English  |  正體中文  |  简体中文  |  Items with full text/Total items : 26994/38795
Visitors : 2392402      Online Users : 69
RC Version 4.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
Scope Adv. Search
LoginUploadHelpAboutAdminister

Please use this identifier to cite or link to this item: http://ntour.ntou.edu.tw:8080/ir/handle/987654321/40605

Title: Simulation for Near Source Two-Dimensional Wave Field and its Application to the Study of Ground Motion Characteristics of the 1999 Chi-Chi, Taiwan Earthquake
Authors: Kuo-Liang Wen
Yi-Ling Huang
Bor-Shouh Huang
Contributors: 國立臺灣海洋大學:應用地球科學研究所
Keywords: Near source two-dimensional strong ground-mption
Temporal and spatial distribution snapshots of ground-motion
The Chi-Chi earthquake
Date: 2004-03
Issue Date: 2017-02-06T01:14:00Z
Publisher: Terrestrial, Atmospheric and Oceanic Sciences
Abstract: Abstract: The characteristics of near source two-dimensional strong ground-motion resulting from complex fault rupture processes and velocity structures have been examined based on two-dimensional wave field modeling. To construct the two-dimensional surface seismic wave field, the synthetic seismogram of each grid space was simulated by theoretical Green¡¦s functions. Numerical experiments were constructed by testing different source parameters and velocity structures. The analysis undertaken in this study can be considered as a two-dimensional seismic waveform analysis and offered as a wider view for studying the wave propagation from a large earthquake. Results of this study provide significant information about the temporal and spatial wave field snapshots on the near source area. It is found that the wave fields are strongly affected by the changes of fault geometries, rupture velocities and near fault seismic velocity structures. In this study, the newly developed wave field simulation procedure is applied to analyze the near source ground motion characteristics of the 1999 Chi-chi, Taiwan earthquake. Summing up the modeling results and comparing with the observed near source wave field of the Chi-chi earthquake, we find that the Chelungpu fault has lower seismic velocity in the footwall than in the hanging wall, and seismic velocities of the footwall side, at least on its surface, are lower than its apparent rupture velocities.
Relation: 15(1)
URI: http://ntour.ntou.edu.tw:8080/ir/handle/987654321/40605
Appears in Collections:[應用地球科學研究所] 期刊論文

Files in This Item:

File Description SizeFormat
index.html0KbHTML39View/Open


All items in NTOUR are protected by copyright, with all rights reserved.

 


著作權政策宣告: 本網站之內容為國立臺灣海洋大學所收錄之機構典藏,無償提供學術研究與公眾教育等公益性使用,請合理使用本網站之內容,以尊重著作權人之權益。
網站維護: 海大圖資處 圖書系統組
DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - Feedback