A geological study of the epicentral area of the April 20(21), 2006 Olyutorskii earthquake View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2010-04

AUTHORS

E. A. Rogozhin, A. N. Ovsyuchenko, A. V. Marakhanov, S. S. Novikov

ABSTRACT

Primary and secondary earthquake effects were investigated (surface breakage and felt effects in the villages of Tilichiki, Korf, and Khailino) in the epicentral area of a large earthquake occurring in northern Kamchatka Krai. The primary effects include an extended surface break that can be followed for a length of about 140 km. The secondary (gravitational and vibrational) effects include soil slides and minor rockfalls, snow flows on slopes, resonant cracks, soil liquefaction phenomena consisting of mud cones, mud gryphons, and discharges of soil from cracks. Detailed maps showing the main types of earthquake surface effects have been made. Paleoseismic data show traces of several large earthquakes that have occurred in the Olyutorskii earthquake zone. Radio carbon dating of soil samples from these paleoseismic scarps revealed a history of great earthquakes occurring in Koryakia. In all, four seismic events with magnitudes about that of the 2006 Olyutorskii earthquake have occurred there during 8000 years, the return period of such events being 1000–2500 years. More... »

PAGES

79-86

References to SciGraph publications

  • 2007-02. The Koryak strong earthquake of April 20 (21), 2006: Preliminary results in IZVESTIYA, PHYSICS OF THE SOLID EARTH
  • Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1134/s0742046310020028

    DOI

    http://dx.doi.org/10.1134/s0742046310020028

    DIMENSIONS

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