOZU ◽  
Shogo MIYAJIMA ◽  
Go NAKANISHI ◽  
Masayuki YAMADA

1988 ◽  
Vol 4 (3) ◽  
pp. 635-646 ◽  
Author(s):  
J. G. Anderson ◽  
R. Quaas

The Guerrero digital accelerograph network has been operating, since spring of 1985, on rock sites along the coast of Mexico, above an active subduction zone. The accelerograms collected through June 1987 include examples from events with magnitudes from 3 to 8, all recorded at nearly the same hypocentral distance. Spectra from these accelerograms scale in a manner that is qualitatively consistent with earthquake source theory. Based on four selected events, peak accelerations attenuate more rapidly for small events than for large events.


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