Song J, Jiang H K. 2009. A review on decay and generation of aftershock activity. Seismology and Geology (in Chinese), 31(3): 559-571.
[2]
Sun M, Wang W M, Wwang X et al.2015.Rupture process of the Minxian-Zhangxian, Gansu, China MS6.6 earthquake on 22 July 2013.Chinese J. Geophys. (in Chinese),58(6): 1909-1918,doi: 10.6038/cjg20150607.
[3]
Turcotte D L, Holliday J R, Rundle J B. 2007. BASS, an alternative to ETAS. J. Geophys. Res., 34(12): L12303.
[4]
Utsu T. 1961. A statistical study on the occurrence of aftershocks. Geophys. Mag., 30: 521-605.
[5]
Utsu T, Ogata Y, Matsuura R S. 1995. The centenary of the Omori formula for a decay law of aftershock activity. J.Phys. Earth., 43(1): 1-33.
[6]
Wang J, Schweitzer J, Tilmann F, et al. 2011. Application of the multichannel Wiener filter to regional event detection using NORSAR seismic-array data. Bull. Seism. Soc. Am., 101(6): 2887-2896.
[7]
Wu C Q, Meng X F, Peng Z G, et al. 2014. Lack of spatiotemporal localization of foreshocks before the 1999 MW7.1 Düzce, Turkey, earthquake. Bull. Seism. Soc. Am., 104(1): 560-566.
[8]
Zhao Z X, Kazuo O, Kazuo M, et a1. 1992. P values of continental aftershock activity in China. Acta Seismologica Sinica (in Chinese), 14(1): 9-16.
[9]
Zheng W J, Yuan D Y, He W G, et al. 2013. Geometric pattern and active tectonics in Southeastern Gansu province: Discussion on seismogenic mechanism of the Minxian-Zhangxian MS6.6 earthquake on July 22, 2013. Chinese J. Geophys. (in Chinese), 56(12): 4058-4071, doi: 10.6038/cjg20131211.
[10]
Akaike H. 1974. A new look at the statistical model identification. IEEE Trans. Autom. Control, 19(6): 716-723.
[11]
Bouchon M, Karabulut H, Aktar M, et al. 2011. Extended nucleation of the 1999 MW7.6 Izmit earthquake. Science, 331(6019): 877-810.
[12]
Chen J F, Yang L M. 2011. Study of source parameters'' relationship in Gansu province. Seismological and Geomagnetic Observation and Research (in Chinese), 32(1): 10-14.
[13]
Disaster Prevention Department of China Earthquake Administration. 1995. China historical earthquake catalog (23rd century BC—1911 AD) (in Chinese). Beijing: Seismological Press, 497-499.
[14]
Enescu B, Mori J, Miyazawa M. 2007. Quantifying early aftershock activity of the 2004 mid-Niigata Prefecture earthquake (Mw6.6). J. Geophys. Res., 112: B04310, doi: 10. 1029/2006JB004629.
[15]
Enescu B, Mori J, Miyazawa M, et al. 2009. Omori-Utsu law c-values associated with recent moderate earthquakes in Japan. Bull. Seism. Soc. Am., 99(2A): 884-891.
[16]
Gentili S, Bressan G. 2008. The partitioning of radiated energy and the largest aftershock of seismic sequences occurred in the northeastern Italy and western Slovenia. J. Seismol., 12(3): 343-354.
[17]
Huang Q H. 2006. Search for reliable precursors: A case study of the seismic quiescence of the 2000 western Tottori prefecture earthquake. J. Geophys. Res., 111(B4): B04301, doi: 10.1029/2005/JB003982.
[18]
Husen S, Wiemer S, Smith R B. 2004. Remotely triggered seismicity in the Yellowstone National Park region by the 2002 Mw7.9 Denali Fault earthquake, Alaska. Bull. Seism. Soc. Am., 94(6B): S317-S331.
[19]
Jia K, Zhou S, Wang R. 2012. Stress interactions within the strong earthquake sequence from 2001 to 2010 in the Bayankala block of eastern Tibet. Bull. Seism. Soc. Am., 102(5): 2157-2164.
[20]
Jia K, Zhou S Y, Zhuang J C, et al. 2014. Possibility of the independence between the 2013 Lushan earthquake and the 2008 Wenchuan earthquake on Longmen Shan fault, Sichuan, China. Seismological Research Letters, 85(1): 60-67, doi: 10.1785/0220130115.
