Probabilistic seismic hazard assessment for Bayankhongor aimag of Mongolia

A. D., Odonbaatar Ch, M. D, Bayarsaikhan E, Dembereldulam M
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Abstract

Central Asia is one of the seismically most active regions in the world. Its complex seismicity is due to the collision of the Eurasian and Indian plates, which has resulted in some of the world’s largest intra-plate events over history. The region is dominated by reverse faulting over strike slip and normal faulting events.The GSHAP project, aiming at hazard assessment on a global scale, indicates that the territory of Bayankhongor aimag, Mongolia, in Central Asia is characterized by maximum bedrock peak ground accelerations for 10% probability of exceedance in 50 years as medium as in range of 80 to 160cm/s2. In this study, which has been carried out within the framework of the project “Seismic microzoning map of center of 12 aimags, Mongolia”, the area source model and different kernel approaches are used for a probabilistic seismic hazard assessment for the Mongolia. The seismic hazard is assessed considering shallow (depth <50 km) seismicity only and employs an updated (with respect to previous projects) earthquake catalogue for the region. The hazard maps, shown in terms of 10% probability of exceedance in 50 years, are derived by using the Open Deterministic and Probabilistic Seismic Hazard Assessment (ODPSHA), which is based on the Cornell methodology. The maximum hazard observed in the region reaches 93-98 cm/s2 , which in intensity corresponds to VII in MSK64 scale in the centre of Bayankhongor aimag for 475 years mean return period.
蒙古巴彦淖尔地区地震危险性概率评价
中亚是世界上地震最活跃的地区之一。其复杂的地震活动是由于欧亚板块和印度板块的碰撞,这导致了一些历史上世界上最大的板块内事件。该区域以走滑逆断层和正断层活动为主。GSHAP项目旨在进行全球范围的危险评估,该项目表明,中亚蒙古巴彦洪戈尔省的最大基岩峰值地面加速度为50年内超过10%的概率,中等范围为80至160cm/s2。本研究是在“蒙古国12个省中心地震微区划图”项目的框架内进行的,将区域源模型和不同的核方法用于蒙古国的概率地震危险性评估。地震危险性评估仅考虑浅层(深度<50km)地震活动,并采用该地区更新的(关于以前的项目)地震目录。危险地图以50年内10%的超越概率表示,是通过使用基于康奈尔方法的开放确定性和概率地震危险评估(ODPSHA)得出的。该地区观测到的最大危险达到93-98 cm/s2,其强度相当于巴彦洪戈尔省中心MSK64级的VII级,平均重现期为475年。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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