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Annual Meeting - SCEC.org

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Lett., Seismological Society of America <strong>Annual</strong><br />

<strong>Meeting</strong>, Memphis, TN.<br />

Chen, K. H., Bürgmann, R., and Nadeau, R. M. (2010),<br />

Triggering effect of M 4-5 earthquakes on the<br />

earthquake cycle of repeating events at Parkfield,<br />

Bull. Seism. Soc. Am., 100, 2,<br />

doi:10.1785/0120080369.<br />

Fabian, A., L. Ojha, Z. Peng, and K. Chao (2009),<br />

Systematic search of remotely triggered tremor in<br />

Northern and Southern California, Eos Trans.<br />

AGU, 90(54), Fall Meet. Suppl., Abstract T13D-<br />

1916.<br />

Hauksson, E., J. Stock, K. Hutton, W. Yang, A. Vidal,<br />

and H. Kanamori, The 2010 Mw7.2 El Mayor-<br />

Cucapah Earthquake Sequence, Baja California,<br />

Mexico and Southernmost California, USA: Active<br />

Seismotectonics Along the Mexican Pacific Margin,<br />

Pure Appl. Geophys, Topical Issue: Geodynamics<br />

of the Mexican Pacific Margin, DOI<br />

10.1007/s00024-010-0209-7, 2010.<br />

Horstmann, T., Harrington, R.M., Cochran, E.S., Wang,<br />

T., Potier, C.E. (2010), Automatic tremor detection<br />

and waveform component analysis using a neural<br />

network approach, Abstract S23A-2122, 2010 Fall<br />

<strong>Meeting</strong>, American Geophysical Union.<br />

<strong>SCEC</strong> Research Accomplishments | Report<br />

Li, Y. G., P. Malin, and E. Cochran, High-Resolution Characterization of the Damage Zone on the Parkfield San Andreas Fault<br />

at Depth from Fault-Zone Trapped Waves, Book of Frontiers in Seismology, China High-Education Press, Beijing , in<br />

press, 2011<br />

Ma, S., and D. J. Andrews (2010), Inelastic off-fault response and three-dimensional earthquake rupture dynamics on a strikeslip<br />

fault, J. Geophys. Res., 115, B04304, doi:10.1029/2009JB006382.<br />

Peng, Z., D. P. Hill, D. R. Shelly and C. Aiken (2010), Remotely triggered microearthquakes and tremor in Central California<br />

following the 2010 Mw8.8 Chile Earthquake, Geophys. Res. Lett., 37, L24312, doi:10.1029/2010GL045462.<br />

Peng, Z., C. Wu, and C. Aiken (2011), Delayed triggering of microearthquakes by multiple surface waves circling the Earth,<br />

Geophys. Res. Lett., Geophys. Res. Lett., 38, L04306, doi: 2010GL046373.<br />

Shelly, D. R., Z. Peng, D. P. Hill and C. Aiken (2011), Delayed dynamic triggering of tremor and implications for triggered<br />

creep and earthquakes, Nature Geosci., accepted.<br />

Shelly, D. R., and J. L. Hardebeck (2010), Precise tremor source locations and amplitude variations along the lower␣crustal<br />

central San Andreas Fault, Geophys. Res. Lett., 37, L14301, doi:10.1029/2010GL043672.<br />

Tectonic Geodesy<br />

Figure 6. Accumulated plastic strain in logarithmic scale at a cross<br />

section 15 km from the epicenter from a model using a fractal fault<br />

geometry. The curved black line shows the fault trace at this cross<br />

section. The right side of the fault is a extensional regime, where the<br />

plastic strain is larger.<br />

Introduction<br />

The tectonic geodesy community within <strong>SCEC</strong> has again focused its efforts on inter-related combinations of data gathering<br />

and interpretation. The validation and application of transient detection algorithms was again a major effort, with a wide<br />

range of algorithms being tested against real and synthetic data. We are currently on track to having several detectors running<br />

in a <strong>SCEC</strong>-supported testing framework before the end of the year.<br />

Transient Detection<br />

Duncan Agnew made his FAKENET software available to the community, both for internal testing of detection algorithms as<br />

well as for the generation of new synthetic test data. Some of the major changes this year allowed inclusion of more realistic,<br />

non-sinusoidal seasonal signals and volume sources that imitate the effects of groundwater withdrawal and recharge. Herring<br />

2011 <strong>SCEC</strong> <strong>Annual</strong> <strong>Meeting</strong> | 43

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