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

机译:Sredinny变质地块(Sredinny Range,堪察加半岛)内火山活动的开始

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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.
机译:首次确定了Sredinny变质地块内火山活动开始的年龄(7-6 Ma)。我们认为,该事件是由堪察加半岛与克罗诺茨克弧的碰撞引起的,该弧从石浦斯基半岛的增生开始约7 Ma。我们证明,在中新世晚期,堪察加半岛的斯雷丁尼山脉至少爆发了两种类型的岩石:典型的岛弧岩石在山脉的中部和北部产生,而混合型岩石在其最南端产生。

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  • 来源
    《Doklady Earth Sciences》 |2017年第2期|858-862|共5页
  • 作者单位

    Russian Acad Sci, Inst Geol, Moscow 119017, Russia;

    Russian Acad Sci, Inst Volcanol & Seismol, Far East Branch, Petropavlovsk Kamchatski, Russia;

    Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia;

    Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia;

    Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia;

    Russian Acad Sci, Vernadsky Inst Geochem & Analyt Chem, Moscow, Russia;

    Russian Acad Sci, Vernadsky Inst Geochem & Analyt Chem, Moscow, Russia;

    Russian Acad Sci, Inst Geol, Moscow 119017, Russia;

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