首页|1999年台湾集集MW7.6地震跨断层场地相对运动

1999年台湾集集MW7.6地震跨断层场地相对运动

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为了获得近断层地震动准确的残余位移信息,提出了一种变步长网格搜索地震动基线校正方法.首先基于 1999 年我国台湾MW7.6 集集地震强震动数据,探讨了近断层地震动的位移特征,然后通过地震动时程初始时刻的校正获得了集集地震多组上、下盘台站之间的相对运动时程数据,分析了分别靠近断层上、下盘场地之间相对运动的位移时程特征.结果显示:近断层地震动的滑冲效应显著,断层的平均滑冲速度可高达 1.4 m/s;断层两盘间的相对运动类似于近断层地震动的运动特征,且幅值更大;近断层的残余位移约是断层两盘间最大相对位移的80%.
Relative motions between cross-fault sites resultd from the 1999 MW7.6 Taiwan Chi-Chi earthquake
In order to obtain more accurate residual displacement information generated by near-fault ground motion,this paper proposed a variable step-grid search method for ground motion baseline correction.The core of this method lies in preserving and accurately reflecting the residual displacement information of faults,and solving the problem of extremely low com-putational efficiency in traditional grid search methods when there are many digital seismic sampling points.Based on the strong ground motion data of the 1999 MW7.6 Chi-Chi earth-quake in Taiwan region,this paper uses the variable step-grid search method for ground motion baseline correction to conduct in-depth research on the ground motion displacement characterist-ics near faults.By accurately correcting the initial moment of ground motion time history,this study successfully obtained relative ground motion time history data between multiple sets of the hanging and foot wall stations in the Chi-Chi earthquake.And based on this data,the displace-ment time history characteristics of the relative motion between the hanging and foot wall sites near the fault were analyzed.The research results indicate that the fling-step effect of ground motion is particularly significant in the Chi-Chi earthquake.The maximum displacement and residual displacement of near fault ground motion exceed 8 m and 6 m,respectively,and the average sliding velocity of the fault is as high as 1.4 m/s,fully demonstrating the strong destru-ctive force of the earthquake.This poses challenges to the numerical simulation of fault rupture and related experimental researches.In addition,the relative motion between fault walls also exhibits similar motion characteristics to near fault ground motion,and its amplitude is larger.Therefore,the relative motion data between earthquake fault walls can refer to the time history of near fault ground motion as the input basis for engineering design and analysis.In addition,the residual displacement of the fault is about 80%of the maximum relative displacement between the fault walls.This study provides important information on residual displacement of fault ground motion,which is of great significance to the researches on fields such as earth-quake engineering,earthquake warning,and disaster assessment.

1999 MW7.6 Chi-Chi earthquakenear-fault ground motionscross-fault siterelative movementfaulting

徐龙军、吕淼、张恒、于越、谢礼立

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中国武汉 430056 江汉大学精细爆破国家重点实验室

中国 山东威海 264209 哈尔滨工业大学(威海)土木工程系

中国哈尔滨 150080 中国地震局工程力学研究所

中国哈尔滨 150080 中国地震局地震工程与工程振动重点实验室

美国加利福尼亚州 94305 斯坦福大学土木与环境工程系

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1999年集集MW7.6地震 近断层地震动 跨断层场地 相对运动 断层作用

国家自然科学基金委员会-中国地震局地震科学联合基金湖北省自然科学基金(创新群体)重点项目

U21392072023AFA030

2024

地震学报
中国地震学会 中国地震局地球物理研究所

地震学报

CSTPCD北大核心
影响因子:1.186
ISSN:0253-3782
年,卷(期):2024.46(3)