Variations in lithospheric conductivity in the Kamchatka subduction zone


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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.

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Yu. Moroz

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

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Email: morozyf@kscnet.ru
俄罗斯联邦, bul’v. Piipa 9, Petropavlovsk-Kamchatsky, 683006; ul. Sakhyanova 6a, Ulan-Ude, 670047

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