Access count of this item: 138

Files in This Item:
File Description SizeFormat 
0120080257.pdf1.47 MBAdobe PDFView/Open
Title: Source Rupture Process of the 2004 Chuetsu, Mid-Niigata Prefecture, Japan, Earthquake Inferred from Waveform Inversion with Dense Strong-Motion Data
Authors: Asano, Kimiyuki  kyouindb  KAKEN_id  orcid https://orcid.org/0000-0002-8530-4198 (unconfirmed)
Iwata, Tomotaka  kyouindb  KAKEN_id
Author's alias: 浅野, 公之
Issue Date: 1-Feb-2009
Publisher: Seismological Society of America
Journal title: Bulletin of the Seismological Society of America
Volume: 99
Issue: 1
Start page: 123
End page: 140
Abstract: The kinematic source rupture process of the 2004 Chuetsu, mid-Niigata prefecture, Japan, earthquake, is estimated from strong-motion data by the linear waveform inversion method. In order to develop appropriate Green’s functions, one-dimensional velocity structure models for each station are constructed by modeling the aftershock waveforms. The estimated top of the bedrock is deeper at the western side of the fault and relatively shallow at the eastern side. This tendency coincides with other investigations of seismic tomography and microtremor array observations. The obtained source model shows large slips in the vicinity of the hypocenter. The reverse slipping rupture originated from the deeper part of the fault and propagated toward the up-dip and southwest directions. The near-surface slip is small. Two tests are demonstrated to check the stability of the obtained source model. The first test examines the effects of the number of available stations on the solution, and the second test examines how the difference in the target waveform type affects the solution. The number of stations affects the variation of slip amount, and more than 12 stations appear to be sufficient to obtain a stable solution in this case. The difference in the target wave type in the data set does not significantly affect the solution if the number of stations is sufficient and the Green’s functions are well calibrated. The model obtained using calibrated velocity structure models shows clear image of high-slip area compared to the model obtained using a single velocity structure model.
Rights: This copy is for distribution only by the authors of the article and their institutions in accordance with the Open Access Policy of the Seismological Society of America.
URI: http://hdl.handle.net/2433/209746
DOI(Published Version): 10.1785/0120080257
Appears in Collections:Journal Articles

Show full item record

Export to RefWorks


Export Format: 


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.