Probabilistic seismic hazard assessments for Northern Southeast Asia (Indochina): Smooth seismicity approach

被引:12
作者
Ornthammarath, Teraphan [1 ]
Warnitchai, Pennung [2 ]
Chan, Chung-Han [3 ]
Wang, Yu [4 ]
Shi, Xuhua [5 ]
Phuong Hong Nguyen [6 ]
Le Minh Nguyen [6 ]
Kosuwan, Suwith [7 ]
Thant, Myo [8 ]
机构
[1] Mahidol Univ, Fac Engn, Dept Civil & Environm Engn, 999 Phuttamonton 4 Rd, Salaya 73170, Nakhon Pathom, Thailand
[2] Asian Inst Technol, Civil & Infrastruct Engn Dept, Khlong Luang, Thailand
[3] Natl Cent Univ, Dept Earth Sci, Taoyuan, Taiwan
[4] Natl Taiwan Univ, Dept Geosci, Taipei, Taiwan
[5] Nanyang Technol Univ, Earth Observ Singapore, Singapore, Singapore
[6] Vietnam Acad Sci & Technol, Inst Geophys, Hanoi, Vietnam
[7] Dept Mineral Resources, Act Fault Res Div, Bangkok, Thailand
[8] Myanmar Earthquake Comm, Yangon, Myanmar
关键词
Southeast Asia; seismic hazard map; PSHA; global earthquake model; smooth seismicity; SUBDUCTION-ZONE EARTHQUAKES; STRONG GROUND MOTION; HORIZONTAL COMPONENTS; MYANMAR; MODEL; DEFORMATION; MAGNITUDE; TECTONICS; EQUATIONS; BOUNDARY;
D O I
10.1177/8755293020942528
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
We present an evaluation of the 2018 Northern Southeast Asia Seismic Hazard Model (NSAHM18) based on a combination of smoothed seismicity, subduction zone, and fault models. The smoothed seismicity is used to model observed distributed seismicity from largely unknown sources in the current study area. In addition, due to a short instrumental earthquake catalog, slip rate and characteristic earthquake magnitudes are incorporated through the fault model. To achieve this objective, the compiled earthquake catalogs and updated active fault databases in this region were reexamined with consistent use of these input parameters. To take into account epistemic uncertainty, logic tree analysis has been implemented incorporating basic quantities such as ground-motion models (GMMs) for three different tectonic regions (shallow active, subduction interface, and subduction intraslab), maximum magnitude, and earthquake magnitude frequency relationships. The seismic hazard results are presented in peak ground acceleration maps at 475- and 2475-year return periods.
引用
收藏
页码:69 / 90
页数:22
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