Инд. авторы: Tomshin M.D., Pokhilenko N.P., Tarskikh E.V.
Заглавие: Morphology of the Nyurba Kimberlite Pipe and Its Relationship with the Dolerite Dike
Библ. ссылка: Tomshin M.D., Pokhilenko N.P., Tarskikh E.V. Morphology of the Nyurba Kimberlite Pipe and Its Relationship with the Dolerite Dike // Doklady Earth Sciences. - 2017. - Vol.477. - Iss. 2. - P.1458-1460. - ISSN 1028-334X. - EISSN 1531-8354.
Внешние системы: DOI: 10.1134/S1028334X17120200; WoS: 000419076000018;
Реферат: eng: 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.
Ключевые слова: PROVINCE;
Издано: 2017
Физ. характеристика: с.1458-1460