Observation of surface displacements from GPS analyses before and after the Jiashian earthquake (M=6.4) in Taiwan

NCUIR > College of Earth Sciences > Department of Earth Sciences > journal & Dissertation > Item 987654321/103891

Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/103891

Title:	Observation of surface displacements from GPS analyses before and after the Jiashian earthquake (M=6.4) in Taiwan
Authors:	顏宏元;Chen, Chieh-Hung;Wen, Strong;Yeh, Ta-Kang;Wang, Chung-Ho;Yen, Horng-Yuan;Liu, Jann-Yenq;Hobara, Yasuhide;Han, Peng
Contributors:	地球科學學院地球科學學系
Keywords:	Global positioning system;Hilbert–Huang transform;Jiashian earthquake
Date:	2013-01-30
Issue Date:	2026-04-23 11:39:17 (UTC+8)
Publisher:	Elsevier Ltd.;Elsevier Ltd
Abstract:	摘要： ► We used 100GPS stations to examine changes of surface displacements. ► Our results suggest stress accumulation before the mainshock. ► GPS horizontal displacements agree with distribution of aftershocks. ► Surface displacements triggered by a blind thrust fault can be recorded using GPS. A blind thrust fault with a unique strike, which is orthogonal to the strike of most tectonic structures in Taiwan, triggered the Jiashian earthquake on March 4, 2010 (M=6.4; 22.96°N, 120.70°E). This study utilizes 100 global positioning system stations to examine changes of surface displacements during the Jiashian earthquake. We mitigate effects of short-term noise and long-term plate movements from surface displacement data using a frequency dependent filter via the Hilbert–Huang transform and compute the horizontal azimuth (i.e. GPS-azimuth) using residual data at the NS component relative to residual data at the EW component. Analytical results show that orientations of horizontal azimuths were aligned and orthogonal to the strike of the blind thrust fault. Meanwhile, inverse orientations are observed before and after the earthquake that agrees well with the seismic rebound theory. As stress disturbed on strata a few days before the earthquake, an impeded region can be clearly identified by disordered orientations of horizontal azimuths for anticipating the mainshock. These results provide an additional view to explore stress disturbance associated with earthquakes and offer more information to examine diverse models of tectonic evolution in this region. 出版者： Elsevier Ltd 出版日期： 2013-01-30 出處： Journal of Asian earth sciences, 2013-01, Vol.62, p.662-671 資源來源： Elsevier ScienceDirect Journals Complete 版權： 2012 Elsevier Ltd 識別號： ISSN: 1367-9120 識別號： EISSN: 1878-5786 識別號： DOI: 10.1016/j.jseaes.2012.11.016
Appears in Collections:	[Department of Earth Sciences ] journal & Dissertation

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