[21]
Jiang C S, Wu Z L. 2011. Intermediate-term medium-range accelerating moment release (AMR) prior to the 2010 Yushu MS7.1 earthquake. Chinese J. Geophys. (in Chinese), 54(6): 1501-1510, doi: 10.3969/j.issn.0001-5733.2011.06.009.
[22]
Jiang C S, Wu Z L, Han L B, et al. 2013. Effect of cutoff magnitude Mc of earthquake catalogues on the early estimation of earthquake sequence parameters with implication for the probabilistic forecast of aftershocks: the 2013 Minxian-Zhangxian, Gansu, MS6.6 earthquake sequence. Chinese J. Geophys. (in Chinese), 56(12): 4048-4057, doi: 10.6038/cjg20131210.
[23]
Jiang H K, Zheng J C, Wu Q, et a1. 2007. Earlier statistical features of ETAS model parameters and their seismological meanings. Chinese J. Geophys. (in Chinese), 50(6): 1778-1786.
[24]
Kagan Y Y, Houston H. 2005. Relation between mainshock rupture process and Omori''s law for aftershock moment release rate. Geophys. J. Int., 163(3): 1039-1048.
[25]
Kato A, Obara K, Igarasgi T, et al. 2012. Propagation of slow slip leading up to the 2011 MW9.0 Tohoku-Oki earthquake. Science, 335(6069): 705-708.
[26]
Kato A, Obara K. 2014. Step-like migration of early aftershocks following the 2007 MW6.7 Noto-Hanto earthquake, Japan. Geophys. Res. Lett., 41(11): 3864-3869, doi: 10.1002/2014GL060427.
[27]
Lengliné O, Enescu B, Peng Z X, et al. 2012. Decay and expansion of the early aftershock activity following the 2011, Mw9.0 Tohoku earthquake. Geophysical Research Letters, 39(18), doi: 10.1029/2012GL052797.
[28]
Lolli B, Gasperini P. 2003. Aftershocks hazard in Italy Part I: Estimation of time-magnitude distribution model parameters and computation of probabilities of occurrence. J. Seismol., 7(2): 235-257.
[29]
Marsan D, Enescu B. 2012. Modeling the foreshock sequence prior to the 2011, MW9.0 Tohoku, Japan, earthquake. J. Geophys. Res., 117: B06316, doi: 10.1029/2011JB009039.
[30]
Ogata Y. 1988. Statistical models for earthquake occurrences and residual analysis for point processes. J. Amer. Statist. Assoc., 83(401): 9-27.
[31]
Ogata Y. 1989. Statistical model for standard seismicity and detection of anomalies by residual analysis. Tectonophysics, 169(1-3): 159-174.
[32]
Ogata Y. 2001. Increased probability of large earthquakes near aftershock regions with relative quiescence. J. Geophys. Res., 106(B5): 8729-8744.
[33]
Peng Z G, Vidale J E, Houston H. 2006. Anomalous early aftershock decay rate of the 2004 Mw6.0 Parkfield, California, earthquake. Geophys. Res. Lett., 33(17): L17307, doi: 10.1029/2006GL026744.
[34]
Peng Z G, Vidale J E, Ishii M, et al. 2007. Seismicity rate immediately before and after main shock rupture from high-frequency waveforms in Japan. J. Geophys. Res., 112: B03306, doi: 10. 1029/2006JB004386.
[35]
Peng Z G, Zhao P. 2009. Migration of early aftershocks following the 2004 Parkfield earthquake. Nature Geoscience, 2(12): 877-881.
[36]
Rabinowitz N, Steinberg D M. 1998. Aftershock decay of three recent strong earthquakes in the Levant. Bull. Seism. Soc. Am., 88(6): 1580-1587.
[37]
Sawazaki K, Enescu B. 2014. Imaging the high-frequency energy radiation process of a main shock and its early aftershock sequence: The case of the 2008 Iwate-Miyagi Nairiku earthquake, Japan. J. Geophys. Res.: Solid Earth, 119(6): 4729-4746, doi: 10.1002/2013JB010539.
[38]
Shally D R, Beroza G C, Ide S. 2007. Non-volcanic tremor and low-frequency earthquake swarms. Nature, 446(7133): 305-307.
[39]
Sheherbakov R, Turcotte D L. 2004. A modified form of Bath''s Law. Bull. Seism. Soc. Am., 94(5): 1968-1975.