汶川地震震中映秀地区地表破裂特征
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摘要
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。
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 mainly 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 geological history.
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 mainly 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 geological history.
引文
[1]李勇,周荣军,董顺利,等.汶川特大地震的地表破裂与逆冲-走滑作用[J].成都理工大学学报(自然科学版),2008,35(4):404-413.
[2]徐锡伟,闻学泽,叶建青,等.汶川MS8.0地震地表破裂带及其发震构造[J].地震地质,2006,30(3):597-629.
[3]刘旭宇,姚凯,何新社,等.2008年5月12日汶川MS8.0地震甘肃强震记录与初步分析[J].西北地震学报,2008,30(3):266-269.
[4]周荣军,李勇,Densmore A L,等.青藏高原东缘活动构造[J].矿物岩石,2006,26(2):40-51.
[5]张彬,杨选辉,陆远忠.地震动态应力触发研究进展[J].西北地震学报,2008,30(3):299-301.
[6]李勇,周荣军,Densmore A L,等.青藏高原东缘大陆动力学过程与地质响应[M].北京:地质出版,2006.
[2]徐锡伟,闻学泽,叶建青,等.汶川MS8.0地震地表破裂带及其发震构造[J].地震地质,2006,30(3):597-629.
[3]刘旭宇,姚凯,何新社,等.2008年5月12日汶川MS8.0地震甘肃强震记录与初步分析[J].西北地震学报,2008,30(3):266-269.
[4]周荣军,李勇,Densmore A L,等.青藏高原东缘活动构造[J].矿物岩石,2006,26(2):40-51.
[5]张彬,杨选辉,陆远忠.地震动态应力触发研究进展[J].西北地震学报,2008,30(3):299-301.
[6]李勇,周荣军,Densmore A L,等.青藏高原东缘大陆动力学过程与地质响应[M].北京:地质出版,2006.
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