Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike

M. D. Tomshin; N. P. Pokhilenko; E. V. Tarskikh

doi:10.1134/S1028334X17120200

Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike

M. D. Tomshin, N. P. Pokhilenko, E. V. Tarskikh

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

2 Цитирования (Scopus)

Аннотация

Study of the magmatics in the Nakyn kimberlite field, with consideration of the isotope dating results, allowed us to establish a sequence of their formation. First, 368.5–374.4 Ma ago intrusions of the Vilyui–Markha dike belt formed. Then (363–364 Ma) intrusion of kimberlites took place. In the Early Carboniferous (338.2–345.6 Ma), alkaline basaltic magma intruded through faults controlling the kimberlites. The magmatic activity finished 331–324.9 Ma ago with the formation of explosive breccias. It has been found that the Nyurba kimberlite pipe consists of two bodies: their kimberlite melts have successively intruded through independent channels.

Язык оригинала	английский
Страницы (с-по)	1458-1460
Число страниц	3
Журнал	Doklady Earth Sciences
Том	477
Номер выпуска	2
DOI	https://doi.org/10.1134/S1028334X17120200
Состояние	Опубликовано - 1 дек 2017
Опубликовано для внешнего пользования	Да

Доступ к документу

10.1134/S1028334X17120200

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Цитировать

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Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike. / Tomshin, M. D.; Pokhilenko, N. P.; Tarskikh, E. V.

В: Doklady Earth Sciences, Том 477, № 2, 01.12.2017, стр. 1458-1460.

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

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