Timing of greenschist facies diaphtoresis in the Stanovoi suture zone

The Kalar, Kurulta, Zverev, Sutam, Ayumkan, and Dzhugdzhur tectonic blocks composed of lower Pre cambrian intensely metamorphosed rocks of the Kalar, Kurulta, Zverev, Sutam, and Khobolokh sequences of the Aldan granulitegneiss megacom plex are the main geological elements of the Stanovoi structural...

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Bibliographic Details
Published in:Doklady earth sciences 2015-08, Vol.463 (2), p.782-786
Main Authors: Kotov, A. B., Larin, A. M., Smelov, A. P., Sal’nikova, E. B., Glebovitskii, V. A., Berezkin, V. I., Kovach, V. P., Kravchenko, A. A., Yakovleva, S. Z.
Format: Article
Language:English
Subjects:
Cambrian
Clay
Earth and Environmental Science
Earth Sciences
Geology
Metamorphic rocks
Plate tectonics
Rocks
Tectonics (Geology)
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Summary:The Kalar, Kurulta, Zverev, Sutam, Ayumkan, and Dzhugdzhur tectonic blocks composed of lower Pre cambrian intensely metamorphosed rocks of the Kalar, Kurulta, Zverev, Sutam, and Khobolokh sequences of the Aldan granulitegneiss megacom plex are the main geological elements of the Stanovoi structural suture, which separates the Aldan Shield from the Siberian Platform. Its peculiar feature noted by many researchers [14 and others] is the intense greenschist facies diaphtoresis of its rocks.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X15080206