Email this article Changes in the manner of tectonic movements under the Earth’s evolution
- Authors: Kuzmin M.I.1, Yarmolyuk V.V.2
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Affiliations:
- Vinogradov Institute of Geochemistry, Siberian Branch
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Issue: Vol 469, No 2 (2016)
- Pages: 802-806
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/188712
- DOI: https://doi.org/10.1134/S1028334X16080249
- ID: 188712
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Abstract
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.
About the authors
M. I. Kuzmin
Vinogradov Institute of Geochemistry, Siberian Branch
Author for correspondence.
Email: mikuzmin@igc.irk.ru
Russian Federation, ul. Favorskogo 1a, Irkutsk, 664033
V. V. Yarmolyuk
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: mikuzmin@igc.irk.ru
Russian Federation, Staromonetny per. 35, Moscow, 119017
