00000cab a22000003a 4500 UP-99796217612665425 Buklod 20231008001539.0 a grb 001 u| ta 180131s xx d | ||r ||||| || DENG eng Myo Thant Probabilistic seismic hazard assessment for Yangon Region, Myanmar Myo Thant. December 2014 pp.117-131 According to the seismicity and the records of the previous considerably high magnitude earthquakes, Yangon Region can be regarded as the low to medium seismicity region. Moreover, tectonically, the region is surrounded by the subduction zone between the Indian Plate and Burma Plate to the west and the right lateral Sagaing Fault to the east. The most significant earthquake happened around this region is the Bago earthquake of May 5, 1930 with a magnitude of 7.3. This earthquake caused 500 casualties and great destruction in Bago. However, considerable damage and 50 deaths were recorded in Yangon. It was originated from the Sagaing fault. The seismic hazard analysis is performed for Yangon region by applying the probabilistic way. In conducting seismic hazard analysis, firstly the most possible seismic sources are identified and the seismic source parameters are then determined for each sources. Based on the seismicity, focal mechanism study of the previous events, and the subduction zone of Indian Plate beneath Burma Plate, Sagaing fault, and Kyaukkyan fault. The seismic hazard analysis is carried out for 10% and 2% probabilities of exceedance in 50 years and the seismic hazard maps are represented in terms of peak ground acceleration and spectral acceleration at the periods of 0.2s and 1.0s for those recurrence intervals. Bago earthquake. Peak ground acceleration. Sagaing Fault. Seismic hazard analysis. Spectral acceleration. ASEAN engineering journal 3, 2C (2014 (Dec)). FO UPD DENG Article