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何森凯. 九寨沟漳扎镇M7.0地震灾害分析[J]. 国际地震动态 , 2018, (6): 22-27. DOI: 10.3969/j.issn.0253-4975.2018.06.004
引用本文: 何森凯. 九寨沟漳扎镇M7.0地震灾害分析[J]. 国际地震动态 , 2018, (6): 22-27. DOI: 10.3969/j.issn.0253-4975.2018.06.004
Senkai He. Analysis on M7.0 earthquake disaster in Zhangzha town of Jiuzhaigou[J]. Progress in Earthquake Sciences, 2018, (6): 22-27. DOI: 10.3969/j.issn.0253-4975.2018.06.004
Citation: Senkai He. Analysis on M7.0 earthquake disaster in Zhangzha town of Jiuzhaigou[J]. Progress in Earthquake Sciences, 2018, (6): 22-27. DOI: 10.3969/j.issn.0253-4975.2018.06.004

九寨沟漳扎镇M7.0地震灾害分析

Analysis on M7.0 earthquake disaster in Zhangzha town of Jiuzhaigou

  • 摘要: 2017年8月8日21时19分,九寨沟县漳扎镇发生M7.0地震,震中位于(33.20°N,103.82°E),震源深度约为20 km。地震震中紧邻世界自然遗产九寨沟自然保护区,对保护区造成一定破坏,并导致20人死亡,250余人受伤,将近4万人滞留。针对此次大地震,本文着重分析其震源机制和破坏形式,结果表明:此次九寨沟地震为高倾角的走滑型地震,矩震级MW达到6.5,其断层节面Ⅰ为左旋正断,倾角和滑动角分别为62°和–15°;断层节面Ⅱ为右旋正断,倾角和滑动角分别为77°和–151°;对设防烈度Ⅷ度以下的钢筋混凝土框架结构所造成的最大层间位移角超过GB50011-2010《建筑抗震设计规范》规定的弹性层间位移角限值1/550,并对大跨度结构产生较大影响,容易引发建筑物坍塌;此外,由于此次地震为高倾角的走滑型地震,极易引发山体滑坡,造成二次灾害,增加震后的救援难度。

     

    Abstract: At 21:19 on August 8, 2017, the M7.0 earthquake broke out in Zhangzha town of Jiuzhaigou. The epicenter is located at (33.20°N, 103.82 °E), and the focal depth is about 20 kilometers. The earthquake epicenter is close to the Jiuzhaigou nature reserve, causing some damage to the protected areas, and leading to 20 deaths, more than 250 injuries, and nearly 40 thousand people trapped. In view of this great earthquake, the focal mechanism and damage form were emphatically analyzed in this paper. The results show that the Jiuzhaigou earthquake is a strike slip earthquake, and its moment magnitude is 6.5. Meanwhile, the fault section surface Ⅰ is a left-lateral normal faulting, and the dip angle and the slip angle are 62 degrees and –15 degrees respectively. Besides, the fault plane Ⅱ is right-lateral normal faulting, and the dip angle and the slip angle are 77 degrees and –151 degrees respectively. The maximum drift of the reinforced concrete frame structure exceeds the specified value in GB50011-2010. Moreover, it has a great influence on the long-span structure, and easily causes the collapse of buildings. In addition, due to the strike-slip type of earthquake, it’s easy to touch off landslide along with secondary disaster which increases the difficulty of rescue after the earthquake.

     

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