Comparison study on the coseismic deformation of the 1999 Chi-Chi earthquake and long-term stream gradient changes along the chelungpu fault in central Taiwan

Quocheng Sung, Yen Che Chen, Hen Tsai, Yue Gau Chen, Wen Shan Chen

Research output: Contribution to journalArticle

13 Citations (Scopus)

Abstract

The largest inland earthquake (ML=7.3) of the 20th century in Taiwan occurred at 0147hrs local time on 21 September, 1999 near the small town of Chi-Chi, in central Taiwan. The crustal deformation pattern, caused by the Ch-Chi earthquake, appears to be unrelated to the velocity field that GPS stations measured in the period 1992 to 1995. It exhibits a greater horizontal and vertical slip in the northern block between the Tachia River and the Wu River than in the southern block between the Wu River and the Tzoshui River. This study compares the stream profiles of three rivers in central Taiwan, namely the Tachia, Wu and Tzoshui Rivers, which run westward across the Shuilikeng fault, the Shuangtung fault, the Chelungpu fault and the Changhwa fault. Historical change of stream gradient is retrieved by a comparison of previous maps published by the Japanese authorities in 1904 and produced by the Department of Interior, ROC in 1985. The results, simulated by the diffusion model, indicate that the changes are attributable to the crustal movement in this area over the past 80 years. It is concluded that crustal deformation has been more evident in the block between the Tachia River and the Wu River than that between the Wu River and the Tzoshui River. This result agrees with the faulting net slip caused by the Chi-Chi earthquake. The method used in this study has been verified as a feasible tool in the research of earthquake prediction and seismic hazard assessment. Further studies are necessary in such a tectonically active area as Taiwan.

Original languageEnglish
Pages (from-to)735-750
Number of pages16
JournalTerrestrial, Atmospheric and Oceanic Sciences
Volume11
Issue number3
DOIs
Publication statusPublished - 2000 Jan 1

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Chi-Chi earthquake 1999
river
crustal deformation
earthquake
comparison
crustal movement
earthquake prediction
small town
hazard assessment
seismic hazard
faulting
GPS

All Science Journal Classification (ASJC) codes

  • Oceanography
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)

Cite this

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title = "Comparison study on the coseismic deformation of the 1999 Chi-Chi earthquake and long-term stream gradient changes along the chelungpu fault in central Taiwan",
abstract = "The largest inland earthquake (ML=7.3) of the 20th century in Taiwan occurred at 0147hrs local time on 21 September, 1999 near the small town of Chi-Chi, in central Taiwan. The crustal deformation pattern, caused by the Ch-Chi earthquake, appears to be unrelated to the velocity field that GPS stations measured in the period 1992 to 1995. It exhibits a greater horizontal and vertical slip in the northern block between the Tachia River and the Wu River than in the southern block between the Wu River and the Tzoshui River. This study compares the stream profiles of three rivers in central Taiwan, namely the Tachia, Wu and Tzoshui Rivers, which run westward across the Shuilikeng fault, the Shuangtung fault, the Chelungpu fault and the Changhwa fault. Historical change of stream gradient is retrieved by a comparison of previous maps published by the Japanese authorities in 1904 and produced by the Department of Interior, ROC in 1985. The results, simulated by the diffusion model, indicate that the changes are attributable to the crustal movement in this area over the past 80 years. It is concluded that crustal deformation has been more evident in the block between the Tachia River and the Wu River than that between the Wu River and the Tzoshui River. This result agrees with the faulting net slip caused by the Chi-Chi earthquake. The method used in this study has been verified as a feasible tool in the research of earthquake prediction and seismic hazard assessment. Further studies are necessary in such a tectonically active area as Taiwan.",
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Comparison study on the coseismic deformation of the 1999 Chi-Chi earthquake and long-term stream gradient changes along the chelungpu fault in central Taiwan. / Sung, Quocheng; Chen, Yen Che; Tsai, Hen; Chen, Yue Gau; Chen, Wen Shan.

In: Terrestrial, Atmospheric and Oceanic Sciences, Vol. 11, No. 3, 01.01.2000, p. 735-750.

Research output: Contribution to journalArticle

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AU - Sung, Quocheng

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AU - Chen, Yue Gau

AU - Chen, Wen Shan

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AB - The largest inland earthquake (ML=7.3) of the 20th century in Taiwan occurred at 0147hrs local time on 21 September, 1999 near the small town of Chi-Chi, in central Taiwan. The crustal deformation pattern, caused by the Ch-Chi earthquake, appears to be unrelated to the velocity field that GPS stations measured in the period 1992 to 1995. It exhibits a greater horizontal and vertical slip in the northern block between the Tachia River and the Wu River than in the southern block between the Wu River and the Tzoshui River. This study compares the stream profiles of three rivers in central Taiwan, namely the Tachia, Wu and Tzoshui Rivers, which run westward across the Shuilikeng fault, the Shuangtung fault, the Chelungpu fault and the Changhwa fault. Historical change of stream gradient is retrieved by a comparison of previous maps published by the Japanese authorities in 1904 and produced by the Department of Interior, ROC in 1985. The results, simulated by the diffusion model, indicate that the changes are attributable to the crustal movement in this area over the past 80 years. It is concluded that crustal deformation has been more evident in the block between the Tachia River and the Wu River than that between the Wu River and the Tzoshui River. This result agrees with the faulting net slip caused by the Chi-Chi earthquake. The method used in this study has been verified as a feasible tool in the research of earthquake prediction and seismic hazard assessment. Further studies are necessary in such a tectonically active area as Taiwan.

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