Earthquake Magnitudes Based on Coda-Derived Source Spectra in Taiwan

碩士 === 國立臺灣大學 === 地質科學研究所 === 99 === We apply the coda-derived source spectrum method to estimate earthquake magnitudes in Taiwan. 76 events occurred during the time period from 1996 to 2010 around west-south Taiwan recorded by BATS (Broadband Array in Taiwan for Seismology) with magnitudes between...

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Main Authors: Feng-Shan Tu, 涂鳳珊
Other Authors: 龔源成
Format: Others
Language:zh-TW
Published: 2011
Online Access:http://ndltd.ncl.edu.tw/handle/55114757034282242900
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spelling ndltd-TW-099NTU051381442015-10-16T04:03:10Z http://ndltd.ncl.edu.tw/handle/55114757034282242900 Earthquake Magnitudes Based on Coda-Derived Source Spectra in Taiwan 利用地震尾波估算震源頻譜 Feng-Shan Tu 涂鳳珊 碩士 國立臺灣大學 地質科學研究所 99 We apply the coda-derived source spectrum method to estimate earthquake magnitudes in Taiwan. 76 events occurred during the time period from 1996 to 2010 around west-south Taiwan recorded by BATS (Broadband Array in Taiwan for Seismology) with magnitudes between Mw 3.2 and 6.21 are used in this study. From two horizontal components of waveform data, we extract the coda envelopes at 12 frequency bands between 0.05 and 8.0 Hz. We construct the synthetic coda-envelope by using various empirical distance-frequency-dependent corrections. The derived synthetic coda envelops are compared to the observed coda-envelope to evaluate the dimensionless coda amplitudes. With further considerations on path effects, site effects and source-to-coda transfer functions, the dimensionless coda amplitudes at each frequency band are used to construct the source spectra, which is then used to determine the earthquake magnitudes. The 76 derived coda-magnitudes (MC) are consistent with corresponding moment magnitudes (Mw). Our result also shows the overall deviations between MC and local magnitude (ML) reported from Central Weather Bureau are less than those between Mw and ML. While the implications need further investigation, the results indicate that the broad-band coda information does reconcile, to some extent, the long-lasting discrepancy between the low frequency magnitude (Mw) and the high frequency magnitude (ML) in Taiwan. Moreover, we found out that there is a very stable linear relationship between coda-derived source amplitudes at 2.5 Hz and the ML scale, implying that the source information is well maintained by the high-frequency coda, and this property shows it is potentially very feasible to extend this method to smaller earthquakes in Taiwan. 龔源成 2011 學位論文 ; thesis 77 zh-TW
collection NDLTD
language zh-TW
format Others
sources NDLTD
description 碩士 === 國立臺灣大學 === 地質科學研究所 === 99 === We apply the coda-derived source spectrum method to estimate earthquake magnitudes in Taiwan. 76 events occurred during the time period from 1996 to 2010 around west-south Taiwan recorded by BATS (Broadband Array in Taiwan for Seismology) with magnitudes between Mw 3.2 and 6.21 are used in this study. From two horizontal components of waveform data, we extract the coda envelopes at 12 frequency bands between 0.05 and 8.0 Hz. We construct the synthetic coda-envelope by using various empirical distance-frequency-dependent corrections. The derived synthetic coda envelops are compared to the observed coda-envelope to evaluate the dimensionless coda amplitudes. With further considerations on path effects, site effects and source-to-coda transfer functions, the dimensionless coda amplitudes at each frequency band are used to construct the source spectra, which is then used to determine the earthquake magnitudes. The 76 derived coda-magnitudes (MC) are consistent with corresponding moment magnitudes (Mw). Our result also shows the overall deviations between MC and local magnitude (ML) reported from Central Weather Bureau are less than those between Mw and ML. While the implications need further investigation, the results indicate that the broad-band coda information does reconcile, to some extent, the long-lasting discrepancy between the low frequency magnitude (Mw) and the high frequency magnitude (ML) in Taiwan. Moreover, we found out that there is a very stable linear relationship between coda-derived source amplitudes at 2.5 Hz and the ML scale, implying that the source information is well maintained by the high-frequency coda, and this property shows it is potentially very feasible to extend this method to smaller earthquakes in Taiwan.
author2 龔源成
author_facet 龔源成
Feng-Shan Tu
涂鳳珊
author Feng-Shan Tu
涂鳳珊
spellingShingle Feng-Shan Tu
涂鳳珊
Earthquake Magnitudes Based on Coda-Derived Source Spectra in Taiwan
author_sort Feng-Shan Tu
title Earthquake Magnitudes Based on Coda-Derived Source Spectra in Taiwan
title_short Earthquake Magnitudes Based on Coda-Derived Source Spectra in Taiwan
title_full Earthquake Magnitudes Based on Coda-Derived Source Spectra in Taiwan
title_fullStr Earthquake Magnitudes Based on Coda-Derived Source Spectra in Taiwan
title_full_unstemmed Earthquake Magnitudes Based on Coda-Derived Source Spectra in Taiwan
title_sort earthquake magnitudes based on coda-derived source spectra in taiwan
publishDate 2011
url http://ndltd.ncl.edu.tw/handle/55114757034282242900
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