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Features of Seismic Activation of the Middle Baikal Region, 2008-2011

机译:2008-2011年贝加尔湖中部地区地震活动特征

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摘要

Scenarios for developing focal zones of strong (M_w =5.3) earthquakes that occurred in the Middle Baikal region in 2008 and 2011 are considered. The new (submeridional and sublatitudinal) lines of destruction of the Earth's crust in the water area of the lake are recorded. The facts of seismoactive structures forming in the surrounding mountains (to the southeast) under typical rift conditions of movements are established, which indicates that the basin of Lake Baikal is expanding and growing due to active capturing and processing of its mountain surroundings.
机译:考虑了发展在2008年和2011年发生在贝加尔湖中部地区的强烈(M_w = 5.3)地震震源区的方案。记录了湖泊水域中地壳的新的(次生的和次生的)破坏线。建立了在典型的裂谷运动条件下在周围山脉(东南部)形成地震活动的事实,这表明贝加尔湖的盆地由于积极捕获和处理山脉周围环境而在扩大和增长。

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  • 来源
    《Doklady Earth Sciences》 |2013年第2期|1282-1287|共6页
  • 作者单位

    Institute of the Earth's Crust, Siberian Branch,Russian Academy of Sciences, Irkutsk, Russia;

    Baikal Branch of the Geophysical Service of the Siberian Branch, Russian Academy of Sciences, Irkutsk, Russia;

    Institute of the Earth's Crust, Siberian Branch,Russian Academy of Sciences, Irkutsk, Russia;

    Institute of the Earth's Crust, Siberian Branch,Russian Academy of Sciences, Irkutsk, Russia;

    Institute of Geology of the Geophysical Service of the Siberian Branch, Russian Academy of Sciences, Ulan Ude, Russia;

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