Email this article Correlation of Magmatic and Tectonic Events in the Evolution of West Chukotka Ophiolites
- Authors: Ganelin A.V.1, Sokolov S.D.1
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Affiliations:
- Geological Institute, Russian Academy of Sciences
- Issue: Vol 486, No 1 (2019)
- Pages: 485-489
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/194910
- DOI: https://doi.org/10.1134/S1028334X19050118
- ID: 194910
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Abstract
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.
About the authors
A. V. Ganelin
Geological Institute, Russian Academy of Sciences
Author for correspondence.
Email: al-gan@yandex.ru
Russian Federation, Moscow, 119017
S. D. Sokolov
Geological Institute, Russian Academy of Sciences
Email: al-gan@yandex.ru
Russian Federation, Moscow, 119017
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