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


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Abstract

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.

About the authors

Yu. F. Moroz

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

Author for correspondence.
Email: morozyf@kscnet.ru
Russian Federation, Ulan Ude, 670047; Petropavlovsk-Kamchatsky, 683006

V. A. Loginov

Institute of Volcanology and Seismology, Far East Branch

Email: morozyf@kscnet.ru
Russian Federation, Petropavlovsk-Kamchatsky, 683006

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