The types of breccia of the ophiolite assemblage of Southwestern Crimea and their significance for the paleogeodynamics of the region
- Autores: Promyslova M.Y.1, Demina L.I.1, Gushin A.I.1, Koronovskii N.V.1
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Afiliações:
- Department of Geology
- Edição: Volume 72, Nº 4 (2017)
- Páginas: 263-268
- Seção: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174467
- DOI: https://doi.org/10.3103/S0145875217040056
- ID: 174467
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Resumo
This paper describes the types of breccia of the eastern part of Cape Fiolent, including verd antique (ophicalcite) for the first time, whose formation is associated with ophiolite. It has been shown that the formation of the ophiolite assemblage of the area occurred in the intersection zone of the rift valley and transform fault.
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Sobre autores
M. Promyslova
Department of Geology
Autor responsável pela correspondência
Email: mary.promyslova@gmail.com
Rússia, Moscow, 119991
L. Demina
Department of Geology
Email: mary.promyslova@gmail.com
Rússia, Moscow, 119991
A. Gushin
Department of Geology
Email: mary.promyslova@gmail.com
Rússia, Moscow, 119991
N. Koronovskii
Department of Geology
Email: mary.promyslova@gmail.com
Rússia, Moscow, 119991
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