赵希俊, 刘锡大, 侯建军. 1966年邢台7.2级地震的动力学模型[J]. 华北地震科学, 1997, 15(3): 9-17.
引用本文: 赵希俊, 刘锡大, 侯建军. 1966年邢台7.2级地震的动力学模型[J]. 华北地震科学, 1997, 15(3): 9-17.
Zhao Xijun, Liu Xida, Hou Jianjun. A DYNAMIC MODEL OF 1996 XINGTAI MS 7.2 EARTHQUAKE[J]. North China Earthquake Sciences, 1997, 15(3): 9-17.
Citation: Zhao Xijun, Liu Xida, Hou Jianjun. A DYNAMIC MODEL OF 1996 XINGTAI MS 7.2 EARTHQUAKE[J]. North China Earthquake Sciences, 1997, 15(3): 9-17.

1966年邢台7.2级地震的动力学模型

A DYNAMIC MODEL OF 1996 XINGTAI MS 7.2 EARTHQUAKE

  • 摘要: 根据技新的深地震反射资料、构造应力场和震源机制等资料,建立了1966年邢台7.2缓地震孕震区的平面和剖面的有限元模型。对平面和剖面模型在EW向水平外压力下的最大剪应力分布进行了计算,剪应力相对集中的部位和大震震源位置比较一致。提出了邢台7.2级地震的动力学模型,认为地震的孕育和发生可能需要深、浅部断层、壳内低速层和EW向水平压力的共同作用。虽然由震源机制和地震宏观烈度分布等资料可指出有具体的发震断层存在,但地震的发生,更重要的应该是有各种构造和周围介质以最有利于应力集中方式的相互配合。

     

    Abstract: Based on fhe latest deep seismic reflection section, stress field and focal mechanism parameters, the 6nite elememt model of Xingtai M, 7.2 earthquake is presented. We think that Shulu Fault Basin is sub jected to horizontal external compressive stress field in east-west direction. The distributions of the maximum shear stress on the planer and sectional models are calculated. The results show that concen trati0n points of the maximum shear stress are on the whole consistent with the strong seismic focuses. A dynamic model of 1996 Xingtai M. 7.2 earthquake is presented too. Shallow faults, deep fsults, low-velocity layer in the earth's crust and horizontal compressive stress in east-west direction may be es sential for earthquakes occurring.

     

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