The types of breccia of the ophiolite assemblage of Southwestern Crimea and their significance for the paleogeodynamics of the region
- Авторы: Promyslova M.Y.1, Demina L.I.1, Gushin A.I.1, Koronovskii N.V.1
-
Учреждения:
- Department of Geology
- Выпуск: Том 72, № 4 (2017)
- Страницы: 263-268
- Раздел: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174467
- DOI: https://doi.org/10.3103/S0145875217040056
- ID: 174467
Цитировать
Аннотация
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.
Ключевые слова
Об авторах
M. Promyslova
Department of Geology
Автор, ответственный за переписку.
Email: mary.promyslova@gmail.com
Россия, Moscow, 119991
L. Demina
Department of Geology
Email: mary.promyslova@gmail.com
Россия, Moscow, 119991
A. Gushin
Department of Geology
Email: mary.promyslova@gmail.com
Россия, Moscow, 119991
N. Koronovskii
Department of Geology
Email: mary.promyslova@gmail.com
Россия, Moscow, 119991
Дополнительные файлы
