RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 10, ES5003, doi:10.2205/2007ES000268, 2008
Tectonic position of the Khailino and Olyutorka earthquakesG. P. Yarotskii Institute of Volcanology and Seismology, Far-East Division, Russian Academy of Sciences, Petropavlovsk-Kamchatskii, Russia
 The continent-ocean transition zone has various exogenous and endogenous processes that reflect the geodynamic ecological function of lithosphere. The East Kamchatka suffers the earthquakes with MSK-64 over 9 points. Petropavlovsk-Kamchatsky is in zone of 9.5 points. The area of strong earthquakes included the Hailinskoye (1991) the Olyotorskoye (2006) events with both magnitudes 7.1 that caused the area broadening. We suggest their tectonic position valuation in the block-mass-key (a piano-like) structure in the earth crust in concept of the continent active margin. This structure was formed by the system of the northwestern (320-330o) lateral deep faults. They are located logically and cross Kamchatka, Okhotskoye sea, Okhotsko-Chukotskiy volcanogenic belt and appear on the continent as linear (45o) faults. In Koryak-Kamchatkan region they appear each 75-160 km. They are between-blocks and stretch to the northwest for hundred of kilometers, divide the crust into blocks with vertical movements in different directions and have rather mobile southeastern ends in a transition zone between an ocean and a continent. Peninsulas represent the rising ends of blocks and the coastal gulfs represent the lowering ends of blocks. The scheme was determined from the south Japan to cape Dezhnyov. The both earthquakes occurred in the Vyvenka river-valley. Its northern valley side is a part of the Vyvenskiy deep northeastern fault and it is 12-20 km wide. The river-valley is represented by a depression. Its depth on a surface of Upper-Cretaceous basal complex is 3 km and in the Crystal basal complex comprises over 10 km. The length of the depression increases with the depth! The depression is located in the central part of a lowering block within Olyutorskiy gulf and is divided by lateral between-block faults: Paren'-Talovsko-Tilichkisky and Omolon-Kamensko-Olyutorsky. Along with the Vyvenskiy fault they "cut'' from a mobile end of margin crust a "key'' and that "key'' splits off from the continent and "slides'' into the ocean. Such a mechanism explains the earthquakes on the rest part of Chukotsky belt and supposes that the southeastern part of Koryakskiy highland may suffer the evolution of seismicity. It explains the presence also the gaps and zones of strong earthquakes for the Kurile-Kamchatkan island arc. They meet the width of a distance between the linear between-block faults. The zones of the major earthquakes and aftershocks near Kronotsky and Ozyorny peninsulas, Kunashir, Iturup and south Hokkaido islands justify this statement.
Received 19 January 2008; accepted 27 April 2008; published 18 June 2008.
Keywords: seismisity, tectonics, continental crust, Chukchi seismic belt.
Index Terms: 1734 History of Geophysics: Seismology; 1744 History of Geophysics: Tectonophysics; 3040 Marine Geology and Geophysics: Plate tectonics; 7215 Seismology: Earthquake source observations.
Citation: (2008), Tectonic position of the Khailino and Olyutorka earthquakes, Russ. J. Earth Sci., 10, ES5003, doi:10.2205/2007ES000268.Copyright 2008 by the Russian Journal of Earth Sciences
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