地球物理学报
地毬物理學報
지구물이학보
2010年
2期
305-317
,共13页
长期地震危险性评估%强震潜在危险区%ETAS模型%川滇地区%汶川M_S8.0地震
長期地震危險性評估%彊震潛在危險區%ETAS模型%川滇地區%汶川M_S8.0地震
장기지진위험성평고%강진잠재위험구%ETAS모형%천전지구%문천M_S8.0지진
Long-term seismic hazard evaluation%Potential source zones of strong earthquake%ETAS model%Sichuan-Yunnan region%Wenchuan M_S8.0 earthquake
利用基于时一空传染型余震序列(Epidemic Type Aftershock Sequence,简称ETAS)模型的随机除丛法,重新审视了2008年5月12日汶川M_S8.0地震前可能存在的长期地震活动异常,研究了川滇地区背景地震活动特征,并评估了当前的强震危险状态.对川滇地区1970年以来的M_S3.0以上的背景地震和从集地震活动的研究结果表明,该地区地震丛集特征明显、时空分布很不均匀、地震序列常有前震事件.直接将概率值作为地震计数的权重,对地震丛集率空间分布图像分析表明,汶川M_S8.0地震前,龙门山断裂带中南段存在着长期、大范围的地震丛集率低值区,震前该段处于应力闭锁状态.对川滇地区地震丛集率低值区内背景地震与全部地震的累积次数、b值和新定义的△b等统计参量的分析表明,龙日坝与龙门山断裂带具有地震活动的关联性,川滇地区当前的强震潜在危险区可能是巧家地区和汶川M_S8.0地震破裂尚未穿越的龙门山断裂带南段.此外,还发现b值倾向于反映局部应力场变化,而△b能较为敏感地给出更大范围应力场的相对变化.
利用基于時一空傳染型餘震序列(Epidemic Type Aftershock Sequence,簡稱ETAS)模型的隨機除叢法,重新審視瞭2008年5月12日汶川M_S8.0地震前可能存在的長期地震活動異常,研究瞭川滇地區揹景地震活動特徵,併評估瞭噹前的彊震危險狀態.對川滇地區1970年以來的M_S3.0以上的揹景地震和從集地震活動的研究結果錶明,該地區地震叢集特徵明顯、時空分佈很不均勻、地震序列常有前震事件.直接將概率值作為地震計數的權重,對地震叢集率空間分佈圖像分析錶明,汶川M_S8.0地震前,龍門山斷裂帶中南段存在著長期、大範圍的地震叢集率低值區,震前該段處于應力閉鎖狀態.對川滇地區地震叢集率低值區內揹景地震與全部地震的纍積次數、b值和新定義的△b等統計參量的分析錶明,龍日壩與龍門山斷裂帶具有地震活動的關聯性,川滇地區噹前的彊震潛在危險區可能是巧傢地區和汶川M_S8.0地震破裂尚未穿越的龍門山斷裂帶南段.此外,還髮現b值傾嚮于反映跼部應力場變化,而△b能較為敏感地給齣更大範圍應力場的相對變化.
이용기우시일공전염형여진서렬(Epidemic Type Aftershock Sequence,간칭ETAS)모형적수궤제총법,중신심시료2008년5월12일문천M_S8.0지진전가능존재적장기지진활동이상,연구료천전지구배경지진활동특정,병평고료당전적강진위험상태.대천전지구1970년이래적M_S3.0이상적배경지진화종집지진활동적연구결과표명,해지구지진총집특정명현、시공분포흔불균균、지진서렬상유전진사건.직접장개솔치작위지진계수적권중,대지진총집솔공간분포도상분석표명,문천M_S8.0지진전,룡문산단렬대중남단존재착장기、대범위적지진총집솔저치구,진전해단처우응력폐쇄상태.대천전지구지진총집솔저치구내배경지진여전부지진적루적차수、b치화신정의적△b등통계삼량적분석표명,룡일패여룡문산단렬대구유지진활동적관련성,천전지구당전적강진잠재위험구가능시교가지구화문천M_S8.0지진파렬상미천월적룡문산단렬대남단.차외,환발현b치경향우반영국부응력장변화,이△b능교위민감지급출경대범위응력장적상대변화.
Based on the time-space epidemic-type aftershock sequence (ETAS) model and stochastic declustering method, a retrospective study was conducted to investigate whether long-term seismieity anomalies existed before the May 12, 2008, Wenchuan M_S8.0 earthquake, and to evaluate the current potential risks of strong earthquakes in the Sichuan-Yunnan region. We analyzed the background and clustering of earthquakes above M_L3.0 in the period from 1977 to the day before the Wenchuan M_S8.0 earthquake, the results showed that seismic activity in the Sichuan-Yunnan region was significantly clustered, heterogeneously distributed in space and time, and the earthquake sequences were usually preceded by foreshock events. Through the analysis of the spatial variation of the 'clustering seismicity ratio', we found that there existed a long-term and large area of low 'clustering seismicity ratio' in the middle-south section of Longmenshan faults, which implied that this region had been in a state of stress barrier before the Wenchuan M_S8.0 earthquake. Statistics of several parameters including cumulative numbers of background and total sesimicity, b value and newly defined △b value were conducted to evaluate the current potential risk of strong earthquakes in the areas of low "clustering seismicity ratio' in the Sichuan-Yunnan region. The results showed that the seismic activity is correlated significantly between the Longriba and Longmenshan faults, and that the Qiaojia region and the southern segment of Longmenshan faults have high potential of strong earthquakes. Moreover, we also found that the b value trends to reflect the local variations of stress field, while △b can reveal sensitively the relative variation of the stress field in a larger spatial range.