On finding and using repeating seismic events in and near China

[1] A comprehensive search for repeating seismic events was performed using cross correlation on waveforms for 17,898 seismic events in and near China reported in the Annual Bulletin of Chinese Earthquakes from 1985 to 2005. We define a repeat as an event pair having a high cross correlation (≥0.8) for a particular bandwidth (0.5 to 5 Hz) and time window (5 s before P arrival to 40 s after Lg arrival). Such events typically have hypocenters separated by no more than about 1 km. This result enables a determination of median relative location error of around 15 km for global and regional catalogs that locate events in this study one at a time using phase picks. The maximum location error is on the order of hundreds of kilometers. We use nonnormalized cross-correlation values to measure relative amplitudes of event pairs. The standard deviation is about 0.06 magnitude units, much better than the precision of relative magnitudes for doublet events, which we estimate for the Chinese catalog to have a standard deviation of 0.36 magnitude units. Two thousand three hundred and seventy-nine events out of the 17,898 or 13% of the events in this catalog are classified as repeats, with later years showing an increase in the percentage. About half the repeats occur as isolated doublets, the rest as multiplets of three or larger, up to a 92-event multiplet. Most of the events appear to be triggered or are due to some earthquake interaction since their recurrence intervals are significantly shorter than would be estimated from tectonic loading.

[1]  J. E. Vidale,et al.  Variations in rupture process with recurrence interval in a repeated small earthquake , 1994, Nature.

[2]  L. Burdick,et al.  The reproducing earthquakes of the Galapagos Islands , 1980 .

[3]  G. Beroza,et al.  Coseismic and postseismic velocity changes measured by repeating earthquakes , 2004 .

[4]  David P. Schaff,et al.  Semiempirical Statistics of Correlation-Detector Performance , 2008 .

[5]  Michael A. Ellis,et al.  Active tectonics of the Beichuan and Pengguan faults at the eastern margin of the Tibetan Plateau , 2007 .

[6]  P. Richards,et al.  Wide-scale detection of earthquake waveform doublets and further evidence for inner core super-rotation , 2008 .

[7]  F. Ringdal,et al.  The detection of low magnitude seismic events using array-based waveform correlation , 2006 .

[8]  Y. Ben‐Zion,et al.  Temporal Changes of Shallow Seismic Velocity Around the Karadere-Düzce Branch of the North Anatolian Fault and Strong Ground Motion , 2006 .

[9]  Kevin Mayeda,et al.  mb(LgCoda): A stable single station estimator of magnitude , 1993, Bulletin of the Seismological Society of America.

[10]  F. Waldhauser,et al.  Large-scale relocation of two decades of Northern California seismicity using cross-correlation and double-difference methods , 2008 .

[11]  Felix Waldhauser,et al.  Waveform Cross-Correlation-Based Differential Travel-Time Measurements at the Northern California Seismic Network , 2005 .

[12]  David P. Schaff,et al.  Broad‐scale applicability of correlation detectors to China seismicity , 2009 .

[13]  Paul G. Richards,et al.  The stability of rms Lg measurements and their potential for accurate estimation of the yields of Soviet underground nuclear explosions , 1990, Bulletin of the Seismological Society of America.

[14]  P. Richards,et al.  Repeating Seismic Events in China , 2004, Science.

[15]  H. Kanamori The energy release in great earthquakes , 1977 .

[16]  J. Vidale,et al.  Seismic Evidence for Rock Damage and Healing on the San Andreas Fault Associated with the 2004 M 6.0 Parkfield Earthquake , 2005 .

[17]  W Foxall,et al.  Clustering and Periodic Recurrence of Microearthquakes on the San Andreas Fault at Parkfield, California , 1995, Science.

[18]  Fred W. Klein,et al.  Deep fault plane geometry inferred from multiplet relative relocation beneath the south flank of Kilauea , 1994 .

[19]  P. Silver,et al.  Migration of seismic scatterers associated with the 1993 Parkfield aseismic transient event , 2003, Nature.

[20]  G. Beroza,et al.  Depth constraints on nonlinear strong ground motion from the 2004 Parkfield earthquake , 2005 .

[21]  Gregory C. Beroza,et al.  Detailed observations of California foreshock sequences: Implications for the earthquake initiation process , 1996 .

[22]  B. E. Shaw,et al.  Postseismic response of repeating aftershocks , 1998 .

[23]  V. Keylis-Borok On estimation of the displacement in an earthquake source and of source dimensions , 2010 .

[24]  M. Caffee,et al.  Uniform slip‐rate along the Kunlun Fault: Implications for seismic behaviour and large‐scale tectonics , 2000 .

[25]  G. Beroza,et al.  Nonlinear strong ground motion in the ML 5.4 Chittenden earthquake: Evidence that preexisting damage increases susceptibility to further damage , 2004 .

[26]  Lucile M. Jones,et al.  Foreshocks (1966-1980) in the San Andreas system , 1984 .

[27]  C. R. Allen,et al.  Red River and associated faults, Yunnan Province, China: Quaternary geology, slip rates, and seismic hazard , 1984 .

[28]  C. K. Saikia,et al.  Modified frequency-wavenumber algorithm for regional seismograms using Filon's quadrature: modelling of Lg waves in eastern North America , 1994 .

[29]  G. Beroza,et al.  Evidence for Widespread Nonlinear Strong Ground Motion in the MW 6.9 Loma Prieta Earthquake , 2004 .

[30]  Jim Mori,et al.  Occurrence patterns of foreshocks to large earthquakes in the western United States , 1996, Nature.

[31]  F. Niu,et al.  Spatial clustering and repeating of seismic events observed along the 1976 Tangshan fault, north China , 2007 .

[32]  J R Booker,et al.  Aftershocks Caused by Pore Fluid Flow? , 1972, Science.

[33]  W. Ellsworth,et al.  Fault healing inferred from time dependent variations in source properties of repeating earthquakes , 1995 .