The mechanism of the deep-focus, Sea of Okhotsk earthquake of May 24, 2013 as inferred from static displacements and broadband seismograms

Author:

Abubakirov I. R.,Pavlov V. M.,Titkov N. N.

Publisher

Pleiades Publishing Ltd

Subject

Metals and Alloys,Geophysics,Geotechnical Engineering and Engineering Geology

Reference17 articles.

1. Chebrov, V.N., Kugaenko, Yu.A., Vikulina, S.A., et al., The deep magnitude M w = 8.3 Sea of Okhotsk earthquake of May 24, 2013—the largest seismic event off Kamchatka during the entire period of detailed seismological observation, Vestnik KRAUNTs, Nauki o Zemle, 2013, no. 1, issue 21, pp. 17–24.

2. Droznin, D.V. and Droznina, S.Ya., The DIMAS interactive program for seismic signal processing, Seismicheskie Pribory, 2010, vol. 46, no. 3, pp. 22–34.

3. Ekström, G., Nettles, M., and Dziewoński, A.M., The global CMT project 2004–2010: Centroid-moment tensors for 13,017 earthquakes, Physics of the Earth and Planetary Interiors, 2012, vol. 200, pp. 1–9.

4. Herring, T.A., King, R.W., McClusky, S.C., et al., GAMIT: GPS Analysis at MIT, Release 10.4, Massachusetts Institute of Technology, 2010a.

5. Herring, T.A., King, R.W., McClusky, S.C., GLOBK: Global Kalman Filter VLBI and GPS Analysis Program, Release 10.4, Massachusetts Institute of Technology, 2010b.

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