摘要
SAR interferograms have successfully determined the detailed coseismic displacements in the footwall block of the Chelungpu fault during the Mw 7.6 Chi-Chi earthquake in Taiwan on September 21,1999 (local time). Based on the 3D dislocation model of faults, we infer the preliminary rupturing behavior - a segmented rupturing process - of the Chelungpu thrust from recent SAR interferograms. A key argument controlling the rupture of the Chelungpu thrust may be the recognized segments with different sliding depths of Chinshui Shale.
原文 | ???core.languages.en_GB??? |
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頁(從 - 到) | 241-247 |
頁數 | 7 |
期刊 | Terrestrial, Atmospheric and Oceanic Sciences |
卷 | 14 |
發行號 | 2 |
DOIs | |
出版狀態 | 已出版 - 6月 2003 |