Тип публикации: статья из журнала
Год издания: 2017
Идентификатор DOI: 10.1134/S1028334X17070224
Аннотация: It has been demonstrated on basis of Sm–Nd isotopic analyses of the Cenozoic sands from the Chara and Tokkin Basins in the eastern flank of the Baikal rift zone that the Chara–Olekma Geoblock of the Aldan Shield is an area of intense crust growing processes occurred not only in the Paleoarchaean but in the Mesoarchaean as well. © 2017, Pleiades Publishing, Ltd.
Издание
Журнал: Doklady Earth Sciences
Выпуск журнала: Vol. 475, Is. 1
Номера страниц: 758-761
ISSN журнала: 1028334X
Издатель: Maik Nauka-Interperiodica Publishing
Персоны
- Kotov A.B. (Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, Russian Federation)
- Skovitina T.M. (Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences, Irkutsk, Russian Federation)
- Kovach V.P. (Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, Russian Federation)
- Velikoslavinsky S.D. (Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, Russian Federation)
- Lopatin D.V. (Institute of Earth Sciences of St. Petersburg State University, St. Petersburg, Russian Federation)
- Sklyarov E.V. (Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences, Irkutsk, Russian Federation, Far Eastern Federal University, Vladivostok, Russian Federation)
- Tolmacheva E.V. (Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, Russian Federation)
- Bobrovskaya O.V. (Institute of Earth Sciences of St. Petersburg State University, St. Petersburg, Russian Federation)
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