1920年海原8.5级地震对兰州地区的减震作用
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甘肃省科委基金资助


REDUCIBLE SEISMIC INTENSITY IN THE LANZHOU AREA DUE TO THE 1920 HAIYUAN M8.5 EARTHQUAKE
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    摘要:

    1920年海原8.5级大震在其发震断层两侧160km范围内今后几百年内不会发生大于6.5级的地震.兰州地区距海原大震断层约120km,所以兰州地区今后几百年内也不会发生大于6.5级的地震,即不会发生烈度大于Ⅷ度的地震.而兰州地区是按Ⅷ度抗震设防的,即使今后发生6.5级的地震,其破坏亦不会很严重.这是按最坏情况考虑的.

    Abstract:

    Effective distance to reduce seismic intensity on two sides of the main fault causing the 1920 Haiyuan M8.5 earthquake is about 160 km.Within the distance no M>6.5 earthquake will occur during the future several hundreds of years.Because Lanzhou City is 120 km away from the main fault, in the city no M>6.5 earthquake will occur in a few hundreds of years.Structures and buildings in Lanzhou City were designed according to antiseismic standard of Ⅷ degree on the intensity scale.Even though a M6.5 earthquake will occur in future,its destruction would not be too heavy.It is a consideration in the worst case.

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滕建中,秦保燕,郭安宁.1920年海原8.5级地震对兰州地区的减震作用[J].地震工程学报,1997,19(4):95-97. TENG Jianzhong, QIN Baoyan, GUO Anning. REDUCIBLE SEISMIC INTENSITY IN THE LANZHOU AREA DUE TO THE 1920 HAIYUAN M8.5 EARTHQUAKE[J]. China Earthquake Engineering Journal,1997,19(4):95-97.

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  • 收稿日期:1997-01-15
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  • 在线发布日期: 2017-06-24