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Some Seismological Aspects of the 1999 Chi-Chi Earthquake in Taiwan

1999年台灣集集大地震-地震綜觀

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並列摘要


The Chi-Chi earthquake is the largest inland earthquake in Taiwan during the 20th century. It caused severe damage in central Taiwan. Three possible induced earthquakes triggered by a mainshock are being examined from the strong ground motion data. The occurrence of these three-triggered events can be used to explain the difference between preliminary isoseismal map, based on the real-time data, and final one. They can also explain why a wide area of aftershock distribution Was observed. On the other hand, the overshooting of ground motion at those stations located near the northern end of Chelungpu fault is probably the reason for the complex surface rupture observed between FengYuan and TungShih.

被引用紀錄


陳明湖(2005)。地震災損評估系統應用於地區災害防救計劃之研究〔碩士論文,國立臺北科技大學〕。華藝線上圖書館。https://doi.org/10.6841/NTUT.2005.00227
趙子凱(2000)。集集地震前後震波衰減強度變化之研究〔碩士論文,國立臺灣師範大學〕。華藝線上圖書館。https://www.airitilibrary.com/Article/Detail?DocID=U0021-2603200719104766
曾詠棠(2001)。921集集地震前後t*之時空變化研究〔碩士論文,國立臺灣師範大學〕。華藝線上圖書館。https://www.airitilibrary.com/Article/Detail?DocID=U0021-2603200719113340

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