地震工程学报
地震工程學報
지진공정학보
China Earthquake Engineering Journal
2014年
2期
256-260
,共5页
蒙古国%背景地震%地震危险性分析%空间光滑地震活动性模型
矇古國%揹景地震%地震危險性分析%空間光滑地震活動性模型
몽고국%배경지진%지진위험성분석%공간광활지진활동성모형
Mongolia%background earthquake%seismic hazard analysis%spatially smoothed seis-micity model
根据蒙古国及其周边地区的背景地震目录(M≤6.0),采用空间光滑地震活动性的方法研究了蒙古国地区背景地震危险性水平,给出了蒙古国50年超越概率10%的峰值加速度分布图。结果表明蒙古国大部分地区背景地震危险性水平为0.05 g,部分地区高达0.1~0.15 g,意味着蒙古国地区背景地震危险性高,在进行地震危险性分析和地震区划时应充分考虑背景地震活动,采用不同起始震级的地震活动性模型计算得到的地震危险性水平具有较大的空间差异,因此在采用空间光滑地震活动性模型进行地震危险性分析时应采用多个模型加权平均的方法,平衡地震频度和地震震级的影响。
根據矇古國及其週邊地區的揹景地震目錄(M≤6.0),採用空間光滑地震活動性的方法研究瞭矇古國地區揹景地震危險性水平,給齣瞭矇古國50年超越概率10%的峰值加速度分佈圖。結果錶明矇古國大部分地區揹景地震危險性水平為0.05 g,部分地區高達0.1~0.15 g,意味著矇古國地區揹景地震危險性高,在進行地震危險性分析和地震區劃時應充分攷慮揹景地震活動,採用不同起始震級的地震活動性模型計算得到的地震危險性水平具有較大的空間差異,因此在採用空間光滑地震活動性模型進行地震危險性分析時應採用多箇模型加權平均的方法,平衡地震頻度和地震震級的影響。
근거몽고국급기주변지구적배경지진목록(M≤6.0),채용공간광활지진활동성적방법연구료몽고국지구배경지진위험성수평,급출료몽고국50년초월개솔10%적봉치가속도분포도。결과표명몽고국대부분지구배경지진위험성수평위0.05 g,부분지구고체0.1~0.15 g,의미착몽고국지구배경지진위험성고,재진행지진위험성분석화지진구화시응충분고필배경지진활동,채용불동기시진급적지진활동성모형계산득도적지진위험성수평구유교대적공간차이,인차재채용공간광활지진활동성모형진행지진위험성분석시응채용다개모형가권평균적방법,평형지진빈도화지진진급적영향。
In this article,we calculate seismic hazards from background seismicity by using a spa-tially smoothed seismicity model for Mongolia,and we obtain a peak ground acceleration (PGA) map for 10% probability of exceedance in 50 y.We propose two seismicity models to calculate seismic hazard maps for 10% probability of exceedance in 50 y.The results show that the seismic activity model and the seismic hazard results,both calculated by using the instrumental seismic catalog (M≥ 3.0),can reflect contemporary seismic activity levels and seismic hazard levels of the Mongolia area.In addition,the seismic activity model and the seismic hazard results,both of which are calculated by using historical earthquake data (M≥ 5.0),can quite well represent the seismic hazard level of moderate earthquakes in Mongolia.The two seismic hazard maps both show that the background seismic hazard level is 0.05 g in most areas of Mongolia and that the values of this parameter are high,at 0.1~0.15 g,in other areas,which indicates a background of high seismic hazards in Mongolia.Therefore,it is highly necessary to completely consider the im-pacts of background seismicity when implementing seismic hazard analysis and seismic hazard mapping for Mongolia.Moreover,we compare two seismicity models.The results also illustrate significant spatial differences between the seismicity models with different minimum complete magnitudes.Therefore,when adopting a spatially smoothed seismicity model to analyze seismic hazards for Mongolia,the weighted average of several different models should be considered to balance the impacts of earthquake occurrences and magnitudes.