Age of Ichinsky and Khangar Stratovolcanoes (Sredinny Range, Kamchatka)


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The K–Ar isotopic age of the beginning of formation of Ichinsky (0.35) and Khangar (0.4) stratovolcanoes is established for the first time, as well as the age of the final stage of activity of the Lauchan Ridge (about 0.9 Ma) in the Sredinny Range of Kamchatka. Probably the formation of the studied volcanoes may be caused by the generation of the new deep NNE fault within the Sredinny Range of Kamchatka, which in turn was connected to the regional reasons of the increasing endogenous activity at the North-West Pacific.

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M. Pevzner

Geological Institute RAS

编辑信件的主要联系方式.
Email: m_pevzner@mail.ru
俄罗斯联邦, Moscow, 119017

V. Lebedev

Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry RAS

Email: m_pevzner@mail.ru
俄罗斯联邦, Moscow, 119017

A. Volynets

Institute of Volcanology and Seismology FEB RAS

Email: m_pevzner@mail.ru
俄罗斯联邦, Petropavlovsk-Kamchatsky, 683006

M. Tolstykh

Vernadsky Institute of Geochemistry and Analytical Chemistry RAS

Email: m_pevzner@mail.ru
俄罗斯联邦, Moscow, 119991

Yu. Kostitsin

Vernadsky Institute of Geochemistry and Analytical Chemistry RAS

Email: m_pevzner@mail.ru
俄罗斯联邦, Moscow, 119991

A. Babansky

Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry RAS

Email: m_pevzner@mail.ru
俄罗斯联邦, Moscow, 119017

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