Инд. авторы:	Afanasiev V.P., Pokhilenko N.P., Grinenko V.S., Kostin A.V., Malkovets V.G., Oleinikov O.B.
Заглавие:	Kimberlitic Magmatism in the South-Western Flank of the Vilui Basin
Библ. ссылка:	Afanasiev V.P., Pokhilenko N.P., Grinenko V.S., Kostin A.V., Malkovets V.G., Oleinikov O.B. Kimberlitic Magmatism in the South-Western Flank of the Vilui Basin // Doklady Earth Sciences. - 2020. - Vol.490. - Iss. 2. - P.51-54. - ISSN 1028-334X. - EISSN 1531-8354.
Внешние системы:	DOI: 10.1134/S1028334X20020038; WoS: 000530808300001;
Реферат:	eng: We have analyzed 141 grains of pyrope from Neogene sediments in a quarry of construction materials, in the Kenkeme River catchment, along its left-side tributary (Chakiya River), about 60 km northwest of Yakutsk city. The mineral chemistry patterns of pyropes are typical of Jurassic-Cretaceous barren kimberlites, like the pipes of Obnazhennaya or Muza, but are uncommon to diamondiferous Middle Paleozoic kimberlites. The results allow identifying the magmatic event and placing time constraints on kimberlite magmatism in the southeastern flank of the Vilui basin, which was part of the Late Jurassic-Early Cretaceous tectonic-magmatic event in northeastern Asia.
Ключевые слова:	kimberlite; tectonic-magmatic activity; diamond; pyrope; event of kimberlite magmatism;
Издано:	2020
Физ. характеристика:	с.51-54