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Modeling of coseismic crustal movements initiated by the May 24, 2013, M w=8.3 Okhotsk deep focus earthquake

期刊

DOKLADY EARTH SCIENCES
卷 457, 期 2, 页码 976-981

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MAIK NAUKA/INTERPERIODICA/SPRINGER
DOI: 10.1134/S1028334X1408008X

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资金

  1. RFBR-JSPS [13-05-92101]
  2. FEB RAS [12-III-A-08-186, 12-I-P4-07, 12-I-ONIT-02]
  3. Targeted Comprehensive Research Program of FEB RAS Recent Geodynamics, Active Geostructures and Natural Hazards of the Far East of Russia
  4. Grants-in-Aid for Scientific Research [26109007] Funding Source: KAKEN

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The Okhotsk deep focus earthquake (M (w) = 8.3), the largest in the history of instrumental seismology, occurred on May 24, 2013, at 05:45 UTC in the Sea of Okhotsk near the western coast of the Kamchatka Peninsula. For the first time we have succeeded in catching the field of horizontal and vertical coseismic offsets generated by a strong deep seismic event, and investigating its characteristics using continuous GPS measurements. Based on these data and taking into account the seismological information, we have developed a dislocation model of the Okhotsk deep focus earthquake.

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