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


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

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.

作者简介

M. Pevzner

Geological Institute

编辑信件的主要联系方式.
Email: m_pevzner@mail.ru
俄罗斯联邦, Moscow, 119991

A. Volynets

Institute of Volcanology and Seismology, Far East Branch

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

V. Lebedev

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

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

A. Babansky

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

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

D. Kovalenko

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

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

Yu. Kostitsin

Vernadsky Institute of Geochemistry and Analytical Chemistry

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

M. Tolstykh

Vernadsky Institute of Geochemistry and Analytical Chemistry

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

Yu. Kushcheva

Geological Institute

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


版权所有 © Pleiades Publishing, Ltd., 2017
##common.cookie##