摘要
根据近场强震台加速度记录对2011年10月12日北京市石景山区ML2.1地震的加速度影响场进行了计算分析。同时使用了首都圈宽频带数字台站记录数据通过P波初动格点尝试法解算出该地震的震源机制解,并与加速度影响场进行对比研究。结果表明,此次地震加速度影响场水平向加速度高于垂直向;水平向峰值加速度分布区和加速度影响场高低速度过渡区总体呈EW向或NEE向分布,与震源机制解结果的两个节面走向较为一致;加速度衰减NS向快于EW向。本文研究结果可为强震或较大地震发生后快速判定震害影响场提供参考依据。
An earthquake with a magnitude（ML） of 2.1 occurred at 16：40 UTC,October 12,2011,in the Shijingshan district in Beijing with an epicenter at 39.95° N,116.16° E.Eleven near-field strong motion stations,located less than 20 km from the epicenter,clearly recorded temporal variation of acceleration during the earthquake.The largest value of peak ground acceleration in the east-west（EW） and north-south（NS） components,22.528 gal and 30.989 gal,respectively,were both recorded by station LSG,which is situated approximately 5.6 km from epicenter.The largest value of peak ground acceleration in the vertical component was 12.797 gal,recorded by station CCS at an epicenter distance of 2.2 km.We synthesized the horizontal component by EW and NS records and used Generic Mapping Tools（GMT） software to mesh and illustrate the influence of horizontal and vertical acceleration on the field contour map.The results show that generally,the value of the NS component is larger than that of the EW component,and the horizontal component is larger than the vertical.Moreover,the acceleration distribution and influence field contour map of the horizontal component shows that peak ground acceleration in the southern area is a low value and that in the northern area is high.In addition,the two regions are divided by a transition zone that strikes near east-west（EW） or NEE.We obtained the average peak ground value of three components at 1 s intervals from station records after the earthquake occurred,which we synthesized into horizontal and vertical components to illustrate temporal variations in the map produced by GMT.After analyzing the average value records and temporal variation map,we detected that the decay in the NS direction is faster than that in the EW direction and that decay is faster in the vertical component than that in the horizontal component.Excepting the near-field strong motion stations,23 Capital Circle broadband digital seismic stations recorded digital waveform data during the earthquake.We interpreted initial P-wave polarity from these records and employed grid-point test method to obtain the Focal Mechanism Solution of the event.Results indicate normal faulting dominant in the Beijing-Tianjin area.The best double couple solution of the event is 295°,39° and-74° for strike,dip and rake angel,respectively;those of the other nodal plane are 96°,53°,and-102° with a 13% inconsistency ratio.By combining these results with the acceleration analysis results,we determined that the strike of the second nodal plane with a larger dip angel is near the EW direction,which is consistent with the strike of acceleration transition zone.In addition,the microepicenter of the event does not coincide with the macroepicenter.These findings indicate that the nodal plane of strike 96°,dip 53°,and rake-102°may coincide with the seismogenic fault.Although the work in this study is a preliminary analysis for acceleration records and seismic digital waveform data,the results can provide a reference for quick determination of earthquake influence field and hazard assessment following a large earthquake and are highly significant for earthquake emergency response and disaster relief.
出处
《地震工程学报》
CSCD
北大核心
2013年第1期183-189,共7页
China Earthquake Engineering Journal
基金
国家科技支撑计划"汶川断裂带科学钻探"
关键词
峰值加速度
加速度动态分布
震源机制解
震害影响场
北京地区
Peak ground acceleration
Dynamic acceleration distribution
Focal mechanism solution
Earthquake influence field
Beijing area
