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New Data on the Age of Eclogites from the Belomorian Mobile Belt at Gridino Settlement Area

机译:来自Gridino定居点的Belomorian移动带的榴辉岩年龄的新数据

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摘要

The repeated isotopic and geochemical study of zircons of the eclogite from Stolbikha Island (Gridino settlement area) allows one to interpret the U—Pb age value of about 2700 Ma by central parts of zircon grains as a magmatic event time, probably rejuvenated to a degree by intense manifestation of the eclogite metamorphism of about 1880 Ma age. The Svecofennian high-pressure metamorphism caused a partial recrystallization of zircons of magmatic origin and the appearance of their rims showing typical geochemical characteristics of eclogite zircons.
机译:对来自Stolbikha岛(Gridino居住区)的榴辉岩锆石的同位素和地球化学的反复研究,使人们可以将锆石颗粒中心部分的大约2700 Ma的U-Pb年龄值解释为岩浆事件时间,可能会恢复一定程度。由大约1880 Ma年龄的榴辉岩变质强烈表现出来。 Svecofennian高压变质作用导致岩浆成因的锆石部分重结晶,其边缘出现,显示了榴辉岩锆石的典型地球化学特征。

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  • 来源
    《Doklady Earth Sciences》 |2011年第2期|p.1163-1170|共8页
  • 作者单位

    Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, Russia;

    Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, Russia;

    Plekhanov St. Petersburg Mining Institute, St. Petersburg, Russia;

    Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, Russia;

    Plekhanov St. Petersburg Mining Institute, St. Petersburg, Russia;

    Karpinskii Russian Geological Research Institute, St. Petersburg, Russia;

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