西北地震学报
西北地震學報
서북지진학보
NORTHWESTERN SEISMOLOGICAL JOURNAL
2009年
4期
339-343
,共5页
马博琳%李勇%董顺利%陈浩%闫亮%乔宝成
馬博琳%李勇%董順利%陳浩%閆亮%喬寶成
마박림%리용%동순리%진호%염량%교보성
地表破裂%汶川大地震%映秀地区%逆冲-右行走滑
地錶破裂%汶川大地震%映秀地區%逆遲-右行走滑
지표파렬%문천대지진%영수지구%역충-우행주활
Surface rupture%Wenchuan great earthquake%Yingxiu area%Thrust and dextral strike-slip
汶川8级大震的震中位于映秀镇,地震在映秀地区造成了多处地表破裂,如公路拱曲、地震陡坎,坡中槽新变形等,长度达300余米.经实地全站仪和GPS测量,定量分析了地表破裂的垂直分量与水平分量以及两者之间的比值,以此揭示了映秀-北川断裂的运动性质为逆冲兼右行走滑,在映秀地区逆冲分量大于走滑分量.将本次地震造成的位错数据与震前资料对比,发现汶川地震产生的地表破裂位置与地质历史上映秀-北川断裂造成的断层位错位置是相当吻合的,说明映秀地区Ⅳ级阶地上40余米的的断层陡坎可能是地质历史时期若干次大地震的结果.
汶川8級大震的震中位于映秀鎮,地震在映秀地區造成瞭多處地錶破裂,如公路拱麯、地震陡坎,坡中槽新變形等,長度達300餘米.經實地全站儀和GPS測量,定量分析瞭地錶破裂的垂直分量與水平分量以及兩者之間的比值,以此揭示瞭映秀-北川斷裂的運動性質為逆遲兼右行走滑,在映秀地區逆遲分量大于走滑分量.將本次地震造成的位錯數據與震前資料對比,髮現汶川地震產生的地錶破裂位置與地質歷史上映秀-北川斷裂造成的斷層位錯位置是相噹吻閤的,說明映秀地區Ⅳ級階地上40餘米的的斷層陡坎可能是地質歷史時期若榦次大地震的結果.
문천8급대진적진중위우영수진,지진재영수지구조성료다처지표파렬,여공로공곡、지진두감,파중조신변형등,장도체300여미.경실지전참의화GPS측량,정량분석료지표파렬적수직분량여수평분량이급량자지간적비치,이차게시료영수-북천단렬적운동성질위역충겸우행주활,재영수지구역충분량대우주활분량.장본차지진조성적위착수거여진전자료대비,발현문천지진산생적지표파렬위치여지질역사상영수-북천단렬조성적단층위착위치시상당문합적,설명영수지구Ⅳ급계지상40여미적적단층두감가능시지질역사시기약간차대지진적결과.
On the epicenter area of Wenchuan great earthquake in 2008, Yingxiu town, Sichuan province, the earthquake caused a number of surface rupture, such as road bending deformation, fault scarps and new deformation at "the groove in the slope", the total length of zone is about 300 meters. Using total station and GPS, at 4 rupture points the displacement were measured, and the vertical and level components of offset were analyzed quantitatively, as well as the ratio between them. The result shows that the motion of seismogenic Yingxiu-Beichuan fault is main-ly thrust with some right-lateral strike slip, the thrust component is greater than the strike-slip component at Yingxiu area. Comparing the surface rupture before and after the event at same place, it is revealed that the earthquake rupture is anastomose with the active location of Yingxiu -Beichuan fault during recent geology history, which means that the fault scarp about 40 m on the terrace Ⅳ of Mingjiang river maybe is the results of number of major earthquakes in geolog-ical history.