Changes in the manner of tectonic movements under the Earth’s evolution
- Autores: Kuzmin M.1, Yarmolyuk V.2
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Afiliações:
- Vinogradov Institute of Geochemistry, Siberian Branch
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Edição: Volume 469, Nº 2 (2016)
- Páginas: 802-806
- Seção: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/188712
- DOI: https://doi.org/10.1134/S1028334X16080249
- ID: 188712
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Resumo
Variations in the O, Sr, Nd, and Hf isotopic compositions in rocks of various ages, minerals, and mantle temperature in the geological history are considered. Two periods in the Earth’s history are studied: the beginning of the formation of the planet until the turn of (3.4) 2.7–2.5 Ga and the tectonic movement period in the last 2 Ga, and also the transitional period within 2.7–2.0 Ga.
Sobre autores
M. Kuzmin
Vinogradov Institute of Geochemistry, Siberian Branch
Autor responsável pela correspondência
Email: mikuzmin@igc.irk.ru
Rússia, ul. Favorskogo 1a, Irkutsk, 664033
V. Yarmolyuk
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: mikuzmin@igc.irk.ru
Rússia, Staromonetny per. 35, Moscow, 119017