Correlation of Magmatic and Tectonic Events in the Evolution of West Chukotka Ophiolites

The article is an overview of the magmatic and geodynamic processes that formed Aluchin and Gromadnen-Vurguveem ophiolites in the territory of Western Chukotka. The ophiolites formed into a convergent system between the Siberian continent and the Proto-Arctic Ocean. In the tectonic evolution of this...

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Veröffentlicht in:Doklady earth sciences 2019-05, Vol.486 (1), p.485-489
Hauptverfasser: Ganelin, A. V., Sokolov, S. D.
Format: Artikel
Sprache:eng
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Zusammenfassung:The article is an overview of the magmatic and geodynamic processes that formed Aluchin and Gromadnen-Vurguveem ophiolites in the territory of Western Chukotka. The ophiolites formed into a convergent system between the Siberian continent and the Proto-Arctic Ocean. In the tectonic evolution of this system, important milestones have been identified: the Early Carboniferous, the Later Triassic and the Late Jurassic.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X19050118