期刊文献+

Recurrence Behaviors of Earthquakes along the Kefallinia Transform Fault, Ionian Sea, Greece

Recurrence Behaviors of Earthquakes along the Kefallinia Transform Fault, Ionian Sea, Greece
下载PDF
导出
摘要 We examined the whole strong earthquake recurrence behaviors of two fault zones along the Kefallinia Transform, Ionian Sea, Greece, using seismological data and statistical methods. Our data include 29 events with %M%>5^5 for the period 1636~2003. We found different recurrence behaviors for the Kefallinia Fault Zone (clustering and time-predictable recurrence behaviors) and the Lefkada Fault Zone (near random and non-slip-predictable or non-time-predictable recurrence nature). The different modes may be attributed to: (a) segment interaction along-strike (Kefallinia) by static triggering and (b) the influence of fault systems to the north and east on the recurrence on Lefkada. Within the active periods, earthquake recurrence intervals are distributed in a more dispersed fashion, and can be fitted well by a Weibull distribution. In contrast, the distribution of the quiet periods is relatively less dispersed and difficult to describe by suitable probability functions. We examined the whole strong earthquake recurrence behaviors of two fault zones along the Kefallinia Transform, Ionian Sea, Greece, using seismological data and statistical methods. Our data include 29 events with M 〉 5.5 for the period 1636 - 2003. We found different recurrence behaviors for the Kefallinia Fault Zone (clustering and time-predictable recurrence behaviors) and the Letkada Fault Zone (near random and non-slip-predictable or non-time-predictable recurrence nature). The different modes may be attributed to: (a) segment interaction along-strike (Kefallinia) by static triggering and (b) the influence of fault systems to the north and east on the recurrence on Lefkada. Within the active periods, earthquake recurrence intervals are distributed in a more dispersed fashion, and can be fitted well by a Weibull distribution. In contrast, the distribution of the quiet periods is relatively less dispersed and difficult to describe by suitable probability functions.
出处 《Earthquake Research in China》 2007年第4期409-419,共11页 中国地震研究(英文版)
基金 This paper is part result of the program"Investigation of recurrence modes of large earthquakes alongthe main seismogenic faults in Greece andin China"(20051696) in the frame of bilateral cooperation between China and Greece inthefield of seismology and geophysics sponsored bythe Ministry of Science and Technologyof China This programis mainlyfunded bythe NSF40674024 and the NSF40374019
关键词 地震 历史 概率分布 希腊 Historical earthquake Active fault zone Earthquake recurrence Probability distribution Greece
  • 相关文献

参考文献14

  • 1傅征祥,易桂喜,闻学泽.Earthquake recurrence on whole active fault zones and its relation to that on individual fault-segments[J].Acta Seismologica Sinica(English Edition),2000,13(5):563-574. 被引量:5
  • 2闻学泽.Recurrence behaviors of segment-rupturing earthquakes on active faults of the Chinese mainland[J].Acta Seismologica Sinica(English Edition),1999,12(4):457-465. 被引量:8
  • 3C. Benetatos,A. Kiratzi,Z. Roumelioti,G. Stavrakakis,G. Drakatos,I. Latoussakis.The 14 August 2003 Lefkada Island (Greece) earthquake: Focal mechanisms of the mainshock and of the aftershock sequence[J].Journal of Seismology.2005(2)
  • 4E. M. Scordilis,G. F. Karakaisis,B. G. Karacostas,D. G. Panagiotopoulos,P. E. Comninakis,B. C. Papazachos.Evidence for transform faulting in the Ionian sea: The Cephalonia island earthquake sequence of 1983[J].Pure and Applied Geophysics PAGEOPH.1985(3)
  • 5YiGuixi,WenXueze,XuXiwei.Study on Integrated Recurrence Behaviors of Strong Earthquakes Along Entire Active Fault Zones in the Sichuan-Yunnan Region, China[J].Earthquake Research in China,2003,17(2):145-159. 被引量:1
  • 6Utsu T.Estimation of parametersfor recurrence models of earthquakes[].Bull Earthquake Res lnst Univ Tokyo.1984
  • 7Taymaz T,Jackson J,McKenzie D.Active tectonics of the north and central Aegean Sea[].Geophysical Journal International.1991
  • 8Sorel D.Etude neotectonique damI arc Pgeen externe occidental :les iles ioniennes de Kephallinia et Zakinthos , etI Elide occidentale .These 3e cycle ,Lab.de Gtol .Dyn.Interne .Bit .509[]..1976
  • 9Serpelloni E,Anzidei M,Baldi P.et al.Crustal velocity and strain-ratefieldsinItaly and surroundingregions :newresults fromthe analysis of permanent and non-permanent GPS networks[].Geophysical Journal International.2005
  • 10Scordilis E.M,Karakaisis G.F,Karacostas B.G. et al.Evidence for transformfaulting in the Ionian Sea- theCephalonia island earthquake sequence of 1983[].Pure and Applied Chemistry.1985

二级参考文献16

  • 1傅征祥,易桂喜,闻学泽.Earthquake recurrence on whole active fault zones and its relation to that on individual fault-segments[J].Acta Seismologica Sinica(English Edition),2000,13(5):563-574. 被引量:5
  • 2闻学泽.Recurrence behaviors of segment-rupturing earthquakes on active faults of the Chinese mainland[J].Acta Seismologica Sinica(English Edition),1999,12(4):457-465. 被引量:8
  • 3B. C. Papazachos.A time- and magnitude-predictable model for generation of shallow earthquakes in the Aegean area[J]. Pure and Applied Geophysics PAGEOPH . 1992 (2)
  • 4X. Wen.Rupture segmentation and assessment of probabilities of seismic potential on the Xiaojiang fault zone. Acta Seismologica Sinica . 1993
  • 5Bakun,W H,McEvilly,T V.Recurrence models and Parkfield, California, earthquakes. Journal of Geophysical Research . 1984
  • 6Catalogue ofChinese Historical StrongEarthquakes(23BC~1911AD). . 1995
  • 7Papazachos,B C.A time-predictable model for earthquake generation in Greece. Bulletin of the Seismological Society of America . 1989
  • 8J C Savage,R S Cockerham.Quasi-periodic occurrence of earthquakes in the 1978–1986 Bishop-Mammoth Lakes Sequence, Eastern California. Bulletin of the Seismological Society of America . 1986
  • 9Huang K Z,Mao S P.Slochastic Methods and Applied Fuzzs Mathematics. . 1987
  • 10The Atlas of Hisloric Earthquakes ofChina. . 1990

共引文献9

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部