FRACTIONATION AND ASSIMILATION DURING THE FORMATION OF THE DEVONIAN ANTIDROMIC IGNEOUS SERIES OF THE SISIM AREA IN THE MINUSINSK TROUGH: GEOCHEMICAL AND Sr-Nd ISOTOPIC EVIDENCE

In the Minusinsk trough, being the large fragment of the Devonian Altai-Sayan rift system, the antidromous series along with the homodromous volcanic series are widespread, sialic rocks with SiO2 content over 65 wt. % being predominant. Abundance of high-silica rocks in these series implies an exten...

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Bibliographic Details
Main Author: A. A. Vorontsov
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2022-10-01
Series:Геодинамика и тектонофизика
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Online Access:https://www.gt-crust.ru/jour/article/view/1544
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