Modeling of the strong ground motion of 25th April 2015 Nepal earthquake using modified semi-empirical technique

被引:5
作者
Lal, Sohan [1 ]
Joshi, A. [1 ]
Sandeep [2 ]
Tomer, Monu [3 ]
Kumar, Parveen [4 ]
Kuo, Chun-Hsiang [5 ]
Lin, Che-Min [6 ]
Wen, Kuo-Liang [7 ]
Sharma, M. L. [7 ]
机构
[1] Indian Inst Technol Roorkee, Dept Earth Sci, Roorkee, Uttar Pradesh, India
[2] Banaras Hindu Univ, Inst Sci, Dept Geophys, Varanasi, Uttar Pradesh, India
[3] Geol Survey India, Hyderabad, Telangana, India
[4] Wadia Inst Himalayan Geol, Dehra Dun, Uttar Pradesh, India
[5] Natl Ctr Res Earthquake Engn, Taipei, Taiwan
[6] Natl Cent Univ, Dept Earth Sci, Chungli, Taiwan
[7] Indian Inst Technol Roorkee, Dept Earthquake Engn, Roorkee, Uttar Pradesh, India
关键词
Strong motion; Himalayan seismicity; Displacement spectra; Response spectra; Site amplification; Modeling; EASTERN NORTH-AMERICA; COMPOSITE SOURCE MODEL; SEISMIC SHEAR-WAVES; GREAT EARTHQUAKES; SOURCE PARAMETERS; GREENS-FUNCTIONS; RUPTURE PROCESS; SOURCE SPECTRA; NEAR-FIELD; SIMULATION;
D O I
10.1007/s11600-018-0140-3
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
On 25th April, 2015 a hazardous earthquake of moment magnitude 7.9 occurred in Nepal. Accelerographs were used to record the Nepal earthquake which is installed in the Kumaon region in the Himalayan state of Uttrakhand. The distance of the recorded stations in the Kumaon region from the epicenter of the earthquake is about 420-515 km. Modified semi-empirical technique of modeling finite faults has been used in this paper to simulate strong earthquake at these stations. Source parameters of the Nepal aftershock have been also calculated using the Brune model in the present study which are used in the modeling of the Nepal main shock. The obtained value of the seismic moment and stress drop is 8.26 x 10(25) dyn cm and 10.48 bar, respectively, for the aftershock from the Brune model .The simulated earthquake time series were compared with the observed records of the earthquake. The comparison of full waveform and its response spectra has been made to finalize the rupture parameters and its location. The rupture of the earthquake was propagated in the NE-SW direction from the hypocenter with the rupture velocity 3.0 km/s from a distance of 80 km from Kathmandu in NW direction at a depth of 12 km as per compared results.
引用
收藏
页码:461 / 477
页数:17
相关论文
共 59 条
[1]   SCALING LAW OF SEISMIC SPECTRUM [J].
AKI, K .
JOURNAL OF GEOPHYSICAL RESEARCH, 1967, 72 (04) :1217-&
[2]  
[Anonymous], 1994, J HIMAL GEOL
[3]  
[Anonymous], 1964, J ENG MECH DIVISION
[4]   Earthquake ground-motion prediction equations for eastern North America [J].
Atkinson, Gail M. ;
Boore, David M. .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2006, 96 (06) :2181-2205
[5]  
Atkinson GM, 1998, B SEISMOL SOC AM, V88, P917
[6]  
ATKINSON GM, 1995, B SEISMOL SOC AM, V85, P17
[7]  
Beresnev IA, 1997, B SEISMOL SOC AM, V87, P67
[8]  
Beresnev IA, 1999, B SEISMOL SOC AM, V89, P608
[9]   Processing of strong-motion accelerograms: needs, options and consequences [J].
Boore, DM ;
Bommer, JJ .
SOIL DYNAMICS AND EARTHQUAKE ENGINEERING, 2005, 25 (02) :93-115
[10]  
BOORE DM, 1983, B SEISMOL SOC AM, V73, P1865