First Data on Yatulian (2.1 Ga) Metamorphism in the Belomorian Mobile Belt


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The Sm–Nd isotope ages of apoamphibolite eclogites and eclogite-like garnet-clinopyroxene crystalline schists collected in the Chupa and Engozero segments of the Belomorian mobile belt are estimated. Eclogites and eclogite-like garnet–clinopyroxene rocks demonstrated nearly the same isotope age (2119 ± 170 and 2191 ± 39 Ma, respectively) on the same pair of minerals (garnet–clinopyroxene). The age obtained (about 2.1 Ga) is the oldest indicator of the onset of Paleoproterozoic metamorphism in the Belomorian mobile belt.

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V. Kozlovskiy

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences

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Email: bazil@igem.ru
俄罗斯联邦, Moscow, 119017

V. Savatenkov

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences; Institute of Earth Sciences, St. Petersburg State University

Email: bazil@igem.ru
俄罗斯联邦, St. Petersburg, 119034; St. Petersburg, 119034

L. Terentyeva

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: bazil@igem.ru
俄罗斯联邦, St. Petersburg, 119034

E. Kurdyukov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences

Email: bazil@igem.ru
俄罗斯联邦, Moscow, 119017

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