|Table of Contents|

Study of the Recurrence Interval of M7.5 Earthquake in the MiddlePart of Manila Trench in 1934 and Modeling the TsunamiPropagation Induced by this Earthquake(PDF)

《南京师大学报（自然科学版）》[ISSN:1001-4616/CN:32-1239/N]

Issue:
2016年04期
Page:
0-
Research Field:
·数学与计算机科学·
Publishing date:

Info

Title:
Study of the Recurrence Interval of M7.5 Earthquake in the MiddlePart of Manila Trench in 1934 and Modeling the TsunamiPropagation Induced by this Earthquake
Author(s):
Hong Mingli; Huo Zhenxiang; Ren Luchuan
Institute of Disaster Prevention,Sanhe Hebei 065201,China
Keywords:
tsunami; Numerical simulation; recurrence interval of the earthquake; Manila Trench
PACS:
P315.8
DOI:
10.3969/j.issn.1001-4616.2016.04.003
Abstract:
The Manila Trench was identified as the most dangerous tsunami source in the south China sea. In order to study the earthquake tsunami hazard in South China Sea,we use the method of seismic moment rate to study the recurrence interval of the M7.5 earthquake occurring in the middle part of the Manila trench in 1934. And the COMCOT model are used to model the tsunami propagation scenery induced by this earthquake and provide the tsunami heights and its arrival time for the surrounding regions,which can help to fill in the information gap over the historical data. Besides,we analyze the influences of different locations of fault source on the tsunami heights. Our analysis can provide useful data for the tsunami warning research in Philippine and other surrounding regions in South China Sea.

References:

[1] 魏柏林,康英,陈玉桃,等. 南海地震与海啸[J]. 华南地震,2006,26(1):47-58.
[2]KIRBY S,GEIST E L,LEE W H K,et al. Tsunami Source Characterization for Western Pacific Subduction Zones:A preliminary report[R]. 2006,http://walrus. wr.usgs.gov/tsunami/work-shop/.
[3]叶琳,于福江,吴玮. 我国海啸灾害及预警现状与建议[J]. 海洋预报,2005,22(增刊):147-157.
[4]LIU P L F,WANG X,ANDREW J S. Tsunami hazard and forecast study in south china sea[J]. Journal of Aaian earth sciences,2009,36:2-12.
[5]FIELD E,DAWSON T,FELZER K,et al. Uniform California Earthquake Rupture Forecast,Version 2(UCERF 2)[J]. Bulletin of the seismological society of America,2009,99(4):2 053-2 107.
[6]LIU P L F,WOO S B,CHO Y S. Computer programs for tsunami propagation and inundation[R]. 1998,http://ceeserver.cee.cornell.edu/pllgroup/comcot.htm.
[7]WANG X,LIU P L F. A numerical investigation of Boumerdes—Zem-mouri(Algeria)earthquake and tsunami[J]. Computer modeling in engineering&science,2007,10(6):171-183.
[8]BRUNE J N. Seismic moment,Seismicity,and Rate of Slip along Major Fault Zones[J]. Journal of geophysical research,1968,73(2):777-784.
[9]HANKS T C. Kanamori H. A moment-magnitude moment scale[J]. J Geophys Res,1979,84:2 348-2 350.
[10]NAKAMURA S. On Statistical Tsunami Risk of the Philippines[J]. South East Asian studies,1978,15(4):581-590.
[11]DUONG N A,KIMATA F,MEILANO I,et al. Assessment of Bathymetry Effects on Tsunami Propagation in Viet Nam[J]. Advances in natural science,2009,10(4):457-468.
[12]ACHARYA H K,吴振寰. 菲律宾断层的地震滑动及其构造意义[J]. 地震地质译丛,1981(3):16-18.
[13]HECK N H. List of seismic sea waves[J]. Bull Seism Soc Am,1947,4:269-279.
[14]BAUTISTA B C,BAUTISTA M L P,OLIKE K,et al. A new insight on the geometry of subducting slabs in northern Luzon,Philippines[J]. Tectonophysics,2001,339:279-310.

Memo

Memo:
-
Last Update: 2016-12-31