Studies on Aftershocks in Taiwan: A Review

We reviewed studies on aftershocks in Taiwan for the following topics: the spatial-temporal distributions and focal-plane solutions of aftershocks fromof thirty larger earthquakes with magnitudes > 5; the correlations between the mainshock and the largest aftershock based on dependence of the dif...

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Main Authors: Jeen-Hwa Wang, Kou-Cheng Chen, Peih-Lin Leu, Chien-Hsin Chang
Format: Article
Language:English
Published: Chinese Geoscience Union 2016-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Online Access: http://tao.cgu.org.tw/media/k2/attachments/v276p769.pdf
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spelling doaj-29d81222da39490785d066664445c37a2020-11-25T00:26:12ZengChinese Geoscience UnionTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802016-01-0127676910.3319/TAO.2016.09.12.01Studies on Aftershocks in Taiwan: A ReviewJeen-Hwa WangKou-Cheng ChenPeih-Lin LeuChien-Hsin ChangWe reviewed studies on aftershocks in Taiwan for the following topics: the spatial-temporal distributions and focal-plane solutions of aftershocks fromof thirty larger earthquakes with magnitudes > 5; the correlations between the mainshock and the largest aftershock based on dependence of the differences in magnitudes (ΔM), occurrence times (ΔT), epicenters (ΔH), and focal depths (ΔD) upon the mainshock magnitude, Mm; magnitude-dependence of p-value of Omori’s law of aftershocks; the correlation between the b-value of the Gutenberg-Richter’s frequency-magnitude law and the p-value; application of the epidemic-type aftershock sequences (ETAS) model to describe the aftershock sequence; the mechanisms of triggering aftershocks; and dynamic modeling of aftershocks. The main results are: (1) The spatial distribution of aftershocks for some earthquakes is consistent with the recognized fault; (2) Unlike Båth’s law, ΔM slightly increases with Mm; (3) ΔT does not correlate with Mm; (4) ΔD does not correlate with Mm; (5) ΔT somewhat increases with ΔD; (6) The p-value slightly increases with Mm; (7) There is a negative correlation between the b- and p-values. (8) There was seismic quiescence over a broader region of Taiwan before the 1999 Chi-Chi earthquake; (9) Both the static and dynamic stress changes trigger aftershocks; and (10) Dynamic modeling shows that a decrease in elastic modulus is a significant factor in triggering aftershocks. http://tao.cgu.org.tw/media/k2/attachments/v276p769.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Jeen-Hwa Wang
Kou-Cheng Chen
Peih-Lin Leu
Chien-Hsin Chang
spellingShingle Jeen-Hwa Wang
Kou-Cheng Chen
Peih-Lin Leu
Chien-Hsin Chang
Studies on Aftershocks in Taiwan: A Review
Terrestrial, Atmospheric and Oceanic Sciences
author_facet Jeen-Hwa Wang
Kou-Cheng Chen
Peih-Lin Leu
Chien-Hsin Chang
author_sort Jeen-Hwa Wang
title Studies on Aftershocks in Taiwan: A Review
title_short Studies on Aftershocks in Taiwan: A Review
title_full Studies on Aftershocks in Taiwan: A Review
title_fullStr Studies on Aftershocks in Taiwan: A Review
title_full_unstemmed Studies on Aftershocks in Taiwan: A Review
title_sort studies on aftershocks in taiwan: a review
publisher Chinese Geoscience Union
series Terrestrial, Atmospheric and Oceanic Sciences
issn 1017-0839
2311-7680
publishDate 2016-01-01
description We reviewed studies on aftershocks in Taiwan for the following topics: the spatial-temporal distributions and focal-plane solutions of aftershocks fromof thirty larger earthquakes with magnitudes > 5; the correlations between the mainshock and the largest aftershock based on dependence of the differences in magnitudes (ΔM), occurrence times (ΔT), epicenters (ΔH), and focal depths (ΔD) upon the mainshock magnitude, Mm; magnitude-dependence of p-value of Omori’s law of aftershocks; the correlation between the b-value of the Gutenberg-Richter’s frequency-magnitude law and the p-value; application of the epidemic-type aftershock sequences (ETAS) model to describe the aftershock sequence; the mechanisms of triggering aftershocks; and dynamic modeling of aftershocks. The main results are: (1) The spatial distribution of aftershocks for some earthquakes is consistent with the recognized fault; (2) Unlike Båth’s law, ΔM slightly increases with Mm; (3) ΔT does not correlate with Mm; (4) ΔD does not correlate with Mm; (5) ΔT somewhat increases with ΔD; (6) The p-value slightly increases with Mm; (7) There is a negative correlation between the b- and p-values. (8) There was seismic quiescence over a broader region of Taiwan before the 1999 Chi-Chi earthquake; (9) Both the static and dynamic stress changes trigger aftershocks; and (10) Dynamic modeling shows that a decrease in elastic modulus is a significant factor in triggering aftershocks.
url http://tao.cgu.org.tw/media/k2/attachments/v276p769.pdf
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