Variations in lithospheric conductivity in the Kamchatka subduction zone


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Abstract

The revealed regularities in the behavior of the electric conductivity of the geological medium on the Shipunskii Peninsula are in qualitative agreement with the seismicity variations in the Kamchatka region. The possible nature of variations in deep conductivity is considered.

About the authors

Yu. F. Moroz

Institute of Volcanology, Far East Branch; Geological Institute, Siberian Branch

Author for correspondence.
Email: morozyf@kscnet.ru
Russian Federation, bul’v. Piipa 9, Petropavlovsk-Kamchatsky, 683006; ul. Sakhyanova 6a, Ulan-Ude, 670047


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