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Correlation of magmatic and tectonic events in the evolution of the West Chukotka ophiolites
Author(s) -
A. V. Ganelin,
С. Д. Соколов
Publication year - 2019
Publication title -
doklady akademii nauk. rossijskaâ akademiâ nauk
Language(s) - English
Resource type - Journals
ISSN - 0869-5652
DOI - 10.31857/s0869-56524862202-207
Subject(s) - ophiolite , geology , carboniferous , tectonics , paleontology , arctic , plate tectonics , earth science , oceanography , structural basin
The article is an overview of the magmatic and geodynamic processes that formed Aluchin and Gromadnen-Vurguvem 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.

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