四川地震
四川地震
사천지진
EARTHQUAKE RESEARCH IN SICHUAN
2014年
2期
34-37
,共4页
地震活动图像异常%强震重复性%中等%中强以上地震的相关性%科研成果与地震预测相结合%会商机制
地震活動圖像異常%彊震重複性%中等%中彊以上地震的相關性%科研成果與地震預測相結閤%會商機製
지진활동도상이상%강진중복성%중등%중강이상지진적상관성%과연성과여지진예측상결합%회상궤제
seismicity pattern image%reoccurred strong earthquake%correlation of moderate and strong earth-quakes%combining the research results with the practice
许多强震震例总结表明,在大地震前往往出现多种先兆性地震活动异常,可以作为强震危险区预测的重要依据[1,2]。回顾芦山地震前存在的地震活动图像异常有:川滇2008年开始新一轮大震活跃幕;沿E103°线分布的川滇东缘带是近期大地震的主体活动带;历史上川北M≥6级地震的原地复发,已出现4对,1327年天全地震离逝时间已680余年;1500~2007年中国南北地震带东缘带(银川-通海)M≥7.7级地震空段内(康定-武都),在2008年发生了汶川8级地震,北东向单侧破裂约300 km,但南段(映秀-天全)并未破裂,原缺震“空段”尚余一半;川滇几次中强以上地震后芦山-大邑均发生响应性诱发地震;中等地震月频次异常出现在2012年4月、7月和2013年2月;2013年2月18日四川盆地内三台-盐亭间先发生4.7级地震;四川及邻区大地震后5年左右的晚期强余震及后续强震活动;地震活动性参数b值异常等。这些异常图像的分析和应用有助于芦山地震的总结。
許多彊震震例總結錶明,在大地震前往往齣現多種先兆性地震活動異常,可以作為彊震危險區預測的重要依據[1,2]。迴顧蘆山地震前存在的地震活動圖像異常有:川滇2008年開始新一輪大震活躍幕;沿E103°線分佈的川滇東緣帶是近期大地震的主體活動帶;歷史上川北M≥6級地震的原地複髮,已齣現4對,1327年天全地震離逝時間已680餘年;1500~2007年中國南北地震帶東緣帶(銀川-通海)M≥7.7級地震空段內(康定-武都),在2008年髮生瞭汶川8級地震,北東嚮單側破裂約300 km,但南段(映秀-天全)併未破裂,原缺震“空段”尚餘一半;川滇幾次中彊以上地震後蘆山-大邑均髮生響應性誘髮地震;中等地震月頻次異常齣現在2012年4月、7月和2013年2月;2013年2月18日四川盆地內三檯-鹽亭間先髮生4.7級地震;四川及鄰區大地震後5年左右的晚期彊餘震及後續彊震活動;地震活動性參數b值異常等。這些異常圖像的分析和應用有助于蘆山地震的總結。
허다강진진례총결표명,재대지진전왕왕출현다충선조성지진활동이상,가이작위강진위험구예측적중요의거[1,2]。회고호산지진전존재적지진활동도상이상유:천전2008년개시신일륜대진활약막;연E103°선분포적천전동연대시근기대지진적주체활동대;역사상천북M≥6급지진적원지복발,이출현4대,1327년천전지진리서시간이680여년;1500~2007년중국남북지진대동연대(은천-통해)M≥7.7급지진공단내(강정-무도),재2008년발생료문천8급지진,북동향단측파렬약300 km,단남단(영수-천전)병미파렬,원결진“공단”상여일반;천전궤차중강이상지진후호산-대읍균발생향응성유발지진;중등지진월빈차이상출현재2012년4월、7월화2013년2월;2013년2월18일사천분지내삼태-염정간선발생4.7급지진;사천급린구대지진후5년좌우적만기강여진급후속강진활동;지진활동성삼수b치이상등。저사이상도상적분석화응용유조우호산지진적총결。
A lot of summaries of strong earthquakes indicate that many kind of precursory seismicities appeared be-fore strong earthquakes. We take these precursory seismicities as a key factor to predict the epicenter of future strong earthquake. The seismicity precursory image before the M7. 0 Lushan Earthquake is that the Sichuan-yun-nan seismic regions are in active episode since 2008 . The eastern belts of Sichuan-yunnan along the east longi-tude 103 line were recent main seismicity belts. From the historical earthquakes studies we find the north Sichuan province is an original seismic belts with the magnitude of M6 . 5 and there were 4 pair of earthquakes and 680 years have passed since the 1327 Tianquan Earthquake. From 1500 to 2007,the east boundary seismic belts along the south-north seismic belts from yingchuan to Tonghai in China,was a gap of M≥7. 7 from Kangdin to Tianquan. The 2008 M8. 0 Wenchuan Earthquake broke a fault about 300 km long. But the southern segment did not. The in-duced response earthquakes along the Lushan-Dayu occurred after several strong earthquakes in Sichuan and yun-nan Provinces. The month times anomaly of precursory earthquakes with a middle level happen in three periods that is April,July 2012 and February 2013 respectively. In Sichuan basin there was an M4. 7 Santai Earthquake on 18 February 2013 . There will be strong aftershocks after the strong earthquake of the 2008 M8 . 0 Wenchuan Earth-quake in Sichuan and nearby regions. The abnormal parameter value-b of seismicity appears.