Changes in the manner of tectonic movements under the Earth’s evolution
- 作者: Kuzmin M.1, Yarmolyuk V.2
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隶属关系:
- Vinogradov Institute of Geochemistry, Siberian Branch
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- 期: 卷 469, 编号 2 (2016)
- 页面: 802-806
- 栏目: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/188712
- DOI: https://doi.org/10.1134/S1028334X16080249
- ID: 188712
如何引用文章
详细
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.
作者简介
M. Kuzmin
Vinogradov Institute of Geochemistry, Siberian Branch
编辑信件的主要联系方式.
Email: mikuzmin@igc.irk.ru
俄罗斯联邦, ul. Favorskogo 1a, Irkutsk, 664033
V. Yarmolyuk
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: mikuzmin@igc.irk.ru
俄罗斯联邦, Staromonetny per. 35, Moscow, 119017