Probabilistic seismic hazard analysis in Nepal

被引:0
作者
Thapa Dilli Ram
Guoxin Wang
机构
[1] Dalian University of Technology,State Key Laboratory of Coastal and Offshore Engineering
来源
Earthquake Engineering and Engineering Vibration | 2013年 / 12卷
关键词
seismic hazard assessment; peak ground acceleration; earthquake; Nepal Himalaya;
D O I
暂无
中图分类号
学科分类号
摘要
The seismic ground motion hazard for Nepal has been estimated using a probabilistic approach. A catalogue of earthquakes has been compiled for Nepal and the surrounding region (latitude 26° N and 31.7° N and longitude 79° E and 90° E) from 1255 to 2011. The distribution of catalogued earthquakes, together with available geological and tectonic information were used to delineate twenty-three seismic source zones in Nepal and the surrounding region. By using the seismic source information and probabilistic earthquake hazard parameters in conjunction with a selected ground motion prediction relationship, peak ground accelerations (PGAs) have been calculated at bedrock level with 63%, 10%, and 2% probability of exceedance in 50 years. The estimated PGA values are in the range of 0.07–0.16 g, 0.21–0.62 g, and 0.38–1.1 g for 63%, 10%, and 2% probability of exceedance in 50 years, respectively. The resulting ground motion maps show different characteristics of PGA distribution, i.e., high hazard in the far-western and eastern sections, and low hazard in southern Nepal. The quantified PGA values at bedrock level provide information for microzonation studies in different parts of the country.
引用
收藏
页码:577 / 586
页数:9
相关论文
共 194 条
  • [1] Ader T(2012)Convergence Rate across the Nepal Himalaya and Interseismic Coupling on the Main Himalayan Thrust: Implications for Seismic Hazard Journal of Geophysical Research 117 B04403-206
  • [2] Avouac JP(2004)Magnitude Calibration of North Indian Earthquakes Geophysical Journal International 159 165-13872
  • [3] Zeng JL(1986)Quaternary Extension in Southern Tibet Journal of Geophysical Research 91 13803-589
  • [4] Caen HL(2006)Plate Motion of India and Interseismic Strain in the Nepal Himalaya from GPS and DORIS Measurements Journal of Geodesy 80 567-128
  • [5] Bollinger L(1995)Location and Magnitude of the 1833 Nepal Earthquake and Its Relation to the Rupture Zones of Contiguous Great Himalayan Earthquakes Current Science 69 101-64
  • [6] Galetzka J(1997)GPS Measurements of Present-day Convergence across the Nepal Himalaya Nature 386 61-13407
  • [7] Genrich J(2000)Modeling Mountain Building and the Seismic Cycle in the Himalaya of Nepal Journal of Geophysical Research 105 13389-71
  • [8] Thomas M(1992)Seismotectonics of Himalaya Current Science 62 40-2969
  • [9] Chanard K(1977)Seismic Moments of Major Earthquakes and the Average Rate of Slip in Central Asia Journal of Geophysical Research 82 2945-1606
  • [10] Sapkota SN(1968)Engineering Seismic Risk Analysis Bulletin of the Seismological Society of America 58 1583-264