李家峡水库蓄水后区域地震活动特征及危险性分析
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摘要
根据李家峡水库地震台网 1 998— 2 0 0 2年的地震目录 ,分析了水库蓄水后库坝区和周边研究区的地震活动特征 ,并对未来水库地震的危险性进行了定量评价。分析结果表明 :李家峡水库蓄水以来 ,库坝区 90 %的地震为 0 .0～ 1 .9级的弱小地震 ,且地震活动与水库水位有关 ,相对于水位升高存在 5～ 7个月的滞后期 ;研究区以 1 .0～1 .9级地震为主 ,地震活跃程度呈间息式变化 ,地震月频次呈阶跃式变化。应用经验判别法的预测结果表明 ,未来李家峡水库库坝区存在诱发 5级以上灾害性地震的危险性 ,最大震级在 5 .0～ 5 .4级之间
The present paper has done an analysis and study on the characteristics of earthquakes that have occurred in Lijiaxia reservoir region in the Yellow River Basin in recent years based on statistics and data collected by a seismic network of from May 1998 to December 2002. The riskness of the reservoir seismicity in future is also predicated. The results obtained show that since Lijiaxia is water-filled in 1997, M_L 0-1.9 earthquakes accounts up 90% of the total earthquakes in the reservoir region. Furthermore, these microseismicities prove to be closely connected with the water level of the reservoir and have a 5-7 months lag with changes of the water level. The main magnitude of earthquakes in the studied region is M_L 1.0-1.9, and seismicity frequency is sultant. As predicated, the destructive shock would occur in Lijiaxia reservoir and the largest magnitude of reservoir earthquake in future is M_L 5.0-5.4.
The present paper has done an analysis and study on the characteristics of earthquakes that have occurred in Lijiaxia reservoir region in the Yellow River Basin in recent years based on statistics and data collected by a seismic network of from May 1998 to December 2002. The riskness of the reservoir seismicity in future is also predicated. The results obtained show that since Lijiaxia is water-filled in 1997, M_L 0-1.9 earthquakes accounts up 90% of the total earthquakes in the reservoir region. Furthermore, these microseismicities prove to be closely connected with the water level of the reservoir and have a 5-7 months lag with changes of the water level. The main magnitude of earthquakes in the studied region is M_L 1.0-1.9, and seismicity frequency is sultant. As predicated, the destructive shock would occur in Lijiaxia reservoir and the largest magnitude of reservoir earthquake in future is M_L 5.0-5.4.
引文
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[13]ChangBaoqi(常宝琦) andLiangJibin(梁纪彬).Prediction ofmaximum magnitude of reservoir induced seismicity[J].SourthChinaEarthquake(华南地震),1992,12(1):74～9
[2] GuptaH K.The present status of reservoir induced seismicityinvestigation with special emphasisonKosyna earthquake[J].Tectonophysics,1985,118:287～279
[3] XiaQifa(夏其发).Assessment of reservoir induced earthquake[J].TheChineseJournal ofGeologicalH azard andControl(中国地质灾害与防治学报),2000,11(2):39～45
[4] YangQingyuan(杨清源),DaiLisi(戴丽思),ChenXiancheng(陈献程),et al.Ground motion character of reservoirearthquakes[J].N orthwesternSeismologicalJournal(西北地震学报),1997,19(1):64～69
[5] ZhangWenfu(张文甫).Prediction and assessment of inducedearthquake of reservoirs[J].SichuanWaterPower(四川水力发电),2000,19(2):86～88,92
[6] DingYuanzhang(丁原章),ChangBaoqi(常宝琦),XiaoAnyu(肖安予),etal.EarthquakeInduced byReservior(水库诱发地震)[M].Beijing:SeismologicalPress,1989
[7] GuGongxu(顾功叙).Catalog ofEarthquake inChina(中国地震目录)[M].Beijing:SciencePress,1983
[8] EditorBoard ofEarthquakeAnnals ofChina(中国地震年鉴编辑部).EarthquakeAnnals ofChina(中国地震年鉴)1949-1981,1984,1985,1987-1992,1996,1998-2001[M].Beijing:SeismologicalPress
[9] ZhaoZhu(赵珠).Primary study on the seismicity features inand nearQinghaiL ijiaxiaReservoir area[J].EarthquakeResearchInSichuan(四川地震),1999,(4):1～6
[10]WangJian(王健),GaoXuezhong(高学忠),ZhangL in(张林),et al.Assessment of geologic zones inLongyangxia-Qingtongxia continued hydroelectric power construction[J].QinghaiEnvironment(青海环境),1998,8(3):126～133
[11]GaoShijun(高士钧),GanJiasi(甘家思),WangQingyun(王清云),etal.Conditions and characteristics of induced earthquakein geheyan reservoir area,QingjinanRiver[J].CrustalDef ormation andEarthquake(地壳形变与地震),2001,21(3):93～100
[12]L iJiarong(李家荣).Prediction of the earthquake with thereservoir ofTianshenqiaoHydroelectricStation inNanpanjiang,Guizhou[J].GuizhouGeology(贵州地质),1997,16(4):336～344
[13]ChangBaoqi(常宝琦) andLiangJibin(梁纪彬).Prediction ofmaximum magnitude of reservoir induced seismicity[J].SourthChinaEarthquake(华南地震),1992,12(1):74～9
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