TWO STAGES OF THE CENOZOIC ALKALINE-BASALT VOLCANISM IN THE DARKHAD DEPRESSION (NORTHERN MONGOLIA) – GEOCHRONOLOGY, GEOCHEMISTRY, AND GEODYNAMIC CONSEQUENCES

The isotopic data showed that there are two stages distinguished in the Cenozoic history of the Darkhad depression volcanic activity, the Late Oligocene initial stage (~28.0–26.6 Ma) and the final Late Miocene – Early Pliocene stage (~5.8–4.2 Ma). It has been stated that the rocks of the initial sta...

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Bibliographic Details
Main Authors:	S. S. Tsypukova, A. B. Perepelov, E. I. Demonterova, A. V. Ivanov, S. I. Dril, M. I. Kuzmin, A. V. Travin, Yu. D. Shcherbakov, M. Yu. Puzankov, S. V. Kanakin
Format:	Article
Language:	English
Published:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2022-09-01
Series:	Геодинамика и тектонофизика
Subjects:	cenozoic volcanism darkhad depression northern mongolia geochronology mineralogy geochemistry
Online Access:	https://www.gt-crust.ru/jour/article/view/1529
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TWO STAGES OF THE CENOZOIC ALKALINE-BASALT VOLCANISM IN THE DARKHAD DEPRESSION (NORTHERN MONGOLIA) – GEOCHRONOLOGY, GEOCHEMISTRY, AND GEODYNAMIC CONSEQUENCES

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