The types of breccia of the ophiolite assemblage of Southwestern Crimea and their significance for the paleogeodynamics of the region
- Authors: Promyslova M.Y.1, Demina L.I.1, Gushin A.I.1, Koronovskii N.V.1
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Affiliations:
- Department of Geology
- Issue: Vol 72, No 4 (2017)
- Pages: 263-268
- Section: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174467
- DOI: https://doi.org/10.3103/S0145875217040056
- ID: 174467
Cite item
Abstract
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.
About the authors
M. Yu. Promyslova
Department of Geology
Author for correspondence.
Email: mary.promyslova@gmail.com
Russian Federation, Moscow, 119991
L. I. Demina
Department of Geology
Email: mary.promyslova@gmail.com
Russian Federation, Moscow, 119991
A. I. Gushin
Department of Geology
Email: mary.promyslova@gmail.com
Russian Federation, Moscow, 119991
N. V. Koronovskii
Department of Geology
Email: mary.promyslova@gmail.com
Russian Federation, Moscow, 119991