RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 10, ES5003, doi:10.2205/2007ES000268, 2008
[9] The discussed territory belongs to the Koryak-Kamchatka fold area located in northwestern segment of the Pacific mobile belt. The extreme northwestern part of the territory occurs in the Late Cretaceous Koryak tectonic zone (Koryak autochthon); further southeastwards it is associated successively with the Late Cretaceous Vyvenki uplift, Neogene-Quaternary Vyvenki depression, Paleogene-Neogene Tylgovayam synclinorium with local Tylgovayam and Korf depressions, and with the narrow northern stripe of the Pylgovayam anticlinorium [Kravchenko and Razumnyi, 2002; Kravchenko et al. 2000; Litvinov, 1999].
Citation: 2008), Tectonic position of the Khailino and Olyutorka earthquakes, Russ. J. Earth Sci., 10, ES5003, doi:10.2205/2007ES000268.
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