The Deep Geoelectrical Section of the Avacha–Koryak Zone of Contemporary Volcanism, Kamchatka


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The methods and results of magnetotelluric sounding in the range of 0.0001–1000 s and more with the use small portable magnetotelluric stations are considered. Data on the distribution of electrical conductivity at depths beneath the Avacha–Koryak zone of contemporary volcanism are obtained. The obtained data are interpreted using the modern techniques and methods.

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Yu. Moroz

Institute of Geology, Siberian Branch; Institute of Volcanology and Seismology, Far East Branch

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Email: morozyf@kscnet.ru
俄罗斯联邦, Ulan Ude, 670047; Petropavlovsk-Kamchatsky, 683006

V. Loginov

Institute of Volcanology and Seismology, Far East Branch

Email: morozyf@kscnet.ru
俄罗斯联邦, Petropavlovsk-Kamchatsky, 683006

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