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Stanford Center for Induced and Triggered Seismicity
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Earthquake Seismology
Abercrombie, R. E. (1995). Earthquake source scaling relationships from -1 to 5 ML using seismograms recorded at 2.5-km depth, Journal of Geophysical Research, 100 (12), 24,015 – 24,036, doi: 10.1029/95JB02397.
Aki, K. (1967). Scaling law of seismic spectrum, Journal of Geophysical Research, 72 (4), 1217-1231, doi:10.1029/JZ072i004p01217
Allmann, B. P., P. M. Shearer (2009). Global variations of stress drop for moderate to large earthquakes, Journal of Geophysical Research, 114, B01310, doi:10.1029/2008JB005821
An In‐Depth Seismological Analysis Revealing a Causal Link Between the 2017 MW 5.5 Pohang Earthquake and EGS Project
Astiz, L. , Dieterich, J., Frohlich, C., Hager, B., Juanes, R., Shaw, J., The Potential for Induced Seismicity at the Cavone Oilfield: Analysis of Geological and Geophysical Data, and Geomechanical Modeling
Avouac, J.-P. (2012). Earthquakes: Human induced shaking. Nature Geoscience, 5(11), 763–764.
Bachman, Wiemer, Goertz-Allman, and Woessner (2012) Influence of pore-pressure on the event-size distribution of induced earthquakes, Geophys. Res. Lett., 39 , 1-7.
Baltay, A., G. Prieto, G. C. Beroza (2010). Radiated seismic energy from coda measurements and no scaling in apparent stress with seismic moment, Journal of Geophysical Research, 115, B08341, doi: 10.1029/2009JB006736.
Beyreuther, Hammer, Wasserman, Ohrnberger, and Megies (2012) Constructing a hidden Markov model based earthquake detector: application to induced seismicity, Geophys. J. Int., 189 , 602-610
Campbell, K. W., and Y. Bozorgnia (2008). NGA ground motion model for the geometric mean horizontal component of PGA, PGV, PGD and 5% damped linear elastic response spectra for periods ranging from 0.01 to 10 s, Earthquake Spectra, 24 (1), 139–171
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