The Age of Ultramafic Rocks of the Main Ural Fault
- Авторы: Anfilogov V.N.1, Krasnobaev A.A.2, Valizer P.M.3
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Учреждения:
- Institute of Mineralogy, Ural Branch
- Institute of Geology and Geochemistry, Ural Branch
- Ilmeny State Nature Reserve
- Выпуск: Том 482, № 2 (2018)
- Страницы: 1249-1251
- Раздел: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/194121
- DOI: https://doi.org/10.1134/S1028334X1810001X
- ID: 194121
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Аннотация
The results of U–Pb zircon age dating of ultramafic massifs occurring as a chain along the Main Ural Fault zone (MUF) are given. Three groups of ages were obtained (Ma): 2500−2800, 600−2100, and 430−440. The first age group represents the time of origin of the ultramafic rocks in the Earth’s mantle. The second age group records the time of metamorphism of these rocks prior to intrusion into the host rocks. The third age group determines the time of the intrusion of ultramafic magma into the host rocks. It was established that the intrusion of ultramafic magma along the entire length of the Ural ultramafic belt occurred in the age range of 430−440 Ma.
Об авторах
V. Anfilogov
Institute of Mineralogy, Ural Branch
Автор, ответственный за переписку.
Email: anfilogov@mineralogy.ru
Россия, Miass, 456317
A. Krasnobaev
Institute of Geology and Geochemistry, Ural Branch
Email: anfilogov@mineralogy.ru
Россия, Yekaterinburg, 620016
P. Valizer
Ilmeny State Nature Reserve
Email: anfilogov@mineralogy.ru
Россия, Miass, 456317
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