Age and origin of rocks of the Daldyn Group of the Anabar Shield: Evidence from U-Pb zircon dating, Sm-Nd and Lu-Hf isotope systematics


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The Hf-Nd isotope systematics was used to determine the genesis of zircons from granulites of the Daldyn Group of the Anabar Shield. Obtained age of magmatic crystallization for biotite–hypersthene crystalline schists and garnet amphibolites agree with position of zircons within terrestrial array. Magmatic genesis of plagiogranite neosome under granulite conditions was established for leucocratic plagiogneisses.

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L. Sergeeva

Institute of Earth Sciences

编辑信件的主要联系方式.
Email: sergeeva.luda02@yandex.ru
俄罗斯联邦, Universitetskaya nab. 7/9, St. Petersburg, 199034

N. Gusev

Karpinskii All-Russia Research Institute of Geology

Email: sergeeva.luda02@yandex.ru
俄罗斯联邦, Srednii pr. 74, St. Petersburg, 199106

K. Lokhov

Institute of Earth Sciences; Karpinskii All-Russia Research Institute of Geology

Email: sergeeva.luda02@yandex.ru
俄罗斯联邦, Universitetskaya nab. 7/9, St. Petersburg, 199034; Srednii pr. 74, St. Petersburg, 199106

V. Glebovitskii

Institute of Earth Sciences; Institute of Precambrian Geology and Geochronology

Email: sergeeva.luda02@yandex.ru
俄罗斯联邦, Universitetskaya nab. 7/9, St. Petersburg, 199034; nab. Makarova 2, St. Petersburg, 197034

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