On a more precise assessment of seismic hazards for the city of Ulaanbaatar, Mongolia

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• 作者：S. Demberel (1)
  V. S. Imaev (2)
  E. A. Rogozhin (3)
  O. P. Smekalin (2)
  M. Ulziibat (1)
  A. V. Chipizubov (2)
  
• 关键词：earthquake ; fault ; paleoseismology ; trench ; magnitude ; intensity ; seismic hazard
• 刊名：Seismic Instruments
• 出版年：2014
• 出版时间：April 2014
• 年：2014
• 卷：50
• 期：2
• 页码：85-96
• 全文大小：
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• 作者单位：S. Demberel (1)
  V. S. Imaev (2)
  E. A. Rogozhin (3)
  O. P. Smekalin (2)
  M. Ulziibat (1)
  A. V. Chipizubov (2)
  
  1. Research Center of Astronomy and Geophysics, Mongolian Academy of Sciences, Ulaanbaatar, Mongolia
  2. Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences, Irkutsk, Russia
  3. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia
  
• ISSN：1934-7871

文摘

The recent geological, geophysical, and paleoseismic research of the Hustai, Emeelt, and Gunjiin active seismogenic faults in the vicinity of Ulaanbaatar provided evidence of prehistoric seismic events there. In particular, dislocations of two fault-forming paleo-earthquakes were revealed in the Gunjiin tectonic zone. The shocks occurred in the Late Pleistocene-Early Holocene. The presence of ruptures, initially identified by morphological characteristics, was proven by trenching studies and materials of geophysical profiles. The magnitudes of the ancient earthquakes are estimated to be 6.5-.0. The obtained results provide grounds for reassessment of the possible level of seismic hazards for the territory of Ulaanbaatar to at least 8.