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FigureS1.pdfPDF document157KEvidence of tremors triggered in QCM by surface waves from the 11 March 2011 Mw9.0 Tohoku-Oki mainshock as recorded at the MOBC station. (a) Instrument-corrected transverse, radial, and vertical component unfiltered velocity seismograms with Love and Rayleigh waves marked. (b) Band-pass filtered 5−15 Hz instrument-corrected velocity seismogram depicting tremors triggered by the Love and Rayleigh waves of the Tohoku-Oki mainshock. (c) Spectrogram showing the frequency contents of the triggered tremors.
FigureS3.pdfPDF document2291KComparison of MOBC and BBB station transverse velocity components after correcting the amplitude of the MOBC station north component. The shifted BBB seismogram (gray) was shifted by the difference in 4.1 km/s Love wave arrival times at the MOBC and BBB stations.
FigureS2.pdfPDF document23KVertical velocity amplitude spectra for all mainshocks. Symbols are the same as in Figure 4b.
FigureS4.pdfPDF document8KTransverse PGVs and dynamic stress versus back azimuth for earthquakes to the Queen Charlotte Fault region (low-pass filtered 30 s). Symbols are the same as in Figure 4a.
TableS1.pdfPDF document21KSupporting Information
TableS2.pdfPDF document15KSupporting Information
Aiken_etal_GRL_2013_SUPP_revised.txtplain text document4KSupporting Information

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