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Petrology of Mantle Xenoliths in Rocks of the Bezymyannyi Volcano (Kamchatka)

机译:Bezymyannyi火山(堪察加半岛)岩石中的地幔异种岩岩石学

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摘要

Most peridotite xenoliths in island-arc lavas are represented by their spinel varieties that reflect the composition of the island-arc lithospheric mantle [7]. In Kamchatka, mantle xenoliths are found in rocks from the Avachinskii, Klyuchevskoi, and Shiveluch volcanoes, as well as in baslalts of the Kharchino and Bakening areal zones. The field works in the Bezymyannyi Volcano area of 2009 yielded xenoliths of spinel harzburgites. This communication is dedicated to description of their petrographic and mineralogical properties, which were used for assessing parameters of the lithospheric mantle and revealing relations between andesites of this volcano and mantle source.
机译:岛弧熔岩中的大多数橄榄岩异岩都以其尖晶石种类代表,反映了岛弧岩石圈地幔的组成[7]。在堪察加半岛,在Avachinskii,Klyuchevskoi和Shiveluch火山的岩石中,以及在Kharchino和Bakening面带的玄武岩中都发现了地幔异岩。 2009年Bezymyannyi火山地区的野外工作产生了尖晶石harzburgites异种石。本交流致力于描述其岩石学和矿物学特性,这些特性用于评估岩石圈地幔参数并揭示该火山与地幔源安山岩之间的关系。

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  • 来源
    《Doklady Earth Sciences》 |2010年第2期|p.1317-1320|共4页
  • 作者

    V.D.Shcherbakov; P.Yu.Plechov;

  • 作者单位

    Department of Geology, Moscow State University, Moscow, Russia;

    rnDepartment of Geology, Moscow State University, Moscow, Russia;

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