The beginning of volcanic activity within Sredinny metamorphic Massif (Sredinny Range, Kamchatka)


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Abstract

For the first time, the age of the beginning of the volcanic activity within Sredinny metamorphic Massif is determined (7–6 Ma). We suppose that this event was caused by the collision of Kamchatka with the Kronotsk arc that started about 7 Ma from accretion of Shipunsky peninsula. We demonstrate that at least two types of rocks were erupted within Sredinny Range of Kamchatka in late Miocene times: typical islandarc rocks were produced in the central and northern parts of the Range, and hybrid type rocks—in its southernmost part.

About the authors

M. M. Pevzner

Geological Institute

Author for correspondence.
Email: m_pevzner@mail.ru
Russian Federation, Moscow, 119991

A. O. Volynets

Institute of Volcanology and Seismology, Far East Branch

Email: m_pevzner@mail.ru
Russian Federation, Petropavlovsk-Kamchatsky

V. A. Lebedev

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

Email: m_pevzner@mail.ru
Russian Federation, Moscow

A. D. Babansky

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

Email: m_pevzner@mail.ru
Russian Federation, Moscow

D. V. Kovalenko

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

Email: m_pevzner@mail.ru
Russian Federation, Moscow

Yu. A. Kostitsin

Vernadsky Institute of Geochemistry and Analytical Chemistry

Email: m_pevzner@mail.ru
Russian Federation, Moscow

M. L. Tolstykh

Vernadsky Institute of Geochemistry and Analytical Chemistry

Email: m_pevzner@mail.ru
Russian Federation, Moscow

Yu. V. Kushcheva

Geological Institute

Email: m_pevzner@mail.ru
Russian Federation, Moscow, 119991


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